SOLUTIONS MANUAL TO ACCOMPANY INTRODUCTION TO FLIGHT 7th Edition By John D. Anderson, Jr. Chapter 2 2.1 ρ = p/RT = (1.2)(1.01× 105 )/(287)(300) ρ = 1.41 kg/m 2 v = 1/ρ = 1/1.41 = 0.71 m3 /kg 2.2 3 3 k T = (1.38 × 10−23 ) (500) = 1.035 × 10−20 J 2 2 One kg-mole, which has a mass of 4 kg, has 6.02 × 1026 atoms. Hence 1 kg has 1 (6.02 × 1026 ) = 1.505 × 1026 atoms. 4 Mean kinetic energy of each atom = Totalinternal energy = (energy per atom)(number of atoms) = (1.035 ´10-20 )(1.505 ´1026 ) = 1.558 ´ 106 J 2.3 ρ= 2116 slug p = = 0.00237 3 ft RT (1716)(460 + 59) Volume of the room = (20)(15)(8) = 2400 ft 3 Total mass in the room = (2400)(0.00237) = 5.688slug Weight = (5.688)(32.2) = 183lb 2.4 ρ= p 2116 slug = = 0.00274 3 RT (1716)(460 - 10) ft Since the volume of the room is the same, we can simply compare densities between the two problems. Δρ = 0.00274 - 0.00237 = 0.00037 % change = 2.5 Δρ ρ = slug ft 3 0.00037 ´ (100) = 15.6% increase 0.00237 First, calculate the density from the known mass and volume, ρ = 1500 / 900 = 1.67 lb m /ft 3 In consistent units, ρ = 1.67/32.2 = 0.052 slug/ft 3. Also, T = 70 F = 70 + 460 = 530 R. Hence, p = ρ RT = (0.52)(1716)(530) p = 47, 290 lb/ft 2 or p = 47, 290 / 2116 = 22.3 atm 2 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 2.6 p = ρ RT np = np + nR + nT Differentiating with respect to time, 1 dp 1 d ρ 1 dT = + p dt ρ dt T dt or, dp p d ρ p dT = + dt ρ dt T dt or, dp dρ dT = RT + ρR dt dt dt (1) At the instant there is 1000 lbm of air in the tank, the density is ρ = 1000 / 900 = 1.11lb m /ft 3 ρ = 1.11/32.2 = 0.0345slug/ft 3 Also, in consistent units, is given that T = 50 + 460 = 510 R and that dT = 1F/min = 1R/min = 0.016 R/sec dt From the given pumping rate, and the fact that the volume of the tank is 900 ft3, we also have d ρ 0.5 lb m /sec = = 0.000556 lb m /(ft 3 )(sec) dt 900 ft 3 d ρ 0.000556 = = 1.73 × 10−5 slug/(ft 3 )(sec) dt 32.2 Thus, from equation (1) above, dρ = (1716)(510)(1.73 × 10−5 ) + (0.0345)(1716)(0.0167) dt 16.1 = 15.1 + 0.99 = 16.1 lb/(ft 2 )(sec) = 2116 = 0.0076 atm/sec 2.7 In consistent units, T = −10 + 273 = 263 K Thus, ρ = p/RT = (1.7 × 104 )/(287)(263) ρ = 0.225 kg/m3 2.8 ρ = p/RT = 0.5 ×105 /(287)(240) = 0.726 kg/m3 v = 1/ρ = 1/0.726 = 1.38 m3 /kg 3 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 2.9 Fp = Force due to pressure = ò 3 p dx = 0 3 ò (2116 - 10 x) dx 0 = [2116 x - 5 x 2 ] 30 = 6303 lb perpendicular to wall. Fτ = Force due to shear stress = ò 3 τ dx = 0 ò 3 0 90 (x + 1 9) 2 dx 1 = [180 ( x + 9) 2 ] 30= 623.5 - 540 = 83.5 lb tangential to wall. Magnitude of the resultant aerodynamic force = R = (6303) 2 + (835) 2 = 6303.6 lb æ 83.5 ÷ö = 0.76º çè 6303 ÷÷ø θ = Arc Tan çç 3 V∞ sin θ 2 Minimum velocity occurs when sin θ = 0, i.e., when θ = 0° and 180°. 2.10 V = Vmin = 0 at θ = 0° and 180°, i.e., at its most forward and rearward points. Maximum velocity occurs when sin θ = 1, i.e., when θ = 90°. Hence, Vmax = 3 (85)(1) = 127.5 mph at θ = 90°, 2 i.e., the entire rim of the sphere in a plane perpendicular to the freestream direction. 4 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 2.11 The mass of air displaced is M = (2.2)(0.002377) = 5.23 ´ 10-3 slug The weight of this air is Wair = (5.23 ´10-3 )(32.2) = 0.168 lb This is the lifting force on the balloon due to the outside air. However, the helium inside the balloon has weight, acting in the downward direction. The weight of the helium is less than that of air by the ratio of the molecular weights WH c = (0.168) 4 = 0.0233 lb. 28.8 Hence, the maximum weight that can be lifted by the balloon is 0.168 − 0.0233 = 0.145 lb. 2.12 Let p3, ρ3, and T3 denote the conditions at the beginning of combustion, and p4, ρ4, and T4 denote conditions at the end of combustion. Since the volume is constant, and the mass of the gas is constant, then p4 = ρ3 = 11.3 kg/m3. Thus, from the equation of state, p4 = ρ4 RT4 = (11.3)(287)(4000) = 1.3 ´ 107 N/m 2 or, p4 = 1.3 ´ 107 1.01 ´ 105 = 129 atm 2.13 The area of the piston face, where the diameter is 9 cm = 0.09 m, is A= (a) π (0.09) 2 4 = 6.36 ´ 10-3 m 2 The pressure of the gas mixture at the beginning of combustion is p3 = ρ3 RT3 = 11.3(287)(625) = 2.02 ´ 106 N/m 2 The force on the piston is F3 = p3 A = (2.02 ´ 106 )(6.36 ´10-3 ) = 1.28 ´ 104 N Since 4.45 N = l lbf, F3 = (b) 1.28 ´ 104 = 2876 lb 4.45 p4 = ρ4 RT4 = (11.3)(287)(4000) = 1.3 ´ 107 N/m 2 The force on the piston is F4 = p4 A = (1/3 ´107 ) (6.36 ´10-3 ) = 8.27 ´ 104 N F4 = 8.27 ´ 104 = 18,579 lb 4.45 5 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 2.14 Let p3 and T3 denote conditions at the inlet to the combustor, and T4 denote the temperature at the exit. Note: p3 = p4 = 4 ´ 106 N/m 2 (a) ρ3 = p3 4 ´ 106 = 15.49 kg/m3 = RT3 (287)(900) (b) ρ4 = p4 4 ´ 106 = 9.29 kg/m3 = RT4 (287)(1500) 2.15 1 mile = 5280 ft, and 1 hour = 3600 sec. So: æ miles ÷öæ 5280 ft ÷öæ 1 hour ÷ö çç 60 ÷çç ÷çç ÷ = 88 ft/sec. èç hour ÷øèç mile ÷øèç 3600 sec ÷ø A very useful conversion to remember is that 60 mph = 88 ft/sec also, 1 ft = 0.3048 m æ ö æ ÷öç 0.3048 m ÷÷ = 26.82 m ç 88 ft ÷ç ÷÷ ÷èç 1 ft çèç sec ø÷ç sec ø Thus 2.16 88 ft m = 26.82 sec sec 692 miles 88 ft/sec = 1015 ft/sec hour 60 mph 692 miles 26.82 m/sec = 309.3 m/sec hour 60 mph 2.17 On the front face Ff = p f A = (1.0715 ×105 )(2) = 2.143 ×105 N On the back face Fb = pb A = (1.01 × 105 )(2) = 2.02 × 105 N The net force on the plate is F = Ff − Fb = (2.143 − 2.02) ×105 = 0.123 × 105 N From Appendix C, 1 lb f = 4.448 N. So, F= 0.123 ×105 = 2765 lb 4.448 This force acts in the same direction as the flow (i.e., it is aerodynamic drag.) 6 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 2.18 Wing loading = W 10,100 = = 43.35 lb/ft 2 233 s In SI units: W lb 4.448 N 1 ft = 43.35 2 s ft 1 lb 0.3048 m 2 W N = 2075.5 s m2 In terms of kilogram force, kg f N 1kf W = 2075.5 2 = 211.8 2 m 9.8 N m s miles 5280 ft 0.3048 m 5 m = 703.3 km 2.19 V = 437 = 7.033 × 10 hr mile 1 ft hr hr 0.3048 m = 7620 m = 7.62 km Altitude = (25, 000 ft) 1 ft ft 0.3048 m 3 m = 7.925 km 2.20 V = 26, 000 = 7.925 × 10 sec 1 ft sec sec 2.21 From Fig. 2.16, length of fuselage = 33 ft, 4.125 inches = 33.34 ft 0.3048 m = 33.34 ft = 10.16 m ft wing span = 40 ft, 11.726 inches = 40.98 ft 0.3048 m = 40.98 ft = 12.49 m ft 7 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 3 3.1 An examination of the standard temperature distribution through the atmosphere given in Figure 3.3 of the text shows that both 12 km and 18 km are in the same constant temperature region. Hence, the equations that apply are Eqs. (3.9) and (3.10) in the text. Since we are in the same isothermal region with therefore the same base values of p and ρ, these equations can be written as ρ2 p -( g /RT )(h 2- h 1) = 2 = e 0 ρ1 p1 where points 1 and 2 are any two arbitrary points in the region. Hence, with g0 = 9.8 m/sec2 and R = 287 joule/kgK, and letting points 1 and 2 correspond to 12 km and 18 km altitudes, respectively, 9.8 (6000) ρ2 p = 2 = e (287)(216.66) = 0.3884 ρ1 p1 Hence: p2 = (0.3884)(1.9399 ´ 104 ) = 7.53 ´ 103 N/m 2 ρ2 = (0.3884)(3.1194 ´ 10-1) = 0.121 kg/m3 and, of course, T2 = 216.66 K These answers check the results listed in Appendix A of the text within round-off error. 3.2 From Appendix A of the text, we see immediately that p = 2.65 × 104 N/m2 corresponds to 10,000 m, or 10 km, in the standard atmosphere. Hence, pressure altitude = 10 km The outside air density is ρ = p 2.65 ´ 104 = = 0.419 kg/m3 RT (287)(220) From Appendix A, this value of ρ corresponds to 9.88 km in the standard atmosphere. Hence, density altitude = 9.88 km 3.3 At 35,000 ft, from Appendix B, we find that p = 4.99 × 102 = 499 lb/ft2. 3.4 From Appendix B in the text, 33,500 ft corresponds to p = 535.89 lb/ft2 32,000 ft corresponds to ρ = 8.2704 × 10−4 slug/ft3 Hence, T = p 535.89 = = 378 R ρR (8.2704 ´ 10-4 )(1716) 8 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.5 h - hG h = 0.02 = 1 - hG h From Eq. (3.6), the above equation becomes æ r + hG 1 - çç çè r ÷÷ö = 1 - 1 - hG = 0.02 ÷ø r hG = 0.02 r = 0.02(6.357 ´ 106 ) hG = 1.27 ´ 105 m = 127 km 3.6 T = 15 − 0.0065h = 15 − 0.0065(5000) = −17.5°C = 255.5°K a = dT = -0.0065 dh From Eq. (3.12) æ T ö÷-g0 /aR æ 255.5 ÷ö-(2.8) /(-0.0065)(287) p = ççç ÷÷ = çç = 0.533 çè 288 ÷÷ø çè T1 ø÷ p1 p = 0.533 p1 = 0.533 (1.01 ´ 105 ) = 5.38 ´ 104 N/m 2 3.7 n p g (h - h1) =p1 RT h - h1 = - 1 p 1 RT n =(4157)(150) n 0.5 g p1 24.9 Letting h1 = 0 (the surface) h = 17,358 m = 17.358 km 9 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.8 A standard altitude of 25,000 ft falls within the first gradient region in the standard atmosphere. Hence, the variation of pressure and temperature are given by: g æ T ö- aR p = ççç ÷÷÷ çè T1 ÷ø p1 (1) T = T1 + a (h – h1) (2) and Differentiating Eq. (1) with respect to time: g æ g ö æ 1 ö- aR æ g ö çççè - aR -1÷÷÷ø dT 1 dp ÷÷ T çç = ççç ÷÷÷ çè T1 ÷ø èç AR ÷ø p1 dt dt (3) Differentiating Eq. (2) with respect to time: dT dh = a dt dt (4) Substitute Eq. (4) into (3) g æ g ö÷ æ g ö -ççç +1÷÷ dh dp = - p1(T1) aR çç ÷÷÷ T è aR ø çè R ø dt dt (5) In Eq. (5), dh/dt is the rate-of-climb, given by dh/dt = 500 ft/sec. Also, in the first gradient region, the lapse rate can be calculated from the tabulations in Appendix B. For example, take 0 ft and 10,000 ft, we find a = T2 - T1 483.04 - 518.69 °R = = -0.00357 h2 - h1 10, 000 - 0 ft Also from Appendix B, p1= 2116.2 lb/ft2 at sea level, and T = 429.64 °R at 25,000 ft. Thus, g 32.2 = = -5.256 aR (-0.00357)(1716) Hence, from Eq. (5) æ 32.2 ö÷ dp (429.64)4.256 (500) = -(2116.2)(518.69)-5.256 çç çè 1716 ø÷÷ dt dp lb = -17.17 2 dt ft sec 10 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.9 From the hydrostatic equation, Eq. (3.2) or (3.3), or dp = -ρ g0 dh dp dh = -ρ g0 dt dt The upward speed of the elevator is dh/dt, which is dp dp/dt = dt -ρ g0 At sea level, ρ = 1.225 kg/m3. Also, a one-percent change in pressure per minute starting from sea level is dp = -(1.01 ´ 105 )(0.01) = -1.01 ´ 103 N/m 2 per minute dt Hence, dh -1.01 ´ 103 = = 84.1meter per minute dt (1.225)(9.8) 3.10 From Appendix B: At 35,500 ft: p = 535.89 lb/ft2 At 34,000 ft: p = 523.47 lb/ft2 For a pressure of 530 lb/ft2, the pressure altitude is æ 535.89 - 530 ö÷ 33,500 + 500 çç = 33737 ft çè 535.89 - 523.47 ø÷÷ The density at the altitude at which the airplane is flying is ρ = ρ RT = 530 = 7.919 ´ 10-4 slug/ft 3 (1716)(390) From Appendix B: At 33,000 ft: ρ = 7.9656 ´ 10-4 slug/ft 3 At 33,500 ft: ρ = 7.8165 ´ 10-4 slug/ft 3 Hence, the density altitude is æ 7.9656 - 7.919 ö÷ 33, 000 + 500 çç = 33,156 ft çè 7.9656 - 7.8165 ø÷÷ 11 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.11 Let ℓ be the length of one wall of the tank, ℓ = 30 ft. Let d be the depth of the pool, d = 10 ft. At the water surface, the pressure is atmospheric pressure, pa. The water pressure increases with increasing depth; the pressure as a function of distance below the surface, h, is given by the hydrostatic equation dp = ρ g dh (1) Note: The hydrostatic equation given by Eq. (3.2) in the text has a minus sign because hG is measured positive in the upward direction. In Eq. (1), h is measured positive in the downward direction, with h = 0 at the surface of the water. Hence, no minus sign appears in Eq. (1); as h increases (as we go deeper into the water), p increases. Eq. (1) is consistent with this fact. Integrating Eq. (1) from h = 0 where p = pa to some local depth h where the pressure is p, and noting that ρ is constant for water, we have ρ òp dp = ρ g a or, h ò0 dh p − pa = ρ g h or, p = ρ g h + pa Eq. (2) gives the water pressure exerted on the wall at an arbitrary depth h. (2) Consider an elementary small sliver of wall surface of length ℓ and height dh. The water force on this sliver of area is dF = p ℓ dh Total force, F, on the wall is F = ò0 F dF = ò0 d p dh (3) where p is given by Eq. (2). Inserting Eq. (2) into (3), F = or, ò0 d (ρ g h + pa ) dh æ d 2 ö÷ ç F = ρ g çç ÷÷ + pa d çè 2 ø÷÷ (4) In Eq. (4), the product ρ g is the specific weight (weight per unit volume) of water; ρ g = 62.4 lb/ft3. From Eq. (4), (10) 2 + (2116)(30)(10) 2 F = 93, 600 + 634,800 = 728, 400 lb F = (62.4)(30) Note: This force is the combined effect of the force due to the weight of the water, 93,600 lb, and the force due to atmospheric pressure transmitted through the water, 634,800 Ib. In this example, the latter is the larger contribution to the force on the wall. If the wall were freestanding with atmospheric pressure exerted on the opposite side, then the net force exerted on the wall would be that due to the weight of the water only, i.e., 93,600 Ib. In tons, the force on the side of the wall in contact with the water is F = 728, 400 = 364.2 tons 2000 In the case of a freestanding wall, the net force, that due only to the weight of the water, is F = 93, 600 = 46.8 tons 2000 12 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.12 For the exponential atmosphere model, ρ = e-g0 h/(RT ) ρ0 ρ = e-(9.8)(45,000) /(287)(240) = e-6.402 ρ0 Hence, ρ = ρ0e-6.402 = (1225)(1.6575 ´ 10-3 ) = 2.03 ´ 10-3 kg/m3 From the standard atmosphere, at 45 km, p = 2.02 × 10−3 kg/m3. The exponential atmosphere model gives a remarkably accurate value for the density at 45 km when a value of 240 K is used for the temperature. 3.13 At 3 km, from App. A, T = 268.67 K, p = 7.0121 × 104 N/m2, and from App. A, T = 268.02 K, p = 6.9235 × 104 N/m2, and using linear interpolation: = 0.90926 kg/m3. At 3.1 km, = 0.89994 kg/m3. At h = 3.035 km, 0.035 T = 268.67 − (268.67 − 268.02) = 268.44 K 0.1 0.035 p = 7.0121 × 10 4 − (7.0121 × 10 4 − 6.9235 × 10 4 ) 0.1 = 6.98099 × 10 4 N m2 kg 0.035 = 0.906 0.1 m3 ρ = 0.09026 − (0.90926 − 0.89994) 13 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.14 The altitude of 3.035 km is in the gradient region. From Example 3.1, a = –0.0065 K/m. From Eq. (3.14), T = T1 + a (h − h1 ) = Ts + a(h − 0) = 288.16 − (0.0065)(3035) = 268.43 K From Eq. (3.12), p T = p1 T1 − g0 / aR − g0 −9.8 = = 5.25328 aR ( −0.0065)(28.7) So p T = ps Ts 5.25328 268.43 = 288.16 5.25328 = 0.688946 p = 0.688946(1.01325 × 105 ) = 6.9807 × 10 4 N m2 By comparison the approximate result from the solution of Prob. 3.13 differs from the exact result above by 6.980990 − 06.9807 = 4.15 × 10−5 = 0.00415% 6.9807 A very small amount. From Eq. (3.13), ρ T = ρ1 T1 −[( g0 /aR )+1] g0 + 1 = −5.25328 + 1 = −4.25328 aR ρ T = ρs Ts 4.2538 268.43 = 288.16 4.24328 = 0.73958 ρ = 0.73598 ρs = 0.73958 (1.2250) = 0.90599 14 kg m3 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 3.15 We want to calculate hG when hG − h h = 0.01 = 1 − hG hG From Eq. (3.6) h= rhG , where r = 6.356766 × 106 m r + hG Thus, 0.01 = 1 − r r + hG r = 1 − 0.01 = 0.99 r + hG 0.99 (r + hG ) = r 1 − 0.99 hG = r = 0.0101 (6.356766 × 105 ) 0.99 hG = 64.21 × 103 m = 64.21 km 3.16 From Eq. (3.1), r g = g0 r + hG 2 where r = 6.356766 × 106 m, g0 = 9.8 m/sec2, and 0.3048 m hG = (70,000 ft) = 21,336 m 1 ft Thus, 6.356766 × 106 m g = 9.8 = 9.767 6 sec2 6.356766 × 10 + 21,336 9.8 − 9.767 100 = 0.34% 98 Thus, at 70,000 ft, the acceleration of gravity has decreased only by 0.34% compared to its sea level value. 15 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 4 4.1 AV 1 1 = A2V2 Let points 1 and 2 denote the inlet and exit conditions, respectively. Then, æA ö æ1ö V2 = V1 ççç 1 ÷÷÷ = (5) çç ÷÷ = 1.25ft/sec ç è 4 ø÷ èç A2 ø÷ 4.2 From Bernoulli’s equation, V2 V2 p1 + ρ 1 = p2 + ρ 2 2 2 p2 - p1 = ρ 2 (V12 - V22 ) In consistent units, ρ = 62.4 = 1.94 slug/ft 3 32.2 Hence, p2 - p1 = 1.94 [(5) 2 - (1.25)2 ] 2 p2 - p1 = 0.97(23.4) = 22.7 lb/ft 2 4.3 From Appendix A; at 3000m altitude, p1 = 7.01 ´ 104 N/m 2 ρ = 0.909 kg/m3 From Bernoulli’s equation, p2 = p1 + ρ 2 (V12 - V22 ) p2 = 7.01 ´ 104 + 0.909 [602 - 702 ] 2 p2 = 7.01 ´ 104 - 0.059 ´ 104 = 6.95 ´ 104 N/m 2 16 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.4 ρ ρ V12 = p2 + V22 2 2 Also from the incompressible continuity equation p1 + From Bernoulli’s equation, V2 = V1( A1/A2 ) ρ p1 + Combining, 2 V12 = p2 + ρ 2 ( A1/A2 )2 2( p1 - p2 ) é ρ ê ( A1 / A2 )2 - 1ùú ë û V1 = At standard sea level, p = 0.002377 slug/ft3. Hence, 2(80) V1 = (.002377)[(4)2 - 1] = 67 ft/sec æ 60 ö Note that also V1 = 67 çç ÷÷÷ = 46 mi/h. (This is approximately the landing speed of World çè 80 ø War I vintage aircraft). 4.5 p1 + 1 1 ρ V 2 = p3 + ρ V 2 2 2 V12 = 2( p3 - p1) ρ + V32 A1 V1 = A3 V3 , or V3 = (1) A1 V1 A3 (2) Substitute (2) into (1) V12 = 2( p3 - p1) ρ 2( p3 - p1) é æ A ö÷2 ùú ê ρ ê 1 - ççç 1 ÷÷ ú ê èç A3 ÷ø úú êë û or, V1 = Also, A1 V1 = A2 V2 or, æ A ö2 + ççç 1 ÷÷÷ V12 çè A3 ÷ø (3) æA ö V2 = ççç 1 ÷÷÷ V1 çè A2 ÷ø (4) Substitute (3) into (4) V1 = A1 A2 2( p3 - p1) é æ A ö÷2 ùú ê ρ ê 1 - ççç 1 ÷÷ ú çè A3 ÷ø ú ê êë úû 3 2(1.00 - 1.02) ´ 105 V2 = 102.22 m/sec é 1.5 æ 3 ö÷2 ùú ê (1.225) ê 1 - çç ÷÷ ú çè 2 ø ú êë û Note: It takes a pressure difference of only 0.02 atm to produce such a high velocity. V2 = 17 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.6 æ 88 ö V1 = 130 mph = 130 çç ÷÷÷ = 190.7 ft/sec çè 60 ø p1 + 1 1 ρ V12 = p2 + ρ V22 2 2 2 V22 = ( p1 - p2 ) + V12 ρ 2(1760.9 - 1750.0) V22 = + (190.7)2 0.0020482 V2 = 216.8ft/sec 4.7 From Bernoulli’s equation, ρ (V22 - V12 ) 2 And from the incompressible continuity equation, p1 - p2 = V2 = V1 ( A1/A2 ) ρ V12 [( A1/A2 )2 - 1] 2 Hence, the maximum pressure difference will occur when simultaneously: 1. V1 is maximum p1 - p2 = Combining: 2. ρ is maximum i.e., sea level The design maximum velocity is 90 m/sec, and ρ = 1.225 kg/m3 at sea level. Hence, 1.225 (90)2[(1.3)2 - 1] = 3423 N/m 2 2 Please note: In reality the airplane will most likely exceed 90 m/sec in a dive, so the airspeed indicator should be designed for a maximum velocity somewhat above 90 m/sec. p1 - p2 = 4.8 The isentropic relations are γ æ ρ ÷öγ æ T öγ -1 pc = ççç e ÷÷ = ççç c ÷÷÷ çè ρ0 ÷ø p0 èç T0 ÷ø γ Hence, 14-1 1.4 æ ρ öγ -1 æ 1 ö = (300) çç ÷÷ Te = T0 ççç e ÷÷÷ çè 10 ÷ø çè ρ0 ÷ø = 155 K From the equation of state: ρ0 = p0 (10)(1.01 ´ 105 ) = = 11.73kg/m3 (287)(300) RT0 1 Thus, 1 æ p öγ æ 1 ö1.4 ρe = ρ0 ççç e ÷÷÷ = 11.73çç ÷÷÷ = 2.26 kg/m3 çè 10 ø èç p0 ÷ø As a check on the results, apply the equation of state at the exit. pe = ρe RTe ? 1.01 ´ 105 = (2.26)(287)(155) 1.01 ´ 105 = 1.01 ´ 105 It checks! 18 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.9 Since the velocity is essentially zero in the reservoir, the energy equation written between the reservoir and the exit is V2 h0 = he + e or, Ve2 = 2(h0 - he ) 2 However, h = cpT. Thus Eq. (1) becomes (1) Ve2 = 2c p (T0 - Te ) æ Ve2 = 2c p T0 ççç1 èç Te ÷ö ÷÷ T0 ÷ø (2) However, the flow is isentropic, hence γ -1 æp ö γ Tc = ççç c ÷÷÷ çè p0 ÷ø T0 (3) Substitute (3) into (1). Ve = γ -1 ù é ê æ ö γ úú p ÷ 2 c p T0 êê 1 - ççç e ÷÷ ú çè p0 ÷ø ê ú êë úû (4) This is the desired result. Note from Eq. (4) that Ve increases as T0 increases, and as pe/p0 decreases. Equation (4) is a useful formula for rocket engine performance analysis. 4.10 The flow velocity is certainly large enough that the flow must be treated as compressible. From the energy equation, V2 V2 c p T1 + 1 = c p T2 - 2 2 2 At a standard altitude of 5 km, from Appendix A, (1) p1 = 5.4 ´ 104 N/m 2 T1 = 255.7 K Also, for air, cp = 1005 joule/(kg)(K). Hence, from Eq. (1) above, V 2 - V22 T2 = T1 + 1 2 cp T2 = 255.7 + (270)2 - (330)2 2(1005) T2 = 255.7 - 17.9 = 237.8 K Since the flow is also isentropic, γ -1 æT ö γ p2 = ççç 2 ÷÷÷ çè T1 ø÷ p1 γ -1 Thus, æT ö γ p2 = p1 ççç 2 ÷÷÷ çè T ÷ø 1 1.4 æ 237.8 ö÷1.4-1 = 5.4 ´ 104 çç çè 255.7 ø÷÷ p2 = 4.19 ´ 104 N/m 2 Please note: This problem and Problem 4.3 ask the same question. However, the flow velocities in the present problem require a compressible analysis. Make certain to examine the solutions of both Problems 4.10 and 4.3 in order to contrast compressible versus incompressible analyses. 19 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.11 From the energy equation or, V2 c pT0 = c pTe + e 2 Ve2 Te = T0 2 cp Te = 1000 - 15002 = 812.5 R 2(6000) In the reservoir, the density is p0 (7)(2116) = = 0.0086 slug/ft 3 (1716)(1000) RT0 ρ0 = From the isentropic relation, 1 æ T öγ -1 ρc = ççç e ÷÷÷ çè T0 ø÷ ρ0 1 æ 812.5 ö÷1.4-1 ρe = 0.0086 çç = 0.0051 slug/ft 3 çè 1000 ÷÷ø From the continuity equation, m = ρe AeVe Thus, Ae = m ρeVe In consistent units, m = 1.5 = 0.047 slug/sec. 32.2 Hence, Ae = m 0.047 = = 0.061ft 2 (0.0051)(1500) ρcVe æ 88 ö 4.12 V1 = 1500 mph = 1500 çç ÷÷÷ = 2200 ft/sec çè 60 ø V2 V2 C pT1 + 1 C pT2 2 2 2 V22 = 2C p (T1 - T2 ) + V12 V22 = 2(6000)(389.99 - 793.32) + (2200) 2 V2 = 6.3ft/sec Note: This is a very small velocity compared to the initial freestream velocity of 2200 ft/sec. At the point in question, the velocity is very near zero, and hence the point is nearly a stagnation point. 20 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.13 At the inlet, the mass flow of air is m air = ρ AV = (3.6391 ´ 10-4 )(20)(2200) = 16.0/slug/sec m fuel = (0.05)(16.01) = 0.8slug/sec Total mass flow at exit = 16.01 + 0.8 = 16.81slug/sec 4.14 From Problem 4.11, Ve = 1500 ft/sec Te = 812.5 R Hence, γ RTe = ae = (1.4)(1716)(812.5) = 1397 ft/sec V 1500 Mc = e = = 1.07 ae 1397 Thus, Note that the nozzle of Problem 4.11 is just barely supersonic. 4.15 From Appendix A, T∞ = 216.66 K Hence, a∞ = = Thus, γRT (1.4)(287)(216.66) = 295m/sec V 250 M∞ = ∞ = = 0.847 a∞ 295 4.16 At standard sea level, T∞ = 518.69 R a∞ = γ RT = (1.4)(1716)(518.69) = 1116 ft/sec V∞ = M ∞ a∞ = (3)(1116) = 3348ft/sec Since 60 mi/hr - 88 ft/sec., then V∞ = 3348(60/88) = 2283mi/h 4.17 V = 2200 ft/sec a = γRT = M = V 2200 = = 2.27 a 967.94 (1.4)(1716)(389.99) = 967.94 ft/sec 21 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.18 The test section density is ρ = p 1.01 ´ 105 = = 1.173kg/m3 (287)(300) RT Since the flow is low speed, consider it to be incompressible, i.e., with the above density throughout. ρ p1 - p2 = 2 V22[1 - ( A2 /A1) 2 ] (1) In terms of the manometer reading, p1 - p2 = ωΔh (2) where ω = 1.33 ´ 105 N/m3 for mercury. Thus, combining Eqs. (1) and (2), Δh = ρ 2 V2 [1 - ( A2 /A1) 2 ] 2ω 1.173 = 5 (80)2[1 - (1/20)2 ] (2)(1.33 ´ 10 ) Δh = 0.028m = 2.8 cm æ 88 ö 4.19 V2 = 200 mph = 300 çç ÷÷÷ = 293.3 ft/sec çè 60 ø (a) p1 + 1 1 ρ V12 = p2 + ρ V22 2 2 A1 V1 = A2V2 V1 = A2 V2 A1 2 1 æç A2 ÷ö 2 1 2 ÷ p1 + ρ çç ÷÷ V2 = p2 + ρ V2 ç 2 è A1 ø 2 é æ A ÷ö2 ùú 2 1 ê p1 - p2 = ρ ê 1 - ççç 2 ÷÷ ú V2 çè A1 ÷ø ú 2 ê ëê ûú p1 - p2 = 0.002377 2 2ù é ê 1 - æç 4 ÷ö ú (293.3)2 çç ÷÷ ú ê è 20 ø ú ëê û p1 - p2 = 98.15 lb/ft 2 22 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) p1 + 1 1 ρ V12 = p3 + ρ V33 2 2 AV 1 1 = A2V2 : V1 = A2 V2 A1 A2V2 = A3V3 : V3 = A2 V2 A3 p1 - p3 = 2 é æ A ö2 ùú 1 ê çæ A2 ÷ö ρ ê çç ÷÷ - ççç 2 ÷÷÷ ú V22 çè A1 ÷ø ú 2 ê çè A3 ÷ø úû ëê p1 - p3 = 2 é æ 4 ö÷2 ùú 0.002377 ê æç 4 ÷ö çç ÷ ú (293.3)2 ÷ ê çç ÷ ç 20 ø÷ ú è ø è 2 18 ëê û p1 - p3 = 0.959 lb/ft 2 Note: By the addition of a diffuser, the required pressure difference was reduced by an order of magnitude. Since it costs money to produce a pressure difference (say by running compressors or vacuum pumps), then a diffuser, the purpose of which is to improve the aerodynamic efficiency, allows the wind tunnel to be operated more economically. 4.20 In the test section ρ = p 2116 = = 0.00233slug/ft 3 (1716)(70 + 460) RT The flow velocity is low enough so that incompressible flow can be assumed. Hence, from Bernoulli’s equation, 1 ρV 2 2 1 p0 = 2116 + (0.00233)[150(88 / 60)]2 2 (Remember that 88 ft/sec = 60 mi/h.) p0 = p + 1 (0.00233)(220)2 2 p0 = 2172 lb/ft 2 p0 = 2116 + 4.21 The altimeter measures pressure altitude. Thus, from Appendix B, p = 1572 lb/ft2. The air density is then ρ = p 1572 = = 0.00183slug/ft 3 (1716)(500) RT Hence, from Bernoulli’s equation, Vtrue = 2( p0 - p) ρ = 2(1650 - 1572) 0.00183 Vtrue = 292 ft/sec The equivalent airspeed is Ve = 2( p0 - p) ρs = 2(1650 - 1572) 0.002377 Ve = 256 ft/sec 23 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.22 The altimeter measures pressure altitude. Thus, from Appendix A, p = 7.95 × l04 N/m2. Hence, ρ = p 7.95 ´ 104 = = 0.989 kg/m3 (287)(280) RT The relation between Vtrue and Ve is ρs / ρ Vtrue /Ve = Hence, Vtrue = 50 (1.225) / 0.989 = 56 m/sec 4.23 In the test section, a = γ RT = (1.4)(287)(270) = 329 m/sec M = V/a = 250/329 = 0.760 γ æ p0 γ - 1 2 ÷öγ -1 = çç1 + = [1 + 0.2(0.760)2 ]3.5 = 1.47 M ÷÷ çè ø p 2 Hence, p0 = 1.47 p = 1.47(1.01 ´ 105 ) = 1.48 ´ 105 N/m 2 4.24 p = 1.94 ´ 104 N/m 2 from Appendix A. γ -1 é ù 0.286 é ù êæ p ö γ ú ú 2 2 ê çæ 2.96 ´ 104 ÷÷ö 2 ÷ 0 ê ú ç ÷ ê çç - 1ú = - 1ú M1 = çç ÷÷ ÷ ê 4 ú 1.4 - 1 ê çè 1.94 ´ 10 ÷ø γ - 1 ê è p ø÷ ú êë úû ëê ûú M12 = 0.642 M1 = 0.801 γ 4.25 æ p0 γ - 1 2 ö÷γ -1 = çç1 + M ÷÷ ç è ø p 2 p0 = [1 + 0.2(0.65)2 ]3.5 = 1.328 p p = p0 2339 = = 1761 lb/ft 2 1.328 1.328 From Appendix B, this pressure corresponds to a pressure altitude, hence altimeter reading of 5000 ft. 24 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.26 At standard sea level, T = 518.69 R T0 γ -1 2 =1+ M = 1 + 0.2(0.96) 2 = 1.184 T 2 T0 = 1.184T = 1.184 (518.69) T0 = 614.3R = 154.3F 4.27 γ RT1 = a1 = (1.4)(287)(220) = 297 m/sec M1 = V1 / a1 = 596 /197 = 2.0 The flow is supersonic. Hence, the Rayleigh Pitot tube formula must be used. p02 p1 γ é (γ + 1)2 M 2 ù γ -1 é 1 - γ + 2γ M 2 ù 1 1 ú ú ê = êê ú ê ú 2 + γ 1 êë 4γ M1 - 2(γ - 1) úû êë úû p1 é ù 3.5 é 1 - 1.4 + 2(1.4)(2)2 ù (2.4)2 (2) 2 ê ú ê ú = ê ú ê ú 2 2.4 êë 4(1.4)(2) - 2(0.4) úû êë úû p02 = 5.64 p02 p1 p1 = 2.65 ´ 104 N/m 2 from Appendix A. Hence, p02 = 5.64(2.65 ´ 104 ) = 1.49 ´ 105 N/m 2 4.28 q = 1 1 æ γ p ö÷ γ æ p ö÷ 2 γ V2 ÷÷ ρ V 2 = p çç ÷÷V = p ρ V 2 = çç 2 2 çè γ p ø÷ 2 èç γ p ø÷ 2 a2 Hence: q = 4.29 q∞ = γ 2 γ 2 pM 2 p∞ M ∞ 2 = 0.7 p∞ M ∞ 2 (1) Use Appendix A to obtain the values of p∞ corresponding to the given values of h. Then use Eq. (1) above to calculate q∞. h(km) 60 2 p∞(N/m ) 25.6 M 17 2 q∞(N/m ) 5.2 × 10 50 40 87.9 299.8 9.5 3 5.6 × 10 30 1.19 × 10 5.5 3 6.3 × 10 20 3 3 7.5 × 10 3 5.53 × 103 1 3 3.9 × 103 Note that q∞ progressively increases as the shuttle penetrates deeper into the atmosphere, that it peaks at a slightly supersonic Mach number, and then decreases as the shuttle completes its entry. 25 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.30 Recall that total pressure is defined as that pressure that would exist if the flow were slowed isentropically to zero velocity. This is a definition; it applies to all flows — subsonic or supersonic. Hence, Eq. (4.74) applies, no matter whether the flow is subsonic or supersonic. γ /(γ -1) æ p0 γ - 1 2 ÷ö = çç1 + = [1 + 0.2(2)2 ]1.4/0.4 = 7.824 M ∞ ÷÷ çè ø p∞ 2 Hence: p0 = 7.824 p∞ = 7.824(2116) = 1.656 ´ 104 lb ft 2 Note that the above value is not the pressure at a stagnation point at the nose of a blunt body, because in slowing to zero velocity, the flow has to go through a shock wave, which is nonisentropic. The stagnation pressure at the nose of a body in a Mach 2 stream is the total pressure behind a normal shock wave, which is lower than the total pressure of the freestream, as calculated above. This stagnation pressure at the nose of a blunt body is given by Eq. (4.79). p02 p1 γ é (γ + 1) 2 M 2 ù γ -1 é 1 - γ + 2γ M 2 ù ∞ 1 ú = ú ê = êê ú ê ú 2 γ 1 + êë 4γ M 2 - 2(γ - 1) úû êë úû é ù1.4/0.4 é 1 - 1.4 + 2(1.4)(2) 2 ù (2.4)2 (2) 2 ê ú ê ú = 5.639 ê ú ê ú 2 2.4 4(1.4)(2) 2(0.4) ëê ûú ëê ûú Hence, p02 = 5.639 p∞ = 5.639(2116) = 1.193 ´ 104 lb ft 2 If Bernoulli’s equation is used, the following wrong result for total pressure is obtained. 1 γ ρ V∞ 2 = p∞ + p∞ M ∞ 2 2 2 2 4 lb p0 = 2116 + 0.7(2116)(2) = 0.804 ´ 10 2 ft p0 = p∞ + q∞ = p∞ + Compared to the correct result of 1.656 ´ 104 4.31 lb ft 2 , this leads to an error 51%. æ pe γ - 1 2 ö÷ -γ M e ÷÷ = çç1 + èç øγ - 1 p0 2 pe = 5(1.01 ´ 105 )[1 + 0.2(3) 2 ]-3.5 pe = 1.37 ´ 104 N/m 2 -1 æ Te γ - 1 2 ö÷ M e ÷÷ = [1 + 0.2(3)2 ]-1 = çç1 + çè ø T0 2 Te = (500)(0.357) = 178.6 K ρe = pe 1.37 ´ 104 = = 0.267 kg/m3 RTc (287)(178.6) 26 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. -γ 4.32 æ pe γ - 1 2 ö÷γ -1 M e ÷÷ = çç1 + ç è ø p0 2 Hence, 1-γ é ù êæ p ö γ ú 2 ÷ ê çç e ÷ M e2 = - 1úú ÷÷ ê çç γ - 1 ê è p0 ø ú êë úû M e2 = 5[(0.2)-0.286 - 1] = 2.92 M e = 1.71 æ A ö÷2 ççç e ÷÷ = èç A ø÷ t (γ +1)/(γ -1) 1 éê 2 æç γ - 1 ö÷ 2 ùú ÷ 1 M + ç ú γ ø÷÷ M e 2 ëêê γ + 1 èç ûú æ A ö2 1 [(0.833)(1 + 0.2 (1.71)2 )]6 ççç e ÷÷÷ = 2 çè At ÷ø (1.71) Ae = 1.35 At 4.33 -γ /(γ -1) é q γ p 2 γ γ -1 2ù M = M 2 ê1 + M ú = = 0.7M 2 (1 + 0.2M 2 )-3.5 êë úû p0 2 p0 2 2 M M2 q/p0 0 0 0 0.2 0.04 0.027 0.4 0.16 0.100 0.6 0.36 0.198 0.8 0.64 0.294 1.0 1.0 0.370 1.2 1.44 0.416 1.4 1.96 0.431 1.6 2.56 0.422 1.8 3.24 0.395 2.0 4.00 0.358 Note that the dynamic pressure increases with Mach number for M < 1.4 but decreases with Mach number for M > 1.4. I.e., in an isentropic nozzle expansion, there is a peak local dynamic pressure which occurs at M = 1.4. 27 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.34 First, calculate the value of the Reynolds number. Re L = ρ∞V∞ L (1, 225)(200)(3) = = 4.10 ´ 107 μ∞ (1.7894 ´ 10-5 ) The dynamic pressure is q∞ = 1 1 ρ∞V∞ 2 = (1.225)(200)2 = 2.45 ´ 104 N/m 2 2 2 δL = 5.2L = Re L Cf = 1.328 = Re L Hence, 5.2(3) = 0.0024 m = 0.24 cm 4.1 ´ 107 and 1.328 4.1 ´ 107 = 0.00021 The skin friction drag on one side of the plate is: D f = q∞ Sc f = (2.45 ´ 104 )(3)(17.5)(0.00021) D f = 270 N The total skin friction drag, accounting for both the top and the bottom of the plate is twice this value, namely Total Df = 540 N 4.35 δ = 0.37 L (Re L ) 0.2 = 0.37(3) (4.1 ´ 107 )0.2 = 0.033 m = 3.3 cm From Problem 4.24, we find δ turbulent /δ laminar = 3.3 = 13.75 0.24 The turbulent boundary layer is more than an order of magnitude thicker than the laminar boundary layer. Cf = 0.074 (Re L ) 0.2 = 0.074 (4.1 ´ 107 )0.2 = 0.0022 The skin friction drag on one side is then D f = q∞ Sc f = (2/45 ´ 104 )(3)(17.5)(0.0022) D f = 2830 N The total, accounting for both top and bottom is Total Df = 5660 N From Problem 4.24, we find ( D f turbulent ) /( D flaminar ) = 5660 = 10.5 540 The turbulent skin friction drag is an order of magnitude larger than the laminar value. 28 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.36 Rex cr = ρ∞V∞ xcr μ∞ æ μ ö (106 )(1.789 ´ 10-5 ) xcr = Re xcr ççç ∞ ÷÷÷ = çè ρ∞V∞ ø÷ (1.225)(200) xcr = 7.3 ´ 10-2 m The turbulent drag that would exist over the first 7.3 × 10−2 m of chord length from the leading edge (area A) is D fA = D fA = 0.074 (Recτ )0.2 0.074 (106 )0.2 q∞ S A (on one side) (2.45 ´ 104 )(7.3 ´ 10-2 )(17.5) D f A = 146 N (on one side) From Problem 4.25, the turbulent drag on one side, assuming both areas A and B to be turbulent, is 2830N. Hence, the turbulent drag on area B alone is: D f B = 2830 - 146 - 2684 N (turbulent) The laminar drag on area A is D fA = DfA D fA 1.328 q∞ S (Recr )0.5 1.328 (2.45 ´ 104 )(7.3 ´ 10-2 )(17.5) = (106 )0.5 = 42 N (laminar) Hence, the skin friction drag on one side, assuming area A to be laminar and area B to be turbulent is D f = D f A (laminar) + D f B (turbulent) D f = 42 + 2684 = 2726 N The total drag, accounting for both sides, is Total Df = 5452 N Note: By comparing the results of this problem with those of Problem 4.25, we see that the flow over the wing is mostly turbulent, which is usually the case for real airplanes in flight. 29 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.37 The relation between changes in pressure and velocity at a point in an inviscid flow is given by the Euler equation, Eq. (4.8) dp = -ρVdV Letting s denote distance along the streamline through the point, Eq. (4.8) can be written as dp dV = -ρ V ds ds dp (dV/V ) = -ρ V 2 ds ds or, (a) (dV/V ) = 0.02 per millimeter ds Hence, dp N = -(1.1)(100)2 (0.02) = 220 2 per millimeter ds m (b) dp N = -(1.1)(1000) 2 (0.02) = 22, 000 2 per millimeter ds m Conclusion: At a point in a high-speed flow, it requires a much larger pressure gradient to achieve a given percentage change in velocity than for a low speed flow, everything else being equal. 4.38 We use the fact that total pressure is constant in an isentropic flow. From Eq. (4.74) applied in the freestream. γ æ öγ -1 p0 γ -1 = ççç1 + = [1 + 0.2 (0.7)2 ]3.5 = 1.387 M ∞ 2 ÷÷÷ p∞ γ è ø÷ From Eq. (4.74) applied at the point on the wing, γ æ p0 γ - 1 2 ÷öγ -1 = çç1 + = [1 + 0.2 (1.1)2 ]3.5 = 2.135 M ÷÷ çè ø p 2 Hence, é æ p ö æ p öù æ 1.387 ö÷ p == 0.65 p∞ p = êê ççç 0 ÷÷÷ / ççç 0 ÷÷÷ úú p∞ = çç çè 2.135 ÷÷ø ∞ ÷ ÷ ç ëê è p∞ ø è p ø úû At a standard altitude of 3 km, from Appendix A, p∞ = 7.0121 ´ 104 N/m 2 . Hence, p = (0.65)(7.0121 ´ 104 ) = 4.555 ´ 104 N/m 2 4.39 This problem is simply asking what is the equivalent airspeed, as discussed in Section 4.12. Hence, 1/2 1/2 -3 ö æ ÷÷ö = (800) çç 1.0663 ´ 10 ÷÷ = 535.8ft.sec ç -3 ÷÷ ÷÷ èç 2.3769 ´ 10 ø÷ sø æ ρ Ve = V ççç èç ρ 30 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.40 (a) From Eq. (4.88) æ A ÷ö2 çç e ÷ = çèç A ÷÷ø t = γ +1 1 éê 2 æç γ - 1 2 ö÷ ùú γ -1 + 1 M e ÷÷ ç ø úû 2 M e 2 êë γ + 1 èç 6 1 ì ï 2 é ï 2 ùü ï ï + = 2.87 ´ 105 1 0.2 (10) êë úû ý 2í ï ï 2.4 (10) î ï ï þ Hence, Ae = At (b) 2.87 ´ 105 = 535.9 Form Eq. (4.87) γ æ p0 γ - 1 2 ÷öγ -1 = çç1 + = [1 + 0.2 (10)2 ]3.5 = 4.244 ´ 104 M e ÷÷ çè ø pe 2 At a standard altitude of 55 km, p = 48.373 N/m2. Hence, p0 = (4.244 ´ 104 )(48.373) = 2.053 ´ 106 N/m 2 = 20.3atm (c) From Eq. (4.85) T0 γ -1 2 =1+ M e = 1 + 0.2 (10)2 = 21 Te 2 At a standard altitude of 55 km, T = 275.78 K. Hence, T0 = 275.78 (21) = 5791 K Examining the above results, we note that: 1. The required expansion ratio of 535.9 is huge, but is readily manufactured. 2. The required reservoir pressure of 20.3 atm is large, but can be handled by proper design of the reservoir chamber. 3. The required reservoir temperature of 5791 K is tremendously large, especially when you remember that the surface temperature of the sun is about 6000 K. For a continuous flow hypersonic tunnel, such high reservoir temperatures can not be handled. In practice, a reservoir temperature of about half this value or less is employed, with the sacrifice made that “true temperature” simulation in the test stream is not obtained. 4.41 The speed of sound in the test stream is ae = γ RTe = (1.4)(287)(275.78) = 332.9 m/sec. Hence, Ve = M eae = 10(332.9) = 3329 m/sec 31 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.42 (a) From Eq. 4.88, for Me = 20 æ A ÷ö2 çç e ÷ = çèç A ÷÷ø t = γ +1 1 éê 2 æç γ - 1 2 ö÷ ùú γ -1 + 1 M e ÷÷ ç ø úû 2 M e 2 êë γ + 1 èç 6 ì ï 2 ï 2 ü 8 ï ï + [1 0.2 (20) ] ý = 2.365 ´ 10 2í ï ï 2.4 (20) î ï ï þ 1 Hence, Ae = 15,377 At (b) From Eq. (4.85) -1 æ T0 γ - 1 2 ÷ö = çç1 + M e ÷÷ = [1 + (0.2)(20) 2 ]-1 = 0.01235 çè ø Te 2 Hence, Te = (5791)(0.01235) = 71.5 K ae = γ RTe = (1.4)(287)(71.5) = 169.5 m/sec Ve = M eae = 20(169.5) = 3390 m/sec Comments: 1. To obtain Mach 20, i.e., to double the Mach number in this case, the expansion ratio must be increased by a factor of 15,377/535.9 = 28.7. High hypersonic Mach numbers demand wind tunnels with very large exit-to-throat ratios. In practice, this is usually obtained by designing the nozzle with a small throat area. 2. Of particular interest is that the exit velocity is increased by a very small amount, namely by only 61 m/sec, although the exit Mach number has been doubled. The higher Mach number of 20 is achieved not by a large increase in exit velocity but rather by a large decrease in the speed of sound at the exit. This is characteristic of most conventional hypersonic wind tunnels — the higher Mach numbers are not associated with corresponding increases in the test section flow velocities. 32 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.43 We will use the sketch shown in Figure 4.47, identifying the separate plan form areas A and B. (a) q∞ = 1 2 ρ∞V∞ 2 = 1 2 (1.23)(20) 2 = 246 N/m 2 ρ V x Re xcr = ∞ ∞ cr = 5 ´ 105 μ∞ Hence: xcr = μ∞ (5 ´ 105 ) (1.789 ´ 10-5 )(5 ´ 105 ) = = 0.3636 m (1.23)(20) ρ∞V∞ Assuming turbulent flow over areas A + B, C f A+ B = 0.074 Re L 0.2 Where Re L = ρ∞V∞ L (1.23)(20)(4) = = 5.5 ´ 106 -5 μ∞ (1.788 ´ 10 ) 0.074 C f A+ B = D f A+ B = 0.0032 (5.5 ´ 106 )0.2 = q∞ SC f = (246)(4)(4)(0.00332) = 13.07 N The turbulent drag on area A is obtained from C fA = 0.074 (Re xcr ) 0.2 = 0.074 (5 ´ 105 )0.2 = 0.00536 D f A = q∞ S C f A = (246)(4)(0.3636)(0.00536) = 1.92 N The turbulent drag on area B is D f B = D f A + B - D f A = 13.07 - 1.92 = 11.15 N The laminar drag on area A is obtained from C fA = 1.328 (Re xcr ) 0.5 = 1.328 (5 ´ 105 )0.5 = 0.00188 (Laminar) D f A = q∞ S C f A = (246)(4)(0.3636)(0.00188) = 0.67 N The total friction drag is D f = D f A + D f B = 0.67 + 11.15 = 11.82 N 33 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) V∞ = 40 m/sec q∞ = 1 Re L = 2 ρ∞ V∞ 2 ρ∞ V ∞ L μ∞ (Turbulent) 2 = 984 N/m 2 (1.23)(40)(4) = 11 ´ 106 1 = = 2 (1.23)(40) (1.789 ´ 10-5 ) C f A+ B = 0.074 Re L 0.2 = 0.074 = 0.00289 (11 ´ 106 )0.2 D f A + B = q∞ S C f A + B = (984)(4)(4)(0.00289) = 45.5 N (Turbulent) C fA = 0.074 (Re xcr ) 0.2 = 0.074 (5 ´ 105 )0.2 = 0.00536 Note that, since Re xcr remains the same, but V∞ is doubled, xcr is half that from part (a) 0.3636 = 0.1818 m 2 xcr = D f A = q∞ S C f A = (984)(4)(0.1818)(0.00536) = 3.84 N Hence, D f A = D f A + B - D f A = 45.5 - 3.84 = 41.66 N (Laminar) C f A = 1.328 (Re xcr ) 0.5 = 1.328 (5 ´ 105 )0.5 = 0.00188 D f A = q∞ S C f A = (984)(4)(0.1818)(0.00188) = 1.345 N Thus, D f = D f A + D f B = 1.345 + 41.66 = 43 N (c) n D f ∝ V¥ Using the results from parts (a) and (b) D fa D fb æ V ö÷n = ççç a ÷÷ çè V ø÷ b æ 20 ön 11.82 = çç ÷÷÷ çè 40 ø 43 0.275 = (0.5)n Taking the log of both sides −0.56 = n (−0.30) 0.56 n= = 1.87 0.30 Note: Skin friction drag does not follow the velocity squared law; rather skin friction varies with velocity at a power slightly less than 2. 34 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.44 (a) For turblent flow, C f ∝ 1 Re 0.2 . Since, Re = ρ∞V∞ L 1 , then C f ∝ 0.2 μ V¥ æ 1 ÷ö ç D f = q∞ S C f ∝ V∞ 2 çç 0.2 ÷÷÷ çè V∞ ÷ø or, Df ∝ V∞1.8 (b) For laminar flow, C f ∝ 1 Re 0.5 ∝ 1 V∞ 0.5 æ ö 2 çç 1 ÷÷ D f ∝ V¥ ç 0.2 ÷÷ çè V¥ ÷ø or, Df ∝ V∞1.5 4.45 (a) M∞ = 1. Since a∞ = 340.3 m/sec at sea level, V∞ = M∞ a∞ = (1)(340.3)=340.3 m/sec q¥ = 1 Re L = C finc = 2 2 ρ V∞ = 1 2 (1.23)(340.3) 2 = 7.12 ´ 104 N/m 2 ρ∞V∞ L (1.23)(340.3)(4) = = 9.36 ´ 107 -5 μ∞ (1.789 ´ 10 ) 0.074 Re L 0.2 = 0.074 (9.36 ´ 107 )0.2 = 0.00188 From Figure 4.44, for the turbulent case, approximate reading of the graph shows, for M∞ = 1, Cf C finc = 0.91 Thus, Cf = 0.91(0.00188) = 0.00171 Df = q∞ S Cf (7.12 × 104)(4)(4)(0.00171) D f = 1948 N 35 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) M∞ = 3 V∞ = M ∞ a∞ = 3(340.3) = 1021m/sec q∞ = 1 2 ρ∞V∞ 2 = 1 2 (1.23)(1021) 2 = 6.41 ´ 105 N/m 2 ρ∞V∞ L (1.23)(1021)(4) = = 2.81 ´ 108 μ∞ (1.789 ´ 10-5 ) Re L = C finc = 0.074 (2.81 ´ 108 )0.2 = 0.00151 From Figure 4.44, for the turbulent case, approximate reading of the graph shows, for M∞ = 3, Cf C finc = 0.56 C f = 0.56(0.00151) = 0.000846 D f = q∞ S C f = (6.41 ´ 105 )(4)(4)(0.000846) D f = 8677 N (c) D f1 D f2 æ V ön = ççç 1 ÷÷÷ çè V2 ø÷ æ 340.3 ö÷n 1948 = çç çè 1020.9 ø÷÷ 8677 0 .2245 = (0.333)n −0.6488 = n (−0.4772) -0.6488 n= = 1.36 -0.4772 1.36 This implies D f ∝ V¥ . This is considerably different than the velocity squared law. In fact, comparing this result, where n = 1.36, with the incompressible result in Problem 4.43, where n = 1.87, indicates that the added effect of compressibility (higher Mach numbers) continues to drive down the exponent. The comparison is only qualitative, however, because the Reynolds numbers in Problem 4.45 are much larger than those in Problem 4.43. In any event, the bottom line of Problems 4.43,4.44, and 4.45 is that flows with friction and/or compressibility do not follow the velocity squared law, but rather for such flows, the skin friction drag varies as V∞n where n is an exponent less than 2. 4.46 (a) The waves travel at the local speed of sound. a = γ RT = (1.4)(287)(288) = 340.2 m/sec. This speed is relative to the gas. Since the gas velocity is zero, then this is also the wave velocity relative to the pipe. One wave travels to the right along the positive x-axis with the velocity 340.2 m/sec, and the other wave travels to the left along the negative x-axis with a velocity of −340.2 m/sec. 36 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) The x-location of the right-running wave at t = 0.2 sec is x = at = (340.2)(0.2) = 68 m The x-location of the left-running wave at t = 0.2 sec is x = at = (−340.2)(0.2) = −68 m 4.47 The waves still travel at the local speed of round relative to the gas. Since the gas itself is moving relative to the pipe, then the wave speed relative to the pipe is the sum of the wave speed relative to the gas and the speed of the gas relative to the pipe. The velocity of rightrunning wave is therefore Vwave = Vgas + wave speed (a) When Vgas = 30 m/sec, Vwave = 30 + 340.2 = 370.2 m/sec The right-running wave travels to the right at 370.2 m/sec relative to the stationary pipe. After 0.2 sec, the x-location of this wave is x = (370.2)(0.2) = 74 m The left-running wave travels to the left at the velocity Vwave = 30 − 340.2 = −310.2 m/sec After 0.2 sec, the x-location of this left-running wave is x = (−310.2)(0.2) = −62 m (b) The flow velocity relative to the pipe is 400 m/sec, which is faster than the speed of sound. The weak pressure distributions, however, continue to propagate to the right and left at the speed of sound relative to the gas. Thus, the right-running wave has a velocity relative to the pipe of Vwave = 400 + 340.2 = 740.2 m/sec After 0.2 sec, the location of this wave is: x = (740.2) 0.2 = 148.02 m The left-running wave has a velocity relative to the pipe of Vwave = 400 − 340.2 = 59.8 m/sec After 0.2 sec, the location of this wave is x = (59.8) (0.2) = 11.96 m Note: The left-running wave, although it is traveling along to the left at the speed of sound relative to the gas, is moving to the right relative to the pipe because the flow velocity in the pipe is higher than the speed of sound. 37 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.48 The element of air initially has a pressure and density at the standard altitude of 1000 m of, from Appendix A, p1 = 8.9876 × 104 N/m2 and ρ1 = 1.1117 kg/m3 At a standard altitude of 2000 m, p2 = 7.9501 × 104 N/m2. The density of the element of air, assuming it has experienced an isentropic process, is, from Eq. (4.37) 1 1 æ 7.9501 ´ 104 ÷ö1.4 æ p öγ ÷÷ ρ2 = ρ1 ççç 2 ÷÷÷ = 1.1117 ççç çè 8.9876 ´ 104 ÷ø÷ èç p1 ø÷ ρ2 = 1.0184 kg/m3 Comparing with the standard density at 2000 m of 1.0066 kg/m3, we see that the raised element of air has a higher density and is therefore heavier than its surrounding neighbors. This situation is a stable atmosphere because the isentropically perturbed element will tend to sink back down to its originally lower altitude. 4.49 A1V1 = A2V2 V1 = A2 0.5 V = (120) = 15 mph A1 2 4 From the answer to Problem 2.15, 60 mph = 26.82 m/sec. 26.82 = (15) = 6.705 m/sec V1 = 60 4.50 p1 + 1 2 ρ V12 = p2 + 1 2 ρ V22 ( p2 = p1 + 1 2 ρ V12 − V22 ) p1 = 1 atm = 1.01 × 105 N/m 2 ρ = 1.23 kg/m3 V1 = 6.705 m/sec 26.82 = 53.64 m/sec V2 = (120) 60 p2 = 1.01 × 105 + 1 2 (1.23)[(6.705)2 − (53.64)2 ] p2 = 0.99258 × 105 N/m 2 38 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.51 Let x be the distance along the diffuser, and hD the height at the diffuser entrance. At any location x, the distance from the top to the bottom wall is hD + 2x tan θ where θ is the angle of the wall. Thus, the cross-sectional area at any location x is A = (2) [hD + 2 x tan θ ] Thus, dA = 4 tan θ = 4 tan15° = 1.0718 m dx 4.52 The flow velocity at the entrance to the diffuser is the same as in the test section V2 = 120 mph = 53.64 m/sec At the exit of the diffuser, since V2 A2 = V3 A3 A 0.5 (53.64) = 7.66 m/sec V3 = 2 V2 = 3.5 A3 4.53 AV = const dv dA +V =0 dx dx dv V dA =− dx A dx A From the solution of Problem 4.51, dA = 1.0718 m dx Thus, dV V = −1.0718 A dx (a) At the entrance, V2 = 53.64 m/sec (from Prob. 4.52) A2 = (0.5)(2) = 1 m 2 dV 53.64 = −1.0718 = −57.49 sec −1 1 dx (b) At the exit, V3 = 7.66 m/sec (from Prob. 4.52) V dV 7.66 = −1.0718 3 = −1.0718 = −1.173 sec −1 7 dx A3 39 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.54 From the Euler equation, Eq. (4.8) in the text, dp = − ρVdV dp dV = − ρV dx dx (a) At the inlet, from the solutions of Problems 4.52 and 4.53, V2 = 53.64 m/sec and dV = −57.49 sec −1 dx Thus, dp = −(1.23)(53.64)( −57.49) = 3.793 × 103 N/m3 dx (b) At the exit, V3 = 7.66 m/sec and dV = −1.173 sec −1 dx Thus, dp = −(1.23)(7.66)( −1.173) = 11.05 N/m3 dx 4.55 tan 15° = (3.5 − 0.5) / 2 1.5 = x x x= 1.5 1.5 = = 5.6 m tan15° 0.2679 4.56 From the solution of Problem 4.54, dp 3 3 = 3.793 × 10 N/m dx 2 dp 3 = 11.05 N/m dx 3 3.793 × 103 + 11.05 N dp = = 1902 dx ave 2 m2 xs = 183 183 = = 0.096 m 1902 dp dx ave 4.57 From the solution of Problem 4.56, (xs)laminar = 0.096 m. −1 ( xs )turbulent = ( xs )laminar dp 506 dx ave −1 dp 183 dx ave = 2.765 ( xs )turbulent = (2.765)(0.096) = 0.265 m 40 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.58 At h = 7,500 ft, from App. B, T∞ = 491.95oR, p∞ = 1602.3 lb/ft2, and ∞ = 1.8975 × 10–3 slug/ft3. a∞ = γ RT∞ = (1.4)(1716)(491.95 = 1087 ft/sec 88 V∞ = 229 mph = 335.9 ft/sec 60 M∞ = V∞ 335.9 = = 0.309 a∞ 1087 p0 = ρ∞ + 1 2 ρ∞V∞2 = 1602.3 + (0.5)(1.8975 × 10−3 )(335.9)2 = 1709 lb/ft 2 4.59 At h = 25,000 ft, from App. B, T∞ = 429.64oR, p∞ = 786.33 lb/ft2, and ∞ =1.0663 × 10–3 slug/ft3. a∞ = γ RT∞ = (1.4)(1716)(429.64) = 1016 ft/sec 88 V∞ = 610 = 894.67 ft/sec 60 M∞ = V∞ 894.67 = = 0.88 a∞ 1016 The flow is subsonic, but compressible. From Eq. (4.74), γ p0 γ − 1 2 γ −1 M∞ = 1 + p∞ 2 p0 = [1 + 0.2(0.88)2 ]3.5 = (1.15488)3.5 = 2.303 p∞ ρ0 = 2.303 p∞ = 2.303 (786.33) = 1811 41 lb ft 2 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 4.60 At h = 35,000 ft, from App. B, T∞ = 394.08oR, p∞ = 499.34 lb/ft2, and ∞ = 7.382 × 10–4 slug/ft3. a∞ = γ RT∞ = (1.4)(1716)(394.08) = 973 ft/sec 88 V∞ = 1328 = 1947.7 ft/sec 60 V 1947.7 M∞ = ∞ = = 2.00 a∞ 973 The flow is supersonic. From Eq. (4.79), γ (γ + 1)2 M ∞2 γ −1 1 − γ + 2γ M ∞2 = p∞ 4γ M ∞2 − 2(γ − 1) γ +1 p02 1.4 0.4 1 − 1.4 + 2(1.4)(2) 2 (2.4) 2 (2)2 = = 5.64 2 2.4 4(1.4) (2) − 2(0.4) p02 = 5.64(499.34) = 2817 lb/ft 2 42 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 5 5.1 Assume the moment is governed by M = f (V∞ , ρ∞ , S , μ∞ , a∞ ) More specifically: M = Z (V∞ a , ρ∞b , S d , a∞e , μ∞ f ) Equating the dimensions of mass, m, length, ℓ, and time t, and considering Z dimensionless, æ ö÷a æç m ö÷b 2 çç ÷ ç ÷ = çè t ø÷ çè 3 ø÷ t2 m2 d æ öe æ ( ) çç èç t ÷÷ çç m ö÷÷ ø÷ çè t ÷ø f 1 = b + f (For mass) 2 = a – 3b + 2d + e – f (For length) −2 = −a − e − f (for time) Solving a, b, and d in terms of e and f, and, b=1−f a=2−e−f and, 2 = 2 − e − f − 3 + 3f + 2d + e − f or 0 = −3 + f + 2d d = Hence, 3- f 2 M = Z V∞ 2-e- f ρ∞1- f S (3- f ) / 2 a∞ e μ∞ f 2 = Z V∞ ρ∞ SS ö÷ f ö÷e æç μ ∞ ÷ ÷÷ çç 1/2 ÷÷÷ ÷ ç ø V ρ S è ø ∞ ∞ ∞ æ çç èç V 1/2 ç a∞ Note that S l/2 is a characteristic length; denote it by the chord, c. æ a öc æ μ öf 2 ∞ ÷÷ M = ρ∞ V¥ S c Z ççç ∞ ÷÷÷ ççç ÷ èç V∞ ø÷ èç V∞ ρ∞c ø÷ However, a∞ /V∞ = 1/M ∞ and μ∞ 1 = Re V∞ ρ∞c Let æ 1 ö÷e æ 1 ö f ÷÷ = cm ÷÷ çç Z ççç ç ÷ 2 èç M ∞ ø è Re ÷ø where cm is the moment coefficient. Then, as was to be derived, we have M = or, 1 ρ∞ V∞ 2c cm 2 M = q∞ S c cm 43 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.2 From Appendix D, at 5° angle of attack, c = 0.67 cmc/4 = -0.025 (Note: Two sets of lift and moment coefficient data are given for the NACA 1412 airfoil—with and without flap deflection. Make certain to read the code properly, and use only the unflapped data, as given above. Also, note that the scale for cmc/4 is different than that for cℓ—be careful in reading the data.) With regard to cd, first check the Reynolds number, Re = ρ∞V∞c (0.002377)(100)(3) = μ∞ (3.7373 ´ 10-7 ) Re = 1.9 ´ 106 In the airfoil data, the closest Re is 3 × 106. Use cd for this value. cd = 0.007 (for c = 0.67) The dynamic pressure is q∞ = 1 1 ρ∞V∞ 2 = (0.002377)(100) 2 = 11.9lb/ft 2 2 2 The area per unit span is S = 1(c) = (1)(3) = 3ft 2 Hence, per unit span, L = q∞ S c = (11.9)(3)(0.67) = 23.9 lb D = q∞ S cd = (11.9)(3)(0.007) = 0.25lb M c/4 = q∞ S c cmc/4 = (11.9)(3)(3)(-0.025) = -2.68 ft.lb 5.3 ρ∞ = p∞ (1.01 ´ 105 ) = RT∞ (287)(303) = 1.61kg/m3 From Appendix D, c = 0.98 cmc/4 = -0.012 Checking the Reynolds number, using the viscosity coefficient from the curve given in Chapter 4, μ∞ = 1.82 ´ 10-5 kg/m sec at T = 303 K, ρ V c (11.57)(42)(0.3) Re = ∞ ∞ = = 8 ´ 105 5 μ∞ 1.82 ´ 10 This Reynolds number is considerably less than the lowest value of 3 × 106 for which data is given for the NACA 23012 airfoil in Appendix D. Hence, we can use this data only to give an educated guess; use cd ≈ 0.01, which is about 10 percent higher than the value of 0.009 given for Re = 3 × 106 The dynamic pressure is 1 1 q∞ = ρ∞V∞ 2 = (1.161)(42)2 = 1024 N/m 2 2 2 The area per unit span is S = (1)(0.3) = 0.3m 2 . Hence, L = q∞ S c = (1024)(0.3)(0.98) = 301N D = q∞ S cd = (1024)(0.3)(0.01) = 3.07 N M c/4 = q∞ S c cm = (1024)(0.3)(0.3)(-0.012) = -1.1Nm 44 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. From the previous problem, q∞ = 1020 N/m2 5.4 L = q∞ S c Hence, L q∞ S c = The wing area S = (2)(0.3) = 0.6 m 2 Hence, c = 200 = 0.33 (1024)(0.6) From Appendix D, the angle of attack which corresponds to this lift coefficient is α = 2 From Appendix D, at α = 4, 5.5 c = 0.4 Also, æ 88 ö V∞ = 120 çç ÷÷÷ = 176ft/sec çè 60 ø q∞ = 1 1 ρ∞ V∞ 2 = (0.002377)(176)2 = 36.8lb/ft 2 2 2 L = q∞ S c L 29.5 S = = = 2 ft 2 q∞c (36.8)(0.4) L = q∞ S c 5.6 D = q∞ S cd Hence, L q Sc c = ∞ = D q∞ S cd cd We must tabulate the values of cℓ /cd for various angles of attack, and find where the maximum occurs. For example, from Appendix D, at α = 00 , c = 0.25 cd = 0.006 Hence L c 0.25 = = = 4.17 D cd 0.006 A tabulation follows. α 0° 1° 2° 3° 4° 5° 6° 7° 8° 9° cℓ 0.25 0.35 0.45 0.55 0.65 0.75 0.85 0.95 1.05 1.15 cd 0.006 0.006 0.006 0.0065 0.0072 0.0075 0.008 0.0085 0.0095 0.0105 cℓ 41.7 58.3 75 84.6 90.3 100 106 112 111 110 cd From the above tabulation, æ L ö÷ çç ÷ » 112 çè D ø÷ max 45 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.7 At sea level ρ∞ = 1.225 kg/m3 ρ∞ = 1.01 ´ 105 N/m 2 Hence, q∞ = 1 1 ρ∞V∞ 2 = (1.225)(50) 2 = 1531 N/m 2 2 2 From the definition of pressure coefficient, Cp = 5.8 p - p∞ (0.95 - 1.01) ´ 105 = = -3.91 q∞ 1531 The speed is low enough that incompressible flow can be assumed. From Bernoulli’s equation, 1 1 ρ V∞ 2 = p∞ + ρ∞V∞ 2 = p∞ + q∞ 2 2 1 1 q∞ - ρV 2 ρV 2 p - p∞ 2 2 Cp = = = 11 q∞ q∞ ρ∞ V∞ 2 2 p+ Since ρ = ρ∞(constant density) æ V ö÷2 æ 62 ö2 ÷÷ = 1 - çç ÷÷ = 1 - 1.27 = -0.27 C p = ççç çè 55 ø÷ çè V∞ ø÷ 5.9 The flow is low speed, hence assumed to be incompressible. From Problem 5.8, æ V ö÷2 æ 195 ÷ö2 ÷÷ = 1 - çç C p = 1 - ççç = -0.485 çè 160 ø÷÷ èç V∞ ø÷ 5.10 The speed of sound is a∞ = γ RT∞ = M∞ = V∞ 700 = = 0.63 a∞ 1107 (1.4)(1716)(510) = 1107 ft/sec Hence, In Problem 5.9, the pressure coefficient at the given point was calculated as −0.485. However, the conditions of Problem 5.9 were low speed, hence we identify C p0 = -0.485 At the new, higher free stream velocity, the pressure coefficient must be corrected for compressibility. Using the Prandtl-Glauert Rule, the high speed pressure coefficient is Cp = C p0 1 - M ∞2 = -0.485 1 - (0.63) 2 46 = -0.625 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.11 The formula derived in Problem 5.8, namely æ V ö÷2 ÷ , C p = 1 - ççç çè V∞ ø÷÷ utilized Bernoulli’s equation in the derivation. Hence, it is not valid for compressible flow. In the present problem, check the Mach number. a∞ = M∞ = γ RT∞ = (1.4)(1716)(505) = 1101 ft/sec 780 = 0.708. 1101 The flow is clearly compressible! To obtain the pressure coefficient, first calculate ρ∞ from the equation of state. p∞ 2116 = = 0.00244 slug/ft 3 RT∞ (1716)(505) ρ∞ = To find the pressure at the point on the wing where V = 850 ft/sec, first find the temperature from the energy equation c pT + V2 V 2 = c pT∞ + ∞ V 2 V 2 -V2 T = T∞ + ∞ 2c p The specific heat at constant pressure for air is cp = γR = γ -1 (1.4)(1716) ft lb = 6006 (1.4 - 1) slug R Hence, T = 505 + 7802 - 8502 = 505 - 9.5 = 495.5 R 2(6006) Assuming isentropic flow γ æ T ö÷γ -1 p ÷ = ççç çè T∞ ÷÷ø p æ 495.5 ÷ö3.5 p = (2116) çç = 1980 lb/ft 2 çè 505 ÷÷ø From the definition of Cp p - p∞ p - p∞ 1980 - 2116 = = 1 1 2 q∞ ρ∞ V∞ (0.00244)(780)2 2 2 C p = -0.183 Cp = 47 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.12 A velocity of 100 ft/sec is low speed. Hence, the desired pressure coefficient is a low speed value, C p0 . Cp = C p0 1 - M ∞2 From problem 5.11, C p = -0.183 and M ∞ = 0.708. Thus, 0.183 = C p0 1 - (0.708)2 C p0 = (-0.183)(0.706) = -0.129 5.13 Recall that the airfoil data in Appendix D is for low speeds. Hence, at α = 4, c 0 = 0.58. Thus, from the Prandtl-Glauert rule, c = c 0 1 - M∞ 2 = 0.58 1 - (0.8)2 = 0.97 5.14 The lift coefficient measured is the high speed value, c . Its low speed counterpart is c 0 , where c = c 0 1 - M ∞2 Hence, c 0 = (0.85) 1 - (0.7)2 = 0.607 For this value, the low speed data in Appendix D yield α = 2 48 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.15 First, obtain a curve of Cp,cr versus M∞, from 2 C p,cr = γ M ∞2 γ /(γ -1) éæ ù ê ç 2 + (γ - 1)M ∞2 ö÷ ú ÷÷ ê çç ú 1 ê çè ú γ +1 ÷÷ø êë úû Some values are tabulated below for γ = 1.4 . M∞` 0.4 0.5 0.6 0.7 0.8 0.9 1.0 Cp,cr −3.66 −2.13 −1.29 −0.779 −0.435 −0.188 0 Now, obtain the variation of the minimum pressure coefficient, Cp, with M∞, where C p0 = -0.90. From the Prandtl-Glauert rule, Cp = Cp = C p0 1 - M ∞2 -0.90 1 - M ∞2 Some tabulated values are: M∞ Cp 0.4 −0.98 0.5 −1.04 0.6 −1.125 0.7 −1.26 0.8 −1.5 0.9 −2.06 A plot of the two curves is given on the next page. From the intersection point, M cr = 0.62 49 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.16 The curve of Cp, cr versus M∞ has already been obtained in the previous problem; it is a universal curve, and hence can be used for this and all other problems. We simply have to obtain the variation of Cp with M∞ from the Prandtl-Glauert rule, as follows: Cp = M∞ Cp C p0 1 - M∞ 0.4 −0.71 2 = 0.5 −0.75 -0.65 1 - M ∞2 0.6 −0.81 0.7 −0.91 0.8 −1.08 0.9 −1.49 The results are plotted below. From the point of intersection, M cr = 0.68 Please note that, comparing Problems 5.15 and 5.16, the critical Mach number for a given airfoil is somewhat dependent on angle of attack for the simple reason that the value of the minimum pressure coefficient is a function of angle of attack. When a critical Mach number is stated for a given airfoil in the literature, it is usually for a small (cruising) angle of attack. 5.17 Mach angle = μ = arc sin (1/M) μ = arc sin (1/2) = 30° 50 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.18 æ 1 èç M μ = Sin-1 çç d = h/Tanμ = ö÷ -1 æ 1 ö ÷ = Sin ççç ÷÷÷ = 23.6 ø÷ è 25 ø 10km = 22.9 km 0.436 5.19 At 36,000 ft, from Appendix B, T∞ = 390.5R ρ∞ = 7.1 ´ 10-4 slug/ft 3 Hence, a∞ = γ RT∞ = (1.4)(1716)(390.5) = 969 ft/sec V∞ = a∞ M ∞ = (969)(2.2) = 2132 ft/sec 1 1 ρ∞V∞ 2 = (7.1 ´ 10-4 )(2132) 2 = 1614 lb/ft 2 2 2 In level flight, the airplane’s lift must balance its weight, hence L = W = 16,000 lb. From the definition of lift coefficient, q∞ = CL = L/q∞ S = 16, 000 /(1614)(210) = 0.047 Assume that all the lift is derived from the wings (this is not really true because the fuselage and horizontal tail also contribute to the airplane lift.) Moreover, assume the wings can be approximated by a thin flat plate. Hence, the lift coefficient is given approximately by CL = 4α M ∞2 - 1 Solve for α, 1 1 CL M ∞2 - 1 = (0.047) (2.2)2 - 1 4 4 α = 0.023 radians (or 1.2 degrees) α = The wave drag coefficient is approximated by CDw = Hence, 4α M ∞2 - 1 = 4(0.023)2 (2.2)2 - 1 = 0.00108 Dw = q∞ S CDw = (1614)(210)(0.00108) Dw = 366 lb 51 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.20 (a) At 50,000 ft, ρ ∞ = 3.6391 × 10−4 slug/ft3 and T∞ = 390°R. Hence, γ RT∞ = a∞ = and (1.4)(1716)(390) = 968 ft/sec V∞ = a∞ M ∞ = (968)(2.2) = 2130 ft/sec The viscosity coefficient at T∞ = 390°R = 216.7 K can be estimated from an extrapolation of the straight line given in Fig. 4.30. The slope of this line is dμ (2.12 - 1.54) ´ 10-5 kg = = 5.8 ´ 10-8 dT (350 - 250) (m)(sec)(K) Extrapolating from the sea level value of μ = 1.7894 ´ 10-5 kg/(m)(sec), we have at T∞ = 216.7 K. μ∞ = 1.7894 ´ 10-5 - (5.8 ´ 10-8 )(288 - 216.7) μ∞ = 1.37 ´ 10-5 kg/(m)(sec) Converting to English engineering units, using the information in Chapter 4, we have μ∞ = ö 1.37 ´ 10-5 æç slug -7 slug ÷÷ 3.7373 10 ´ = 2.86 ´ 10-7 ç ÷ -5 ççè ÷ ft sec ø ft sec 1.7894 ´ 10 Finally, we can calculate the Reynolds number for the flat plate: Re L = ρ∞V∞ L 3.6391 ´ 10-4 (2130)(202) = = 5.47 ´ 108 μ∞ 2.86 ´ 10-7 Thus, from Eq. (4.100) reduced by 20 percent C f = (0.8) 0.07 (Re L ) 0.2 = (0.8) 0.074 (5.74 ´ 108 )0.2 = 0.00106 The wave drag coefficient is estimated from cd ,w = where α = Thus, 4α 2 M ∞2 - 1 2 = 0.035 rad. 57.3 cd ,w = 4(0.035) 2 (2.2)2 - 1 = 0.0025 Total drag coefficient = 0.0025 + (2) (0.00106) = 0.00462 Note: In the above, Cf is multiplied by two, because Eq. (4.100) applied to only one side of the flat plate. In flight, both the top and bottom of the plate will experience skin friction, hence that total skin friction coefficient is 2(0.00106) = 0.00212. (b) If α is increased to 5 degrees, where α = 5/57.3 − 0.00873 rad, then cd ,w = 4(0.0873)2 (2.2)2 - 1 = 0.01556 Total drag coefficient = 0.01556 + 2(0.00106) = 0.0177 52 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (c) In case (a) where the angle of attack is 2 degrees, the wave drag coefficient (0.0025) and the skin friction drag coefficient acting on both sides of the plate (2 × 0.00106 = 0.00212) are about the same. However, in case (b) where the angle of attack is higher, the wave drag coefficient (0.0177) is about eight times the total skin friction coefficient. This is because, as α increases, the strength of the leading edge shock increases rapidly. In this case, wave drag dominates the overall drag for the plate. æ km ö÷æç 1h ö÷æç 1000m ö÷ ÷÷ç 5.21 V∞ = 251 km/h = çç 251 ÷ç ÷ = 69.7 m/sec çè h ÷øççè 3600sec ø÷èç 1km ø÷ ρ∞ = 1.225 kg/m3 1 1 ρ∞ V∞ 2 = (1.225)(69.7) 2 = 2976 N/m 2 2 2 L 9800 CL = = = 0.203 q∞ S (2976)(16.2) q∞ = CDi = CL 2 (0.203)2 = = 0.002894 π e AR π (0.62)(7.31) Di = q∞ S CDi = (2976)(16.2)(0.002894) = 139.5 N 5.22 V∞ = 85.5 km/h = 23.75 m/sec 1 1 ρ∞ V∞ 2 = (1.225)(23.75)2 = 345 N/m 2 2 2 L 9800 CL = = = 1.75 q∞ S (345)(16.2) q∞ = CDi = CL 2 (1.75)2 = = 0.215 π eAR π (0.62)(7.31) Di = q∞ S CDi = (345)(16.2)(0.215) = 1202 N Note: The induced drag at low speeds, such as near stalling velocity, is considerably larger than at high speeds, near maximum velocity. Compare the results of Problems 5.20 and 5.21. 5.23 First, obtain the infinite wing lift slope. From Appendix D for a NACA 65-210 airfoil, C = 1.05 at α = 8 C = 0 at α L = 0 = -1.5° Hence, a0 = 1.05 - 0 = 0.11 per degree 8 - (-1.5) The lift slope for the finite wing is a = a0 0.11 = = 0.076 degree 57.3 a0 57.3(0.11) 1+ 1+ π (9)(5) π ei AR At α = 6°, CL = a(α - α L = 0 ) = (0.076)[6 - (-1.5)] = 0.57 The total drag coefficient is CL 2 (0.57)2 = (0.004) + π eAR π (0.9)(5) = 0.004 + 0.023 = 0.027 CD = cd + CD 53 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.24 q∞ = 1 1 ρ∞ V∞ 2 = (0.002377)(100)2 = 11.9 lb/ft 2 2 2 at α = 10°, L = 17.9 lb. Hence L 17.9 = = 1.0 q∞ S (11.9)(1.5) CL = at α = −2°, L = 0 lb. Hence αL = 0 = −2° dCL 1.0 - 0 = = 0.083 per degree dα [10 - (-2)] a = This is the finite wing lift slope. a = a0 57.3 a0 1+ π e AR Solve for aο. a0 = a 0.083 = 57.3 a 57.3(0.083) 11+ π e AR π (0.96)(6) a0 = 0.11 per degree 54 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.25 At α = −1°, the lift is zero. Hence, the total drag is simply the profile drag. CL 2 = cd + 0 = cd π eAR 1 1 = ρ∞ V∞2 = (0.002377)(130)2 = 20.1 lb/ft 2 2 2 CD = cd + q∞ Thus, at α = α L = 0 = -1° cd = D 0.181 = = 0.006 q∞ S (20.1)(1.5) At α = 2°, assume that cd has not materially changed, i.e., the “drag bucket” of the profile drag curve (see Appendix D) extends at least from −1° to 2°, where cd is essentially constant. Thus, at α = 2°, CL = L 5 = = 0.166 q∞ S (20.1)(1.5) CD = D 0.23 = = 0.00763 q∞ S (20.1)(1.5) However: CD = cd + CL 2 π eAR 0.00763 = 0.006 + (0.166)2 0.00146 = 0.006 + π e(6) e e = 0.90 To obtain the lift slope of the airfoil (infinite wing), first calculate the finite wing lift slope. (0.166 - 0) = 0.055 per degree [2 - (-2)] a 0.055 a0 = = 57.3a 57.3(0055) 11π eAR π (0.9)(6) a = a0 = 0.068 per degree 5.26 Vstall = 2W = ρ∞ S CLmax 2(7780) (1.225)(16.6)(2.1) Vstall = 19.1 m/sec = 68.7 km/h 55 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.27 (a) α = 5 = 0.087 radians 57.3 c = 2πα = 2π (0.087) = 0.548 (b) Using the Prandtl-Glauert rule, c = (c) c 0 1 - M ∞2 = 0.548 1 - (0.7)2 = 0.767 From Eq. (5.50) c = 4α 2 M∞ - 1 = 4(0.087) (2)2 - 1 = 0.2 5.28 For V∞ = 21.8 ft/sec at sea level 1 1 q∞ = ρ∞ V∞ 2 = (0.002377)(21.8)2 = 0.565 lb/ft 2 2 2 1 ounce = 1/16 lb = 0.0625 lb. L 0.0625 CL = = = 0.11 q∞ S (0.565)(1) For a flat plate airfoil c = 2πα = 2 ⋅ π (3 / 57.3) = 0.329 The difference between the higher value predicted by thin airfoil theory and the lower value measured by Cayley is due to the low aspect ratio of Cayley’s test wing, and viscous effects at low Reynolds number. 5.29 From Eqs. (5.1) and (5.2), writtten in coefficient form CL = CN cos α − CA sin α CD = CN sin α + CA cos α Hence: CL = 0.8 cos 6° - 0.06 sin 6° = 0.7956 - 0.00627 = 0.789 CD = 0.8 sin α + 0.06 cos α = 0.0836 + 0.0597 = 0.1433 Note: At the relatively small angles of attack associated with normal airplane flight, CL and CN are essentially the same value, as shown in this example. 56 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.30 First solve for the angle of attack and the profile drag coefficient, which stay the same in this problem cL = a α = or, a0 α 1 + 57.3 a0 /(π e1 AR) CL [1 + 57.3 a0 / π e1 AR] a0 0.35 = {1 + 57.3(0.11)/[π (0.9)(7)]} = 4.2° 0.11 α = The profile drag can be obtained as follows CL 0.35 CD = = = 0.012 (CL / CD ) 29 or, CD = cd + CL2 π e AR cd = CD - CL2 (0.35)2 = 0.012 = 0.0062 π e AR π (.9)(7) Increasing the aspect ratio at the same angle of attack increases CL and reduces CD. For AR = 10, we have a0 α CL = a α = 1 + 57.3 a0 /(π e1 AR) = (0.11)(4.2) = 0.3778 1 + 57.3(0.11)/[π (0.9)(10)] CD = cd + CL2 (0.3778)2 = 0.062 = 0.0062 + 0.005048 = 0.112 π e AR π (.9)(10) Hence, the new value of L/D is CL 0.3778 = = 33.7 CD 0.0112 57 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.31 For incompressible flow, from Bernoulli’s equation, the stagnation pressure is 1 p0 = p∞ + 2 2 ρ∞ V∞ Let S be the surface area of each face of the plate. The aerodynamic force exerted on the front face is Ffront = p0 S and the aerodynamic force on the back face is Fback = p∞ S The net force, which is the drag, is D = Ffront - Fback = ( p0 - p∞ )S From Bernoulli’s equation, p0 - p∞ = 1 2 2 ρ ∞ V∞ Thus, D = CD 1 2 ρ ∞ V∞ 2 S 1 ρ∞V∞ 2 S 2 = = 1 1 ρ∞V∞ 2 S ρ∞V∞ 2 S 2 2 D Hence, CD = 1 5.32 The drag of the airplane is D = q∞ S CD (1) The drag of a flat plate at 90° to the flow, with an area f and drag coefficient of 1, is D = q∞ f CDpblc = q∞ f (1) (2) Equating Eqs. (1) and (2) q∞ S CD = q∞ f or, f = CD S 5.33 f = CD S = (0.0163)(233) = 3.8ft 2 58 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.34 From Appendix D, for the NACA 2412 airfoil at zero angle of attack, Cd = 0.006. This is the profile drag coefficient, the sum of skin friction drag and pressure drag due to flow separation. To estimate the skin friction drag coefficient, from Eq. (4.101) Cd , f = 0.074 Re0.2 L = 0.074 (8.9 ´ 106 )0.2 = 0.023 This is the skin friction coefficient due to flows over only one side of the plate. Including both the top and bottom surfaces of the plate, cd , f = 2(0.003) = 0.006 Since from Section 5.12 cd = cd , f + cd , p we have: cd , p = cd - cd , f = 0.006 - 0.006 = 0. For this case, the pressure drag due to flow separation is negligible. 5.35 From Appendix D, for the NACA 2412 airfoil at an angle of attack of 6°, cd = 0.0075 Assuming, as in Problem 5.34, that the skin friction drag is given by the flat plate result at zero angle of attack, we have cd , f = 0.006 Thus, cd , p = cd - cd , f = 0.0075 - 0.006 = 0.0015 For this case, the percentage of drag due to pressure drag is cd , p cd = 0.0015 = 0.2, or 20% 0.0075 Clearly, as the angle of attack of the airfoil increases, the region of separated flow grows larger, and the pressure drag due to flow separation increases. The large increase in cd at higher values of cl, hence a, seen in Appendix D is due almost entirely to an increase in pressure drag due to flow separation. 59 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.36 In Problem 5.34, the total turbulent skin friction drag coefficient along one surface of the airfoil (top or bottom) was calculated to be 0.003. The transition Reynolds number is 500,000. This implies that the turbulent skin friction coefficient based on the running length of surface from the leading edge to the transition point, xcr, is 0.074 0.074 0.074 (cd , f ) xcr = = = = 0.00536 0.2 0.2 13.8 (Re x,cr ) (500, 000) The contribution of this turbulent skin friction drag coefficient to the total turbulent skin friction drag coefficient for the complete surface calculated to be 0.003 in Problem 5.34 is æ 500, 000 ÷ö 0.00536 çç ÷ = 3.01 ´ 10-4 çè 8.9 ´ 106 ÷ø Hence, the contribution to the overall skin friction drag coefficient for one surface of the airfoil due to the turbulent flow from the transition point to the trailing edge of the airfoil is: (cd , f ) turb = 0.003 - 3.01 ´ 10-4 = 0.0027 The laminar skin friction drag coefficient for the flow from the leading edge to the transition point is, from Eq. (4.98) C f , laminar 1.328 = Re x , cr 1.328 1.328 = = 1.878 ´ 10-3 707.1 500, 000 Since the laminar skin friction is acting only on that part of the surface from x = 0 to x = xcr, then its contribution to the total overall skin friction coefficient for the whole top surface is æ 500, 000 ö÷ (cd , f )lam = 1.878 ´ 10-3 çç ÷ = 1.055 ´ 10-4 çè 8.9 ´ 106 ø÷ Therefore, the total skin friction coefficient for one surface, including both the laminar flow from x = 0 to xcr, and turbulent flow from xcr to the trailing edge, is cd , f = 1.055 ´ 10-4 + 0.0027 = 0.0028 Including both the upper and lower surfaces, then we have cd , f = 2(0.0028) = 0.0056 cd = cd , f + cd , p Thus, cd , p = cd - cd , f = 0.006 - 0.0056 = 0.004 The percentage of the total drag due to pressure drag due to flow separation is then cd , p cd = 0.0004 = (100) = 6.7% 0.006 In contrast to the result obtained in the solution to Problem 5.34, the more realistic result obtained here shows that the pressure dag is not negligible, although it is small compared to the skin friction drag. Note: This problem is similar to worked Example 4.28 in the text. In Example 4.28, the respective skin friction drag forces on various parts of the surface are calculated and are used to solve the problem. In our solution here for Problem 5.36, we have used only the various skin friction coefficients to solve the problem. We do not need to calculate forces. Indeed, in the statement of the problem there is no velocity, density, or surface area given, so we can not calculate forces; none is needed. However, we have been careful in the present calculation to account for the specific regions of the surface to which the calculated coefficients apply, and to multiply the coefficients obtained over the portion of surface between x = 0 and xcr from Eqs. (4.98) and (4.101) by the ratio xcr / L = 500, 000 / 8.9 ´ 106 = 0.0056. It is instructive to work out Example 4.28 in the text using only the various skin friction coefficients as we have used here, and then to calculate total drag Df at the very end of the calculation. You get the same answer as was obtained in Example 4.28. 60 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.37 (a) From Eq. (4.98), Cf = 1.328 Re 1.328 = = 4.43 × 10−4 9 × 106 This is for one side of the flat plate. The total skin friction drag coefficient including both sides of the plate is C f = 2(4.43 × 10−4 ) = 0.000885 (b) From Eq. (4.101) Cf = 0.074 (Re)0.2 = 0.074 (9 × 106 )0.2 = 0.074 = 0.003 24.59 For both sides of the plate, C f = 2(0.003) = 0.006 The section drag coefficient for the NACA 2415 airfoil from App. D is 0.0064. If the boundary layer were laminar, then the fraction of drag due to friction is (0.000885/0.0064) = 0.138, or 13%. If the boundary layer were turbulent, then the fraction of drag due to friction is 0.006/0.0064 = 0.938, or 93.8%. These results highlight the large effect of a turbulent boundary on the drag of an airfoil as compared to a laminar boundary layer. 5.38 (See Section 4.19 for the solution technique.) Assuming all turbulent flow, C f = 0.006 (from Problem 5.37). Transition takes place at location xcr 650,000 = = 0.072 c 9 × 106 The turbulent drag coefficient on the area upstream of transition would be 0.074 0.074 Cf = 2 = 2 = 0.0102 0.2 14.54 (650, 000) Thus, the relative turbulent drag contribution due to the area downstream of the transition point is 0.006 − (0.0102)(0.072) = 0.006 − 0.000734 = 0.005266 The laminar drag coefficient on the area upstream of transition is 1.328 1.328 Cf = 2 = 806 2 = 0.0033 650, 000 The laminar drag contribution over this area is (0.0033)(0.072) = 0.000238 The total skin friction drag coefficient is laminar contribution + turbulent contribution = 0.000238 + 0.005266 = 0.0055 The total section drag coefficient is 0.0064 from App. D. Thus, 0.0055 Friction drag percentage = 100 = 86% 0.0064 Pressure drag percentage = 14% 61 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 5.39 Assuming all turbulent flow, Cf = 0.074 0.074 = = 0.003749 0.2 (Re) (3 × 106 )0.2 Taking into account both sides of the plate C f = (0.003749) 2 = 0.0075 Transition takes place at location xcr 650,000 = = 0.2167 c 3 × 106 The turbulent drag coefficient on the area upstream of transition would be 0.074 Cf = 2 = 0.0102 0.2 (650, 000) The turbulent drag contribution due to the area downstream of the transition point is 0.0075 – (0.0102)(0.2167) = 0.00529 The laminar drag coefficient on the area upstream of transition is 1.328 Cf = 2 = 0.0033 650, 000 The laminar drag contribution over this area is (0.0033)(0.2167) = 0.000715 The total skin friction drag coefficient is 0.000715 + 0.00529 = 0.0060 The experimental data for the total section drag coefficient from App. D is 0.0068. 0.006 Friction drag percentage = 100 = 88% 0.0068 Pressure drag percentage = 11.8% 62 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 6 6.1 (a) V¥ = 350 km/hr = 97.2 m/sec 1 1 2 ρ¥V¥ = (1.225)(97.2)2 = 5787 N/m 2 2 2 38220 W CL = = = 0.242 (5787)(27.3) q¥S q¥ = (0.242)2 CL 2 = 0.03 + π eAR π (0.9)(75) CD = 0.03 + 0.0028 = 0.0328 CD = C D 0 + CL / CD = 0.242 / 0.0328 = 7.38 TR = (b) W 38, 220 = = 5179 N CL /C D 7.38 q¥ = CL = 1 1 2 ρ¥V¥ = (0.777)(97.2) 2 = 3670 N/m2 2 2 W 38, 220 = = 0.38 q¥ S (3670)(27.3) CL 2 (0.38)2 = 0.03 + π eAR π (0.9)(7.5) CD = 0.03 + 0.0068 = 0.0368 Cd = CD0 + CL / CD = 0.38 / 0.0368 = 10.3 TR = 6.2 V¥ = 200 W 38,220 = = 3711N CL /CD 10.3 88 = 293.3ft/sec 60 1 1 2 ρ¥V¥ = (0.002377)(293.3)2 = 102.2 lb/ft 2 2 2 5000 L W CL = = = = 0.245 (102.2)(200) q¥ S q¥ S q¥ = CDi = (0.245) CL 2 = = 0.0024 π e AR π (0.93)(8.5) Since the airplane is flying at the condition of maximum L/D, hence minimum thrust required, C Di = C De . Thus, CD = CD0 + CDi = 2CDi = 2(0.0024) = 0.1048 D = q¥ SCD = (102.2)(200)(0.0048) = 98.1lb. 63 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.3 (a) Choose a velocity, say V∞ =100 m/sec q¥ 1 1 2 ρ¥V¥ = (1.225)(100) 2 = 6125 N/m 2 2 2 103,047 W CL = = = 0.358 (6125)(47) q¥S (0.358)2 CL 2 = 0.032 + π eAR π (0.87)(6.5) = 0.032 + 0.007 = 0.0392 CD = CD0 + CD TR = 103, 047 W = = 11287 N 9.13 CL / CD PR = TRV¥ = (11, 287)(100) = 1.129 ´ 106 watts PR = 1129 kw A tabulation for other velocities follows on the next page: V (m/sec) CL CD CL/CD PR (kw) 100 0.358 0.0392 9.13 1129 130 0.212 0.0345 6.14 2182 160 0.140 0.0331 4.23 3898 190 0.099 0.0325 3.05 6419 220 0.074 0.0323 2.29 9900 250 0.057 0.0322 1.77 14,550 280 0.046 0.0321 1.43 20,180 310 0.037 0.0321 1.15 27,780 (b) PA = TAV¥ = (2)(40298)V¥ = 80596V¥ The power required and power available curves are plotted below. From the intersection of the PA and PR curves, we find, Vmax = 295 m/sec at sea level 64 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (c) At 5 km standard altitude, ρ = 0.7364 kg/m3 Hence, ( ρ 0 /ρ )1/2 = (1.225/0.7364)1/2 = 1.29 Valt = ( ρ0 /ρ )1/2V0 = 1.29 V0 PRalt = ( ρ0 /ρ )1/2 PR 0 = 1.29 PR 0 From the results from part (a) above, PR 0 V0 (m/sec) (kw) 100 130 160 190 220 250 (d) PRak Valt (m/sec) (kw) 129 168 206 245 284 323 1456 2815 5028 8281 12,771 18,770 1129 2182 3898 6419 9900 14,550 æ ρ ö TAall =TA 0 ççç ÷÷÷ = 0.601TA 0 çè ρ0 ÷ø PAalt = TAalt V¥ = (0.601)(80596)V¥ = 48438V¥ Hence, The power required and power available curves are plotted below. From the intersection of the PR and PA curves, we find Vmax = 290 m/sec at 5 km Comment: The mach numbers corresponding to the maximum velocities in parts (b) and (d) are as follows: At sea level a¥ = γ RT¥ = M¥ = V¥ 295 = = 0.868 a¥ 340 (1.4)(287)(288.16) = 340 m/sec At 5 km altitude a¥ = M¥ = γ RT¥ = (1.4)(287)(255.69) = 321m/sec V¥ 290 = = 0.90 a¥ 321 These mach numbers are slightly larger than what might be the actual drag-divergence Mach number for an airplane such as the A-10. Our calculations have not taken the large drag rise at drag-divergence into account. Hence, the maximum velocities calculated above are somewhat higher than reality. 65 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.4 (a) Choose a velocity, say V¥ = 100 ft/sec 1 1 ρ¥V¥2 = (0.002377)(100)2 = 11.89 lb/ft 2 2 2 W 3000 CL = = = 1.39 q¥ S (11.89)(181) q¥ = CD = CD0 + CL 2 (1.39)2 = 0.027 + π e AR π (0.91)(6.2) CD = 0.027 + 0.109 = 0.136 TR = W 3000 3000 = = = 293.5 lb CL /CD (1.39) /(0.136) 10.22 PR = TR ⋅ V¥ = (293.5)(100) = 29350 ft lb/sec In terms of horsepower, PR = 29350 = 53.4 hp 550 A tabulation for other velocities follows: V∞ (ft/sec) CL CD CL/CD PR (hp) 70 2.85 0.485 5.88 64.9 100 1.39 0.136 10.22 53.4 150 0.62 0.0487 12.37 64.3 200 0.349 0.0339 10.29 106 250 0.223 0.0298 7.48 182 300 0.155 0.0284 5.46 300 350 0.114 0.0277 4.12 463 (b) At sea level, maximum PA = 0.83 (345) = 286 hp. The power required and power available are plotted below. From the intersection of the PA and PR curves, Vmax = 295ft/sec = 201mph at sea level 66 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (c) At a standard altitude of 12,000 ft, ρ = 1.648 ´ 10-3 slug/ft 3 Hence, ( ρ 0 /ρ )1/2 = (0.002377 / 0.001648)1/ 2 = 1.2 Valt = ( ρ0 /ρ )1/2V0 = 1.2V0 PRak = ( ρ0 /ρ )1/2 PR0 = 1.2 PR0 Using the results from part (a) above, PR0 V0 (ft/sec) 70 100 150 200 250 300 (hp) 64.9 53.4 64.3 106 182 300 PRah Valt (ft/sec) (hp) 84 120 180 240 300 360 77.9 64.1 76.9 127 218 360 (d) Assuming that the power output of the engine is proportional to p∞, æ 0.001648 ÷ö PAalt = (ρ /ρ0 ) PA 0 = çç P = 0.693 PA 0 çè 0.002377 ÷÷ø A 0 At 12,000 ft, PA = 0.693(286) = 198 hp The power required and power available curves are plotted below. From the intersection of the PA and PR curves, Vmax = 290ft/sec =198 mph at12,000 ft. 6.5 From the PA and PB curves generated in Problem 6.3, we find approximately: excess power = 9000 kw at sea level excess power = 5000 kw at 5 km Hence, at sea level excess power 9 ´ 106 watts = = 87.3m/sec W 1.0307 ´ 105 N and at 5 km altitude, R/C = R/C = 5 ´ 106 1.03047 ´ 105 = 48.5 m/sec 67 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.6 From the PA and PR curves generated in Problem 6.4, we find approximately: excess power = 232 hp at sea level excess power = 134 hp at 12,000 ft Hence, at sea level, R/C = excess power (232)(550) = = 42.5ft/sec W 3000 and at 12,000 ft altitude, (134)(550) = 24.6 ft/sec 3000 R/C = 6.7 Assuming (R/C)max varies linearly with altitude, (R/C)max = ah + b From the two (R/C)max values from Problem 6.5, 87.3 = a(o) + b 48.5 = a(5000) + b Hence, b = 87.3 a = -0.00776 (R/C)max = -0.00776h + 87.3 To obtain the absolute ceiling, set (R/C)max = 0, and solve for h. h= 87.3 = 11, 250 m 0.00776 Hence, absolute ceiling ≈ 11.3 km 6.8 (R/C)max = ah + b From the results of Problem 6.6, 42.5 = a(0) + b 24.6 = a(12, 000) + b Hence, b = 42.5 a = -0.00149 (R/C)max = -0.00149h + 42.5 To obtain the absolute ceiling, set (R/C)max = 0, and solve for h. 42.5 = 28,523ft 0.00149 absolute ceiling ≈ 28,500 ft h= COMMENT TO THE INSTRUCTOR In the previous problems dealing with a performance analysis of the twin-jet and single-engine piston airplanes, the answers will somewhat depend on the precision and number of calculations made by the student. For example, if the PR curve is constructed from 30 points instead of the six or eight points as above, the subsequent results for rate-of-climb and absolute ceiling will be more accurate than obtained above. Some leeway on the students' answers is therefore advised. In my own experience, I am glad when the students fall within the same ballpark. 68 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.9 R = h (L/D) max = 5000(7.7) = 38,500 ft = 729 miles 6.10 First, we have to calculate the CL corresponding to maximum L/D. æC çç L ççè C D ö÷ ÷÷ = ÷ø max C D,0 C D,Oπ e AR 2C D,0 1æ C = ççç L 4 çè CD ö÷ ÷÷ ÷ø = π e AR 4C D,0 -2 π e AT = (0.25) π (0.7)(4.11) (7.7)2 max = 0.038 At maximum L/D, C D,0 = CD,i = 0.038 Hence: CD = 2(0.038) =0.076 æC CL = CD ççç L çè CD ö÷ ÷÷ = (0.076)(7.7) = 0.585 ø÷ Also: æ L ö÷-1 = Arc Tan (0.13) çè D ø÷÷ max θ min = Arc Tan çç θmin = 7.4 V¥ = 2 cos θ çæ W ç ρ C èç S ¥ L ö æ 1400 ö÷ 2 cos(7.4) çç ÷÷÷ = ÷ = 97.2 ft/sec ø (0.002175)(0.585) èç 231 ø÷ 6.11 From Eq. (6.85), ( π eARCD0 æLö = ççç ÷÷÷ è D ømax 2CD0 t/2 ) Putting in the numbers: 1/2 æ L ö÷ [ π (0.9)(6.72)(0.025) ] ç = ççè D ø÷÷ 0.050 max 69 = 13.78 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.12 Aviation gasoline weighs 5.64 Ib per gallon, Hence, WF = (44)(5.64) = 248lb. Thus, the empty weight is W1 = 3400 - 248 = 3152lb. The specific fuel consumption, in consistent units, is c = 0.42/(550)(3600) = 2.12 ´ 10-7 ft-1 The maximum L/D can be found from Eq. (6.85). (π e AR CDc )1/2 æ L ö÷ [ π (0.91)(6.2)(0.027) ]1/2 çç ÷ = = = 12.8 çè D ø÷ 2 CD 2(0.027) max c Thus, the maximum range is: æ η öæ C ö R = çç ÷÷÷ççç L ÷÷÷ çè c ÷øèç C ø÷ D max æW ö n ççç 0 ÷÷÷ èç W1 ø÷ æ ö æ 3400 ö÷ 0.83 R = çç ÷÷÷ (12.8) n çç ÷ 7 çè 2.12 ´ 10 ø èç 3152 ø÷ R = 3.8 ´ 106 ft In terms of miles, R = 3.8 ´ 106 = 719 miles 5280 To calculate endurance, we must first obtain the value of (CL3/2 /CD ) max From Eq. (6.87), æ C 3/2 ÷ö (3 CD 0 π e AR)3/4 çç L ÷ = ç C ÷÷ 4 CDc çè D ÷ø max Putting in the numbers: æ C 3/2 ö÷ [ 3(0.027) π (0.91)(6.2) ]1/2 çç L ÷ = = 11.09 çç C ÷÷ 4(0.027) è D ø÷max Hence, the endurance is æ η ö C3 / 2 E = çç ÷÷÷ L (2 ρ¥ S )1/2 (W1-1/ 2 - W0-1/ 2 ) çè c ø C D æ ö÷ 0.83 1/ 2 E = çç ÷ (11.09) [ 2(0.002377)(181) ] (3152-1/ 2 - 3400-1/ 2 ) 7 çè 2.12 ´ 10 ø÷ E = 2.67 ´ 104 sec = 7.4 hr 70 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.13 One gallon of kerosene weighs 6.67 Ib. Since 1 Ib = 4.448 N, then one gallon of kerosene also weighs 29.67 N. Thus, W f = (1900)(29.67) = 56,370 N Wt = W0 - W f = 136,960 - 56,370 = 80,590 N In consistent units, ct = 1.0 N = 2.777 ´ 10-4 sec-1 (N)(hr) Also, at a standard altitude of 8 km. ρ¥ = 0.526 kg/m3 Since maximum range for a jet air craft depends upon maximum CL1/2 /C D , we must use Eq. (6.86). æ C 1/2 ö÷ çç L ÷ ÷÷ çç è CD ø÷ max æ1 ö1/4 çç CD π e AR ÷÷ ÷ø çè 3 c = 4 CDc 3 Putting in the numbers, é1 ù1/4 ê (0.032)(0.87)(6.5) ú æ C 1/2 ÷ö ê3 ûú ççç L ÷÷ = ë = 15.46 ÷ 4 çè CD ø÷ (0.032) max 3 For a jet airplane, the range is R = 2 æ1 çç ρ¥ S çèç ct 2 ö÷æç C 1/2 ö÷ 1/2 ÷ç L ÷÷ (W0 - W11/2 ) ÷ç ø÷çè CD ø÷÷ é ù1/2 æ 2 1 ÷÷ö (15.46) é (136,960)1/2 - (80,590)1/2 ù ú çç R = 2ê êë úû ê (0.526)(47) ú çè 2.777 ´ 10-4 ÷ø ë û R = 2.73 ´ 106 m = 2730 km The endurance depends on CLCD. From Eq. (6.85), (π e AR CDc )1/2 æ L ö÷ [ π (0.87)(6.5)(0.032) ]1/2 çç ÷ = = = 11.78 çè D ø÷ 2 CDc 2 (0.032) max The endurance for a jet aircraft is E = E = 1 æç C L ÷ö çæ W0 ÷ö ÷÷ n ç ÷÷ ç ct ççè CD ÷ø ççè W1 ÷ø 1 -4 æ 136,960 ÷ö (11.78) n çç ÷ çè 80,590 ÷÷ø 2.777 ´ 10 E = 22, 496 sec = 6.25 hr 71 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.14 CL3/ 2 = CD CL3/ 2 CD0 + CL2 π e AR -2 éæ ù æ d (CL3 / 2 / CD ) CL2 ö÷÷æç 3 12 ö÷ CL ö÷ ú æç CL2 ö÷÷ çç 3/ 2 ç ê = ê ç CD0 ÷ç C ÷ - C L çç 2 ÷÷ ú çç CD + π e AR ÷÷ = 0 π e AR ø÷÷çè 2 L ø÷ d CL èç π e AR ÷ø ú èç 0 êë çè ø÷ û 3 12 1 CL5 / 2 CL CD0 = 0 2 2 π e AR 3 CD0 - CL2 =0 π e AR CD0 = Hence, 1 CD 3 i This is Eq. (6.80) To obtain Eq. (6.81) C1/2 L = CD C1/2 L CD0 + CL2 π e AR -2 éæ ùæ 2 d (C1/ CL2 ö÷÷ 1 - 12 CL2 ö÷÷ - 12 æç 2 CL ö÷ ú ç L /C D ) = ê çç C ÷÷ ú çç CD + ÷ C - C L çç ÷ =0 ê çç D0 π e AR ÷÷ø 2 L π e AR ÷÷ø d CL èç π e AR ÷ø ú èç 0 êë è û 1 3 CL5/2 -1 = 0 CD0 CL 2 2 2 π e AR CD0 - 3 CL3/2 =0 π e AR CD0 = 3 C Di 6.15 From Eq. (6.81), CD0 = 3 C Di CD0 = 3 CL2 π e AR 1 æ1 ö2 CL = çç π e AR C D0 ÷÷÷ çè 3 ø Thus, 1 æ 12 ö÷ çç CL ÷ ÷÷ çç çç CD ÷÷÷ è ø max æ1 ö4 çç π e AR CD ÷÷ ÷ø 0 çè 3 This is Eq. (6.86) = 4 CD0 3 From Eq. (6.80), CD0 = 1 CD 3 i CD0 = CL2 3π e AR 1 Thus, CL = (3π e AR CD0 ) 2 æ 32 ö÷ çC ÷ ççç L ÷÷ çç C D ÷÷÷ è ø max æ ç 3π e AR C D0 = çç çç 4 CD è 0 3 ö4 ÷÷÷ (This is Eq. (6.87) ÷÷ø 72 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.16 AR = b 2 /S , hence b = S AR = (47)(6.5) = 17.48 m h = 5 ft = (5 / 3.28) m = 1.524 m h/b = 1.54 /17.48 = 0.08719 φ = (16 h/b)2 1 + (16 h / b) 2 VL0 = 1.2Vstall = 1.2 = 1.946 = 0.66 2.946 2W ρ¥S CL,max = 1.2 2(103, 047) = 80.3 m/sec (1.255)(47)(0.8) Hence, 0.7 0.7VL0 = 56.2 m/sec. This is the velocity at which the average force is evaluated. 1 1 2 ρ¥V¥ = (1.225)(56.2)2 = 1935 N/m 2 2 2 L = q¥ S C L = (1935) (47)(0.8) = 72, 760 N q¥ = æ CL2 ÷÷ö ç D = q¥ S C D = q¥ S çç C D0 + φ ÷ çè π e AR ÷÷ø D = (1935)(47)[(0.032) + (0.66)(0.8)2 /π (0.87)(6.5)] D = 5072 N From Eq. (6.90) s L0 = = 1.44 W 2 g ρ¥CL,max { T - [ D + μr (W - L) ] ave } 1.44 (103047)2 (9.8)(1.225)(47)(0.8) { 80595 - [ 5072 + (0.2)(103047 - 72760) ]} sL0 = 452 m 73 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.17 b= S AR = (181)(6.2) = 33.5 ft. h/b = 4 / 33.5 = 0.1194 φ = (16h/b)2 1 + (16h/b) VL0 = 1.2 2 = 3.65 = 0.785 4.65 2W ρ¥ S CL,max = 1.2 2(3000) = 135 ft/sec (0.002377)(181)(1.1) 0.7 = VL0 = 0.7(135) = 94.5 ft/sec. q¥ = 1 1 2 ρ¥V¥ = (0.002377)(94.5) 2 = 10.6 1b/ft 2 2 2 L = q¥S CL = (10.6)(181)(1.1) = 2110 1b æ C L2 ö÷÷ ç D = q¥ S CD = q¥ S çç CD,0 + φ ÷ çè π e AR ÷ø÷ é (0.785)(1.1)2 ùú D = (10.6)(181) êê (0.027 + = 154.6 lb π (0.91)(6.2) úúû êë T = (550 HPA )/V¥ = (550)(285) / 94.5 = 1659 lb S L0 = 1.44 W 2 g ρ¥ S C L,max {T - [ D + μr (W - L)]ave} 1.44 (3000)2 (32.2)(0.002377)(181)(1.1){1659 - [154.6 + (0.2)(3000 - 2110]} S L0 = 572 ft. = 6.18 VT = 1.3 2W ρ¥ S CL,max = 1.3 2(103, 047) = 46.39 m/sec (1.23)(47)(2.8) 0.7 VT = 32.47 m/sec. q¥ 1 2 ρ¥V¥ = (0.5)(1.23)(32.47)2 = 648.4 N/m 2 2 Since the lift is zero after touchdown, C D = C D,0⋅ D = q¥ S C D,0 = (648.4)(47)(0.032) = 975.2 N SL = 1.69 W 2 g ρ¥CL,max [ [ D + μr (W - L) ]0.7V T SL = 1.69 (103047)2 = 268 m (9.8)(1.23)(47)(2.8)[975.2 + (0.4)(103, 047)] 74 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.19 VT = 1.3 2W ρ¥S CL,max = 1.3 2(3000) = 114.4 ft/sec (0.002377)(181)(1.8) 0.7 VT = 80.08 ft/sec. q¥ = 1 1 2 ρ¥ V¥ = 0.5(0.002377)(80.08) 2 = 7.62 1b/ft 2 2 2 D = q¥ S C D,0 = (7.62)(181)(0.027) = 37.2 1b SL = 1.69 W 2 g ρ¥S CL,max [ [ D + μr (W - L) ]0.7V T SL = 2 1.69 (3000) = 493 ft (32.2)(0.002377)(181)(1.8)[37.2 + 0.4 (3000)] æ 88 ö 6.20 V¥ = 250 mph = 250 çç ÷÷÷ ft/sec = 366.6 ft/sec çè 60 ø = 366.6 (0.3048) m/sec = 111.7 m/sec. q¥ = 1 2 ρ¥V¥ = (0.5)(1.23)(111.7)2 = 7673 N/m 2 2 L = q¥ S CL,max = (7673)(47)(1.2) = 4.358 ´ 105 N n = R = w= L 4.328 ´ 105 = = 4.2 W 103047 2 V¥ g n2 - 1 = (111.7)2 9.8 (4.2)2 - 1 = 312 m V¥ 111.7 = = 0.358 rad/sec R 312 75 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. T = D = q¥S CD 6.22 From Eq. (6.13) CL2 π e AR From Eq. (6.1 c) C D = C D, 0 + Combining (1) and (2) é CL2 ùú T = q¥ S êê CD, 0 + π e AR úúû êë L = W = q¥ S CL From Eq. (6.14) CL = W q¥ S Substitute (4) into (3) é ù W2 W2 ú = q SC T = q¥S êê CD,0 + 2 + ¥ D, 0 ú q¥ Sπ e AR q¥ Sπ e AR ûú ëê Multiply by q∞ W2 Sπ e AR 2 q¥T = q¥ SCD, 0 + or 2 q¥ SCD, 0 - q¥T + W2 =0 Sπ e AR From the quadratic formula: T T2 q¥ = q¥ = 2 V¥ = V¥ 4 SCD, 0W 2 Sπ e AR 2 SCD, 0 T æç W ç W èç S æT çç èç W 2 4 C D, 0 ÷÷ö W æçç T ÷÷ö ÷ø π e AR S èç W ÷ø 1 2 = ρ¥V¥ 2 C D, 0 2 ÷÷öæçç W ÷øèç S é ê æç T ê çç ê èW = ê ê ê ê êë 2 4 C D, 0 ÷÷ö + W ççæ T ÷÷ö ÷ø π e AR S çè W ÷ø ρ¥CD, 0 ÷÷öæçç W ÷øèç S 2 4 C D, 0 ÷÷ö + W ççæ T ÷÷ö ÷ø S çè W ÷ø π e AR ρ¥CD, 0 ù1/ 2 ú ú ú ú ú ú ú úû For Vmax : T = (TA )max (V¥ )max é æW ê æç TA ö÷ çç ê çç ÷÷ ê è W ømax èç S = ê ê ê ê êëê ù1/ 2 4 C D, 0 ú ö÷ W æ TA ÷ö 2 ç ú ÷÷ø + S èçç W ÷÷ø π e AR ú max ú ú ρ¥CD, 0 ú ú úûú 76 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.23 From Figure 6.2, ( L/D) max = 18.5, and CD, 0 = 0.015. From Eq. (6.85) ö (CD, 0π e AR)1/2 ÷÷÷ = ÷ 2 CD,0 D ømax æC çç L ççè C 4 CD, 0 (CL /CD )2 max e= or, e= π AR 4 (0.015)(18.5)2 = 0.83 π (7.0) Please note: Consistent with the derivation of Eq. (6.85) where a parabolic drag polar is assumed with the zero-lift drag coefficient equal to the minimum drag coefficient, for the value of CD,0 in this problem we read the minimum drag coefficient from Figure 6.2. 6.24 Drag: D = q¥ SCD Power Available: PA = η Ps Also, PA = TAV¥ Hence TA = η Ps V¥ (a) At an altitude of 30,000 ft, ρ∞ = 0.00089068 slug/ft3 and T∞ = 411.86°R. The speed of sound is a¥ = γ RT¥ = (1.4)(1718)(411.86) = 994.7 ft/sec Hence, at Mach one, the flight velocity is V∞ = 994.7 ft/sec q¥ = 1 1 2 ρ¥V¥ = (0.00089068)(994.7)2 = 440.6 1b/ft 2 2 2 The drag coefficient at Mach one, as given in the problem statement is CD, 0 (at M ¥ = 1) = 10[CD, 0 (at low speed)] = 10(0.0211) = 0.211 Hence, drag at Mach one is D = q¥S CD = (440.6)(334)(0.211) = 31, 0511b The thrust available is obtained as follows. The engine produces 1500 horsepower supercharged to 17,500 ft. Above that altitude, we assume that the power decreases directly as the air density. At 17,500 ft, ρ∞ = 0.0013781 slug/ft3. Hence HP = ρ¥ (at 30,000 ft) 0.00089068 (1500) = (1500) = 969 HP 0.0013781 ρ¥ (at 17,500 ft) From Eq. (3), above TA = η Ps V¥ = (0.3)(969)(550) = 1611b 994.7 Consider the airplane in a vertical dive at Mach one. The maximum downward vertical force is W + TA = 12,441 + 161 = 12,602 lb. However, the drag is the retarding force acting vertically upward, and it is 31,051 lb. At Mach one, the drag far exceeds the maximum downward force. Hence, it is not possible for the airplane to achieve Mach one. 77 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) At an altitude of 20,000 ft, ρ¥ = 0.0012673 slug/ft 3 T¥ = 447.43R a¥ = V¥ = q¥ = (1.4)(1716)(447.43) = 1036.8 ft/sec 1 1 2 ρ¥ V¥ = (0.0013672)(1036.8) 2 = 6811b/ft 3 2 2 D = q¥ S CD = (681)(334)(0.211) = 47,993 lb The thrust available is obtained as follows HP = ρ¥ (at 20,000 ft) 0.0012673 (1500) = (1500) = 1379 HP 0.0013781 ρ¥ (at 17,500 ft) Hence, TA = η Ps V¥ = (0.3)(1379)(550) = 219 lb 1036.8 In a vertical, power-on dive at 20,000 ft, the maximum vertical force downward is W + TA = 12,441 + 219 = 12,660 lb. However, the drag is the retarding force acting vertically upward, and it is 47,993 lb. At Mach one, the drag far exceeds the maximum downward force. Hence it is not possible for the airplane to achieve Mach 1. 6.25 Taking the analytical approach given in Example 6.19, from Eq. (E6.19.1) PA = 1 W2 3 S C D, 0 + ρ¥V¥ 1 2 ρ V¥ Sπ e AR 2 b2 (14.45) 2 = = 19.3 S 11.45 W = 1020 kg f = (1020)(9.8) = 9996 N AR = PA = η (bhp) = (0.9)(85) = 76.5 hp Using consistent units, noting that 1 hp = 746 Watts PA = (76.5)(746) = 5.71 ´ 10 4Watts 1 1 ρ¥ S CD, 0 = (1.23)(11.45)(0.03) = 0.2113 2 2 1 1 ρ¥ Sπ e AR = (1.23)(11.45) π (0.7)(19.3) = 298.9 2 2 Inserting these numbers into Eq. (1) 3 5.71 ´ 104 = 0.2113 V¥ + or, 3 5.71 ´ 104 = 0.2113V¥ + Solving Eq. (2) for V∞ (9996)2 298.9 V¥ 3.343 ´ 105 V¥ V¥ = Vmax = 62, 6 m/sec. 78 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.26 From Eq. (6.67) R = η CL c CD n W0 W1 ö÷ (CD, 0 π e AR)1/2 [ (0.03) π (0.7)(19.3) ]1/ 2 ÷÷ 18.8 = = ÷ 2 CD,0 2(0.03) D ømax æC çç L ççè C Using consistent units, c = 0.2 é kg f ù çæ 9.8N ú çç = 0.2 êê úç (hp)(hr) ëê (hp)(hr) ûú èç 1 kg f kg f ö÷ é 1 hp ùæ 1 hr ö ÷÷ ÷÷ ê úç ÷ ê 746 Nm/s ú çççè 3600 sec ÷÷ø ÷øë û 7 = 7.3 ´ 10m-1 W0 = 1020 kg f = 1020 (9.8) = 9996 N W1 = W0 - Wfuel = 9996 - (295)(9.8) = 7105 N From Eq. (6.67) R = η CL W n 0 = c CD W1 æ ö÷ æ 9996 ö÷ 0.9 ÷ (18.8) n çç ÷ ççç 7 ÷ èç 7105 ø÷ è 7.3 ´ 10 ø R = 3.44 ´ 106m = 3440 km æ C 3/2 ÷ö ç 6.27 çç L ÷÷÷ çè CD ÷ø = (3 CD, 0 π e AR)3/4 4 CD, 0 max = [ 3(0.03) π (0.7)(19.3) ]3/4 4(0.03) = 22, 77 From Eq. (6.68) æ η öæç C 3/2 ÷ö E = çç ÷÷÷çç L ÷÷÷ (2ρ¥ S )1/2 (W1-1/2 - W0-1/2 ) èç c øçè CD ÷ø Using results from Problem 6.26, æ ö÷ 0.9 E = çç ÷ 22.77[2(1.23) (11.45)]1/2 [(7105)-1/2 - (9996)-1/2 ] çè 7.3 ´ 10-7 ø÷ E = 14.9 ´ 107[0.01186 - 0.01000] E = 2.77 ´ 105 sec or, E = 2.77 ´ 105 = 77 hours 3600 79 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.28 Di = Q¥ S CD, i = q¥ S CL 2 π e AR In steady level flight, L = W, and we have æ L ÷ö2 æ W ÷ö2 ÷÷ = çç CL2 = ççç ÷÷ çè q¥ S ÷ø èçç q¥ S ø÷ Substitute (2) into (1). æ W ÷ö2 1 ÷ Di = Q¥ S ççç çè Q¥ S ÷÷ø π e AR But AR = b2 , hence Eq. (3) becomes S æ W ÷ö2 1 æ S ö çç ÷÷ ÷÷ Di = q¥S ççç ÷ èç d¥ S ÷ø πe èç b2 ø Di = 6.29 (a) q¥ = 1 1 æç W ç π eq¥ çè b 2 2 ρ¥V¥ = q¥ = 198.26 1b/ft 1 ö÷2 ÷÷ QED ø -3 éê æç 88 ö÷ 2ù ÷÷ (300) ú 2 (2.0482 ´10 ) ê èçç ú ø ë 60 û 2 b = 37 ft W = 10,100 1b Di = 1 çæ W ç π eq¥ çè b 2 æ ö2 1 ÷÷ö = çç 10,100 ÷÷ ø÷ π (0.8)(198.26) èç 37 ø÷ Di = 149.5 lb (b) CDi = CL2 π e AR CL = W 10,100 = = 0.2186 q¥ S (198.26)(233) AR = b2 (37)2 = = 5.87 S 233 CL2 (0.2186) 2 = = 0.003245 π eAR π (0.8)(5.86) Di = q¥ S CDi = (168.26)(233)(0.003245) Di = 149.9 lb CDi = The results from parts (a) and (b) agree to within 3-place round off error on the author’s hand calculator. 80 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.30 (a) From (6.45), copied below, for rate-of-climb at the climb angle θ, T = D + W sin θ we have T D = + sin θ W W Assume L = W. Thus, T D = + sin θ W L or, T 1 = + sin θ W L/D (b) At a standard altitude of 31,000 ft, T∞= 408.3 R. a∞ = γRT∞ = (1.4)(1716)(408.3) = 990 ft/sec V∞ = M ∞ a∞ = 0.85(990) = 841.5 ft/sec. The specified rate-of-climb of 300 ft/min, in terms of ft/sec, is 300/60 = 5 ft/sec. From Eq. (6.48) and Fig. 6.28, sin θ = R /C 5 = + 5.94 ´ 10-3 841.5 V∞ Thus, θ = 0.34 - very small. Hence, T 1 1 = + sin θ = + 5.94 ´ 10-3 W L /D 18 or T = 0.0615 W Thus T = 0.0615 W = 0.0615(550, 000) = 33,825 lb. This is the required combined thrust from both engines. The thrust of each engine at this flight condition is 33,825/2, or 16,912 Ib. At 31, 000 ft, ρ∞ = 8.5841 ´ 10-4 slug/ft 3. Assuming the engine thrust is proportional to density, as discussed in Section 6.7, we have for the thrust at sea level, æ 0.002377 ÷ö T = çç ÷ 33825 = 93, 666 lb. çè 8.5841 ´ 10-4 ÷ø This is comparable to the 84,000 lb sea level static thrust of the particular Trent engine mentioned in the problem. 81 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.31 To answer this question, we need to compare the thrust with the weight plus drag at Mach 1; in a vertical climb at Mach 1, if T > W + D, then the airplane will accelerate through Mach 1 in a vertical climb. For an airplane in a vertical climb, lift = 0. Hence, the total drag coefficient is that for zero lift. CD = 0.016(2.3) = 0.368 at Mach 1. Let us assume standard sea-level conditions, where ρ∞ = 1.23 kg/m3 and a∞ = 340.3 m/sec. At march 1, V∞ = a∞ = 340.3 m/sec. Thus, q¥ = 1 2 p¥V¥ = 1 2 (1.23)(340.3)2 = 7.12 ´ 104 N/m 2 D = q¥ S CD = (7.12 ´ 104 )(27.84)(0.0368) = 7.3 ´ 104 N The weight is given as 8,273 kgf; in terms of newtons W = (8273)(9.8) = 8.11 ´ 104 N Hence, D + W = (7.3 + 8.11) ´ 104 = 1.541 ´ 105 N Compare this with the thrust at sea level, T = 131.6 k N = 1.316 ´ 105 N For this case, T < D + W . The airplane can not accelerate through Mach one going straight up at sea level. Since D ∝ ρ∞ and T ∝ ρ∞ , both D and T will decrease by the same factor with an increase in altitude. Because the weight is fixed, T < D + W at all altitudes. Hence, at all altitudes, the airplane can not accelerate through Mach one going straight up. 6.32 At 2000 m, T¥ = 275.16 K and ρ¥ = 1.0066 kg/m3 a¥ = γRT¥ = (1.4)(287)(275.16) = 332.5 m/sec. V 100 M¥ = ¥ = = 0.3 a¥ 332.5 Hence, the airplane is flying at a low Mach number, far below the drag-divergence Mach number. Thus, the zero-lift drag coefficient is CD = 0.016. 2 q¥ = 1 2 ρ¥ V¥ = 1 2 (1.0066)(100)2 = 5033 N/m 2 D = q¥ S C D = (5033)(27.87)(0.016) = 2243 N The acceleration is obtained from Newton’s 2nd Law, F = ma. The net force acting on the airplane in the upward direction is T - W - D = 131.6 ´ 103 - (8273)(9.8) - 2.243 ´ 103 = 131.6 ´ 103 - 81.08 ´ 103 - 2.243 ´ 103 = 48.28 ´ 103 N From the discussion in Section 2.4, the weight in kgf is the same number as the mass in kg. Hence, the mass of the F-16 is 8273 kg. Thus, a= F 48.28 ´ 103 = = 5.84 m/sec2 m 8273 82 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.33 From the definition of TSFC, we have W f = (TSFC) T t = (TSFC) D t = w (TSFC) t L/ D (1) Also, the new thrust specific fuel consumption results in a new fuel weight W f , new = = Wnew L D (TSFC)(1 - ε f ) t W (1 + ε w ) L D (TSFC) (1 - ε f ) t (2) Substituting (1) into (2), we have W f ,new = W f (1 + ε w )(1 - ε f ) (3) Increase in engine weight = Wnew - W = W (1 + ε w ) - W = ε wW Decrease in fuel weight = W f - W f , new = W f - W f (1 + ε w )(1- ε f ) (using Eq.(3)) At the break-even point, we have Wnew - W = W f - W f , new ε wW = W f - W f (1 + ε w )(1 - ε f ) εw W = 1 - (1 + ε w )(1 - ε f ) Wf εw W = -ε w + ε f + ε wε f Wf Since ε w and ε f are very small fractions, we can ignore the product ε wε f . Thus, æ ç ççè ε f = ε w çç1 + W Wf ö÷ ÷÷ ÷ ø÷ and from Eq. (1), we have εf é ù L ê ú ú D = ε w êê 1 + ú (TSFC) t ú ê êë úû 83 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.34 Weight at beginning of flight = 1.35 ´ 106 1b. Weight at end of flight = 1.35 ´ 106 - 0.5 ´ 106 = 0.85 ´ 106 lb. 1.35 ´ 106 + 0.85 ´ 106 = 1.1 ´ 106 lb. 2 From the result of Problem 6.33, we have Average weight during flight = εw = εf 1+ W Wf where ε f = 0.01, W = 1.1 ´ 106 1b, and W f = 0.5 ´ 106 lb. 0.01 εw = 1+ 1.1 ´ 10 6 = 0.01 = 0.00313 3.2 0.5 ´ 106 Wnew = W (1+ε w ) =1.1 ´ 106 (0.00313) = 3438 1b. The weight increase allowed for each engine is therefore 3438 = 859 1b. 4 6.35 C2 TA = D = q∞ S C D = q∞ S CD,0 + L π eAR C2 PA = TAV∞ = q∞ S V∞ CD,0 + L π eAR CL = W q∞ S W 2V∞ W2 PA = q∞ S V∞ C D,0 + = q∞ S V∞ CD,0 + q S π eAR 2 q∞ S π eAR ∞ CD,0 PA (W/S ) = 1 2 ρ∞V∞3 + W (W/S ) 1 2 p∞V∞π eAR CD,0 PA 2(W/S ) = 1 2 ρ∞V∞3 + W (W/S ) p∞V∞π eAR (1) PA = η P where P is the shaft power from the engine. At maximum velocity, P = Pmax. Equation (1) then becomes η Pmax W = CD ,0 1 2 (W/S) 3 + ρ∞ Vmax 2 (W/S) ρ∞Vmax π eAR 84 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.36 For the CP-1, Pmax = 230 hp = (230)(550) = 1.265 × 105 ft lb/sec Pmax / W = 42.88 ft/sec η = 0.8 W = 2950 lb CD ,0 = 0.025 W/S = 2950 /174 = 16.954 lb/ft 2 e = 0.8 AR = b2 /S = (35.8) 2 /174 = 7.366 ρ∞ = 0.002377 slug/ft 3 at sea level From the equation obtained as the result of Problem 6.35, η Pmax W = CD,0 1 2 (W/S ) 3 + ρ∞ Vmax 2 (W/S ) ρ∞Vmax π eAR 3 0.8(42.88) = 1 2 (0.002377) Vmax 3 + 34.304 = 1.75254 × 10−6 Vmax (0.025) 2(16.954) + 16.954 (0.002377)Vmax π (0.3)(7.366) 770.55 Vmax (1) Eq. (1) is an equation for Vmax that yields an analytic solution for Vmax. But it must be solved by trial and error. We will shortcut the trial and error process for this solutions manual by first trying Vmax = 265 ft/sec as obtained from the numerical solution. 34.304 = 1.75254 × 10 −6 (260)3 + 770.55 265 = 32.614 + 2.9077 = 35.52 Difference = 1.216 Let us try a slightly smaller value, say Vmax = 260 ft/sec. 34.304 = 1.75254 × 10 −6 (260)3 + 770.55 260 = 32.80 + 2.96 = 33.76 Difference = −0.544 Try Vmax = 262 ft/sec. 34.304 = 1.75254 × 10 −6 (262)3 + 770.55 262 = 31.519 + 2.941 = 34.46 Difference = 0.156 Try Vmax = 261 ft/sec. 34.304 = 1.75254 × 10−6 (261)3 + 770.55 261 = 31.159 + 2.952 = 34.111 Difference = −0.192 85 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Try Vmax = 261.6 ft/sec. 34.304 = 1.75254 × 10 −6 (26.61)3 + 770.55 261.6 = 31.3748 + 2.9455 = 34.32 Close enough! The analytical value for Vmax is Vmax = 261.6 ft/sec Compared with the numerical value of 265 ft/sec, a 1.3% difference. 6.37 For the CJ-1 TA = (3650) 2 = 7300 lb W = 19,815 lb TA 7300 = = 0.368 W 19,815 S = 318 ft 2 W 19,815 = = 62.3 lb/ft 2 S 318 CD ,0 = 0.02 e = 0.81 AR = (53.3) 2 /318 = 8.934 From Eq. (6.44) Vmax 2 4C TA W + W TA − D ,0 W S S W π eAR = ρ∞ CD,0 1/ 2 1/ 2 4(0.02) 2 (0.368)(62.3) + (62.3) (0.368) − (0.81)(8.934) π = (0.002377)(0.02) = 978.8 ft/sec This is to be compared with the numerical value of 975 ft/sec, a 0.3% difference. 86 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.38 From Eq. 6.53: η P − 0.8776 ( R/C )max = W max W S 1 /2 ρ∞ cD,0 ( L / D )3max 0.001648 = 159.5 hp For the CP-1, at 12,000 ft, hp = 230 0.002377 η P (0.8)(1595) (550) = 23.79 = W 2950 W 2950 = = 16.954 s 174 ρ∞ CD,0 = (0.001648)(0.025) = 4.12 × 10−5 ( L/D) max = (CD,0π eAR)1/ 2 2 CD,0 = [(0.025) π (0.8)(7.366)]1/2 = 13.606 2(0.025) 16.954 1 5 − 6.12 × 10 (13.606)3 / 2 1 = 23.79 − 0.8776(641.49) 50.188 = 23.79 = 11.217 = 12.573 ft/sec (R/C )max = (12.573)(60) = 754.4 ft/min ( R/C )max = 23.79 − 0.8776 The numerical result from Section 6.10 is 755 ft/min. The difference is 0.08%. 87 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 6.39 From Eq. (6.52) 1/ 2 ( R/C )max (W/S ) z = 3 ρ∞ CD ,0 3/ 2 2 3 T 1 − − 2 2 W max 6 2(T/W )max ( L / D)max Z For the CJ-1 (53.3) 2 = 8.934 318 W/S = 19,815 / 318 = 62.31 AR = CD,0 = 0.02 (3650)(2) 0.0011043 T = = 0.171 19.815 0.002378 W max (CD ,0π eAR)1/ 2 [(0.02)π (0.81)(8.934)]1/ 2 0.673 L = = = = 16.858 2 CD ,0 2(0.02) 0.04 D max Z = 1+ 1+ = 1+ 1+ 3 ( L/D)2max (T/W ) 2max 3 (16.858)2 (0.1711) 2 = 1 + 1 + 0.3606 = 2.166 1/ 2 ( R/C )max (62.31)(2.166) (0.1711)3/ 2 × = 3(0.0011043)(0.02) 2.166 3 − 1 − 2 2 6 2(0.1711) (16.858) 2.166 = (2.0369 × 106 )1/ 2 (0.07077)(0.5558) = 56.14 ft/sec = (56.14)(60) ft/min = 3368 ft/min This is compared to the numerical answer of 3369 ft/min given in Section 6.10. 88 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. C2 6.40 T = D = 1 2 ρ∞V∞2 S C D,0 + L π eAR (1) 88 Vmax = 229 mph = 229 = 335.87 ft/sec. 60 ft lb 0.0018975 (0.9) = 9.4795 × 105 Pmax = Pη = (1200)(550) 0.002378 sec Tmax = Pmax 9.4795 × 105 = = 2822 lb 335.87 Vmax S = 987 ft 2 AR = 9.14 e = 0.8 1 2 ρ∞V∞2 S = 1 2 (0.0018975)(335.87)2 (987) = 1.05636 × 105 lb CL = CL2 π eAR = W 25, 000 = = 0.2366 5 1 1.05636 × 10 2 ρ V S 2 ∞ ∞ (0.23666) 2 = 0.0024382 π (0.8)(9.14) From EQ. (1), 2822 = 1.05636 × 105 (CD,0 = 0.0024382) CD ,0 + 0.0024382 = 2822 = 0.0267 1.05636 × 105 CD ,0 = 0.0243 Note: This answer is consistent with the value of CD,0 for the DC-3 given in Figure 6.77. 89 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 7 7.1 CM cg = CM ac + CL (h - hac ) CM ex = CM cg - CL (h - hac ) = 0.005 - 0.05(0.03) = -0.01 7.2 1 1 2 ρ¥V¥ = (1.225)(100)2 = 6125 N/m 2 2 2 At zero lift, the moment coefficient about c.g. is q¥ = CM cg = M cg q¥ S c = -12.4 = -0.003 (6125)(1.5)(0.45) However, at zero lift, this is also the value of the moment coefficient about the a.c. CM ac = -0.003 At the other angle of attack, CL = CM cg = and L 3675 = = 0.4 q¥ S (6150)(1.5) M cg q¥ S c = 20.67 = 0.005 (6125)(1.5)(0.45) Thus, from Eq. (7.9) in the text, CM cg = CM ac + CL (h - hac ) Thus, h - hac = CM cg - CM ac CL = 0.005 - (-0.003) 0.4 h - hac = 0.02 The aerodynamic center is two percent of the chord length ahead of the center of gravity. 7.3 From the results of Problem 7.2, q¥ = 6125 N/m 2 CM ac = -0.003 h - hac = 0.02 In the present problem, the c.g. has been shifted 0.2c rearward. Hence, h - hac = 0.02 + 0.2 = 0.22 Also, CL = L q¥ S = 4000 = 0.435 (6125)(1.5) Thus, CM cg = CM ac + CL (h - hac ) CM cg = -0.003 + 0.435(0.22) = 0.0927 90 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 7.4 From Problem 7.2, we know q¥ = 6125 N/m 2 CM ac = -0.003 h - hac = 0.02 From information provided in the present problem, at α a = 5, CL = L 4134 = = 0.45 q¥ S (6125)(1.5) Hence, a = Also, VH = dCL 0.45 = = 0.09 per degree dα 5 t St (1.0)(0.4) = = 0.593 cS (0.45)(1.5) From Eq. (7.26) in the text, é a æ ¶ε ÷ö ùú CM cg = CM ac + aα a ê ( h - hac ) - VH t çç1 ÷ + VH at (it + ε o ) ç ê ¶α ÷ø úû aè ë é ù æ 0.12 ÷ö (1 - 0.42) ú + (0.593)(0.12)(2.0) CM cg = -0.003 + (0.09)(5) ê (0.02) - (0.593) çç çè 0.09 ÷÷ø ê ú ë û CM cg = -0.052 Hence, the moment is M cg = q¥ S c CM cg = (6125)(1.5)(0.45)(-0.052) M cg = -215 Nm 91 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 7.5 CM cg é a æ ¶ε ÷ö ùú = a ê (h - hac ) - VH t çç1 ÷ ê ¶α a ¶α ÷ø úû a èç ë where, from Problems 7.4 and 7.2, a = 0.09 per degree h - hac = 0.02 CM ac = -0.003 VH = 0.593 at = 0.12 ¶ε = 0.42 ¶α it = 2.08 CM cg é ù æ 0.12 ÷ö ú = -0.039 = (0.09) ê (0.02) - (0.593) çç (1 0.42) ÷ ê ú èç 0.09 ÷ø ¶α a ë û The slope of the moment coefficient curve is negative, hence the airplane model is statically stable. To examine whether or not the model is balanced, first calculate CM 0 . Thus, CM 0 = CM ac + VH at (it + ε 0 ) = -0.003 + (0.593)(0.12)(2.0 + 0) = 0.139 The trim angle of attack can be found from CM cg αe = 0 ¶α α e = -CM 0 /(¶CM cg / ¶α ) = -0.139 /(-0.039) = 3.56 CM cg = CM 0 + 7.6 This is a reasonable angle of attack, falling within the normal flight range. Hence, the airplane model is also balanced. a æ ¶ε ÷ö hn = hacwb + VH t çç1 ÷ ç ¶ε ÷ø aè From Problem 7.2, hn - hacwb = 0.02 Hence, hacwb = h - 0.02 = 0.26 - 0.02 = 0.24 æ 0.12 ÷ö hn = 0.24 + 0.593çç (1 - 0.42) çè 0.09 ÷÷ø hn = 0.70 By definition, static margin = hn - h = 0.70 - 0.26 = 0.44 92 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 7.7 δ trim = CM 0 + (¶CM cg / ¶α a )α n VH (¶CL1 / ¶δ e ) CM 0 = 0.139 (from Problem 7.5) ¶CM cg / ¶α a = -0.039 (from Problem 7.5) α n = 8° VH = 0.593 (from Problem 7.4) ¶CLt / ¶δ e = 0.04 (given) Thus, δ trim = 7.8 0.139 + (-0.039)(8) = -7.29° (0.593)(0.04) F = 1- 1 æç ¶CL1 ç at ççè ¶δ e F = 1- 1 (-0.007) (0.04) = 0.806 0.12 (-0.012) ¢ = CM CM 0 ac ab ÷÷ö ( ¶Che / ¶α1 ) ÷÷ ø ( ¶Che / ¶δ e ) + F VH at (it + ε 0 ) ¢ = -0.003 + (0.806)(0.593)(0.12)(2 + 0) = 0.112 CM 0 This is to be compared with CM 0 = 0.139 from Problem 7.5 for stick-fixed stability. a æ ¶ε ÷ö hn¢ = hacwb + F VH 1 çç1 ÷ a çè ¶α ø÷ (0.12) hn¢ = 0.24 + (0.806)(0.593) (1 - 0.42) = 0.609 (0.09) This is to be compared with hn = 0.70 from Problem 7.6 for stick-fixed stability. hn¢ - h = 0.609 - 0.26 = 0.349 Note that the static margin for stick-free is 79% of that for stick-fixed. ¢ ¶ CM cg ¶α a = -a(hn¢ - h) = -(0.09)(0.349) = -0.031 This is to be compared with a slope of −0.039 obtained from Problem 7.5 for the stick-fixed case. 93 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 7.9 Examining the above figure for a canard, let us trace through the pertinent equations in the text, modifying them appropriately for the canard configuration. Starting with Eq. (7.12) for the moment generated about the center of gravity due to the tail, the minus sign is replaced by a positive, because the tail is now ahead of the center of gravity, creating a positive moment. M cg, t = t Lt (1) Thus, Eq. (7.17) becomes CM , cg, t = VH CL,t (2) Note that the canard tail sees no downwash, and the canard is canted upward relative to the wing-body zero lift link, so Eq. (7.18) for the angle of attack of the tail becomes αt = α wb + it (3) Therefore, Eq. (7.22) is replaced by CM , cg, t = VH atα wb + VH at it (4) In turn, Eq. (7.24) for the total pitching moment becomes CM , cg = CM ,acwb + CLwb (h - hacwb ) + VH CL, t (5) Eq. (7.25) becomes CM , cg = CM , acwb + awbα wb[(h - hacwb ) + VH at ] + VH at it awb (6) Differentiating Eq. (6) with respect to angle of attack, the form that replaces Eq. (7.28) is ¶CM , cg ¶α a For static stability, é a ù = a ê h - hacwb + VH t ú êë a úû ¶ CM , cg ¶αa (7) must be negative. From Eq. (7), therefore, (h - hac wb ) + VH or, (h - hac wb ) < VH at <0 a at a From inequality (8), for the canard configuration to be statically stable, the center of gravity must be sufficiently far forward of the wing-body aerodynamic center to satisfy the inequality (8). This can readily be done in the design of a canard airplane. Indeed, to help shift the wing-body aerodynamic center rearward, helping to satisfy (8), is the reason that canard designs tend to have the wings shifted farther back on the fuselage compared to conventional rear-tail configurations. 94 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 8 8.1 hG = 400 miles = 0.644 ´ 106 rb = re + hG = 6.4 ´ 106 + 0.644 ´ 106 = 7.044 ´ 106 m k 2 = 3 / 986 ´ 1014 m3/sec2 from the text h = r 2θ = rV θ = rbV cos βb = (7.044 ´ 106 )(13 ´ 103 ) cos10° h = 9.018 ´ 1010 m 2 /sec h2 = 8.133 ´ 1021 m 4 /sec2 p = h 2 / k 2 = 8.133 ´ 1021 / 3.986 ´ 107 m This is the numerator of the orbit equation. We now proceed to find the eccentricity. The kinetic energy per unit mass is: T / m = V 2 /2 = (13 ´ 103 )2 /2 = 8.45 ´ 107 m 2 /sec2 The potential energy per unit mass is: φ / m = k 2 / rb = 3.98 ´ 1014 / 7.044 ´ 106 = 5.659 ´ 107 m 2 /sec Hence, H / m = ( T - φ ) / m = (8.45 - 5.659) ´ 107 = 2.791 ´ 107 m 2 /sec2 Thus, the eccentricity is: e = 1+ 2h2 æç H ö÷ 2(8.133 ´ 1021)(2.791 ´ 107 ) = + = 1.96 1 ÷ ç ÷ k 4 çè m ø (3.986 ´ 1014 )2 Obviously, the trajectory is a hyperbola because e > 1, and also because T > | φ |. The orbit equation is r = p 1 + e cos(θ - C ) r = 2.04 ´ 107 1 + 1.96 cos(θ - C ) The phase angle, C, is calculated as follows. Substitute the burnout location (rb = 7.044 ´ 106 m and θ = 0°) into the above equation. 2.04 ´ 107 1 + 1.96 ´ cos(-C ) cos (-C ) = 0.967 95 7.044 ´ 106 = PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Thus C = -14.76°. Hence, the complete equation of the trajectory is r = 2.04 ´ 107 1 + 1.96 cos (θ + 14.76) where θ is in degrees and r in meters. 8.2 Escape velocity = V = For Venus:V = (2)(3.24 ´ 1014 ) / 6.16 ´ 106 = 1.03 ´ 104 m/sec = 10.3 km/sec For Earth:V = (2)(3.96 ´ 1013 ) / 6.39 ´ 106 = 1.11 ´ 104 m/sec = 11.3 km/sec For Mars:V = (2)(4.27 ´ 1013 ) /106 = 5.02 ´ 103 m/sec = 5.02 km/sec For Jupiter:V = 8.3 2k 2 / r (2)(1.27 ´ 1017 ) / 7.14 ´ 107 = 5.96 ´ 104 m/sec = 56.6 km/sec G = 6.67 ´ 10-11 m3/(kg)(sec)2 M = 7.35 ´ 1022 kg GM = k 2 = (6.67 ´ 10-11)(7.35 ´ 1022 ) = 4.9 ´ 1012 m3/sec2 Orbital velocity is V = Vorbital = k 2 /r 4.9 ´ 1012 /1.74 ´ 106 = 1678 m/sec = 1.678 km/sec Escape velocity is larger by a factor of (2)1/2. Vescape = 8.4 2(1.678) = 2.37 km/sec From Kepler’s 3rd law, æ τ ö÷2 æ ö3 çç 1 ÷ = çç a1 ÷÷ ÷ ççè τ 2 ø÷÷ èçç a2 ø÷ a23 = (a1)3 (τ 2 / τ1)2 a2 = (a1)3 (τ 2 / τ1)2/3 a2 = (1.495 ´ 1011)(29.7 /1.0)2/3 = 1.43 ´ 1012 m Please note: The “distant planet” is in reality Saturn. 96 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.5 In order to remain over the same point on the Earth’s equator at all times (assuming the Earth is a perfect sphere), the satellite must have a circular orbit with a period of 24 hours = 8.64.104 sec. As part of the derivation of Kepler’s third law in the test, it was shown that æ 4π 2 ÷ö æ 2ö ÷÷ a3 = çç 4π ÷÷÷ r 3 ç 2 ÷ çè k 2 ÷÷ø èç k ø÷ τ 2 = ççç ç (Remember, the orbit is a circle.) Hence, æ k 2 ÷ö1/3 ç r = çç 2 ÷÷÷ τ 2/3 çè 4π ÷ø æ 3.956 ´ 1014 ö÷1/3 ç ÷÷ (8.64 ´ 104 ) 2/3 = 4.21 ´ 107 m r = çç ÷ çè 4π 2 ø÷ The radius of the Earth is 6.4 × 106 m. Hence, the altitude above the surface of the Earth is hG = 4.21 ´ 107 - 6.4 ´ 106 = 3.57 ´ 107 m = 35, 700 km V = Circular velocity is 8.6 k2 = r 3.956 ´ 1014 4.21 ´ 107 = 3065 m/sec æ4 ö æ4 ö m = ρ v = ρ çç π r 3 ÷÷ = (6963) çç π ÷÷ (0.8)3 = 1.4933 ´ 104 kg ÷ø çè 3 çè 3 ÷ø S = π r 2 = π (0.8) 2 = 2.01 m 2 m 1.4933 ´ 104 = = 7429 km/m3 (1)(2.01) CD S Z = g 0 /RT = 9.8 /(287)(29/88) = 0.000118 m-1 From Eq. (8.97), the density at the altitude for maximum deceleration is ρ = m kg Z sin θ = (7429)(0.000118) sin 30° = 0.4383 3 CD S m From Eq. (8.73) h =- æ 0.4383 ö÷ 1 1 n(ρ /ρ0 )= n çç ÷ = 8710 m 0.000118 çè 1.225 ø÷ Z From Eq. (8.100) dV V 2 Z sinθ (8000)2 (0.000118)(sin 30°) = E = = 694.6 m/sec 2 2e 2e dt max In terms of gs: dV 694.6 = = 70.88 gs 9.8 dt max From Eq. (8.87) V/VE = é ù (1.225) ú -êê ú ´ ° 2(7429) (0.000118) sin 30 ê ë ûú e = 0.247 V = 0.247 VE = 0.247(8000) = 1978 m/sec 97 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.7 3 Aerodynamic heating varies as V¥ . Hence: æ 36, 000 ö÷3 q2 ÷ = 2.37 = çç çè 27, 000 ø÷÷ q1 q2 = (100)(2.37) = 237 Btu/(ft 2 )(sec) 8.8 Assume the mean velocity of the earth around the sun is essentially its circular orbital velocity given by Vearth = k2 = 29.77 ´ 103 m/sec r where k2 = GM, and M is the mass of the sun. From Eq. (1) k 2 = V 2r = (29.77 ´ 103 )2 (147 ´ 109 ) = 1.30 ´ 1020 m3/sec2 The asteroid is moving at 0.9 times the escape velocity from the sun. Vasteroid = 0.9 2k 2 r To intersect with the earth, the asteroid's value of r in Eq. (2) is the same as far for the earth in Eq. (1). Hence, Vasteroid = 0.9 2(1.3 ´ 1020 ) (147 ´ 109 ) = 37.850 ´ 108 m/sec The relative head-on collision velocity, which is the velocity at which the asteroid would enter the earth's atmosphere, is Ventry = Vearth + Vasteroid = 29.77 ´ 103 + 37.85 ´ 103 = 67.62 ´ 103 m/sec = 67.62 km/sec 8.9 Earth’s radius = R = 6.4 ´ 106 m Following the nomenclature in Figure 8.18, rmin = R + (altiude above Earth’s surface) rmin = 6.4 ´ 106 + 4.17 ´ 105 = 6.817 ´ 106 m From Eq. (8.62) rmin = h2 / k 2 1+ e (1) h2 / k 2 1- e (2) and from Eq. (8.61) rmax = Combining (1) and (2) rmax = 1.00132 1+ e = = 1.0026 1- e 0.99868 rmax = rmin (1.0026) = (6.817 ´ 106 )(1.0026) = 6.8347 ´ 106 m Altitude at apogee = 6.8347 ´ 106 - 6.4 ´ 106 = 0.4347 ´ 106 m = 434.7 km 98 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.10 From Eq. (8.71), τ2 = 4π 2 3 a k2 k 2 = 3.956 ´ 1014 m3/sec2 From the solution of Problem 8.9, rmax = 6.8347 ´ 106 m rmin = 6.817 ´ 106 m r + rmin (6.8347 + 6.817) ´ 106 a = max = = 6.82585 ´ 106 m 2 2 Inserting these numbers into Eq. (8.71): τ2 = 4π2 3 4π 2 (6.82585 ´ 106 )3 a = 3.956 ´ 1014 k2 τ 2 = 3.1738 ´ 107 τ = 5634 sec τ = or, 5634 = 1.56 hr 3600 8.11 The angular momentum per unit mass is h = r 2θ . To calculate h, proceed as follows. From Eq. (8.62), rmin = h2 / k 2 1+ e or, h 2 = rmin (1 + e)k 2 From the solution of Problem 8.9, we have rmin = 6.817 ´ 106 m. Thus, h 2 = (6.817 ´ 106 )(1.00132)(3.956 ´ 1014 ) = 2.7 ´ 1021 h = 5.1965 ´ 1010 or, Because h = r 2θ , at perigee θ = 5.1965 ´ 1010 = = 1.1182 ´ 10-3 rad/sec 2 6 2 (rmin ) (6.817 ´ 10 ) h Vperigee = rminθ = (6.817 ´ 106 )(1.1182 ´ 10-3 ) = 7623 m/sec= 7.623 km/sec 99 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.12 (a) Et = V2 k2 r 2 Evaluate this equation at the perigee, where from Example 8.3, rp = 7.169 ´ 106 m , and V p = 9.026 km/sec Et = V p2 2 - k2 (9.026 ´ 103 )2 3.986 ´ 1014 = = rp 2 7.169 ´ 106 4.0734 ´ 10-7 - 5.56 ´ 107 = -1.486 ´ 10-7 joules kg (b) From Example 8.3, a = 1.341 ´ 107 m. Thus Et = - k2 3.986 ´ 1014 joules == -1.486 ´ 10-7 7 2a kg 2(1.341 ´ 10 ) The results are the same, which is to be expected. Eqs. (8.74) and (8.77) are numerically the same. 8.13 From Example 8.6, Vθ = 3432 m/sec. ævö ΔV = 2Vθ sin çç ÷÷÷ = 2(3432) sin 10° = 1191.9 m/sec çè 2 ø Comparing with the impulse calculated in Example 8.6 for a change in inclination angle of 10°, the present impulse is 1191.9/598.2 = 1.99 larger − almost twice as large for double the inclination angle change. We would expect this because, for relatively small angles (in radians) ævö v sin çç ÷÷÷ » çè 2 ø 2 100 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.14 From Example 8.7, we already have V1 = 6794 m/sec and r 2 = r1 = 1.0506 ´ 107 m a2 = rp.2 1- e = 107 = 5 ´ 107 m 1 - 0.8 Thus, 2k 2 k2 2(3.986 ´ 10)14 3.986 ´ 1014 - 2 = r2 a 1.0506 ´ 107 5 ´ 107 V2 = 8241 m/sec e1 sin θ A (0.4654) sin90° = = 0.4654 Tan β1 = 1 + e1 cos θ A 1 + 0.4654 cos90° V2 = β1 = 24.957° For orbit 2, the true anomaly of point A is found from cos θ A = cos θ A = rp, z (1 + e2 ) e2 r2 - 1 e2 1 ´ 107 (1 + 0.8) 7 (0.8)(1.0506 ´ 10 ) - 1 = 2.1416 - 1.25 = 0.8916 0.8 θ A = 26.93° Thus, Tan β 2 = e2 sin θ A (0.8)(0.4529) 0.3623 = = = 0.2115 1 + e2 cos θ 2 1 + (0.8)(0.8916) 1.7133 β 2 = 11.94° α = β1 - β 2 = 24.957 - 11.94 = 13.017° From Eq. (8.89), (ΔV ) 2 = V12 + V2 2 - 2V1V2 cosα = (6794)2 + (8241) 2 - 2(6794)(8241) cos (13.017°) = 14.379 ´ 107 - 10.91 ´ 107 = 3.469 ´ 107 Thus, ΔV = 5890 m/sec 101 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.15 From Example 8.8, V1 = 7771 m/sec and r1 = 6.6 ´ 106 m r2 = 6.4 ´ 106 + 5 ´ 105 = 6.9 ´ 106 m r + r2 6.6 ´ 106 + 6.9 ´ 106 13.5 ´ 106 a = 1 = = = 6.75 ´ 106 m 2 2 2 From Eq. (8.78), Vpt = 2k 2 k2 = r1 a 2(3.986 ´ 10)14 6.6 ´ 10 6 - (3.986 ´ 1014 ) 6.75 ´ 106 = 1.2079 ´ 108 - 0.5905 ´ 108 = 7857.5 m/sec At point 1, the required impulse to enter the Hohmann transfer orbit is ΔV1 = Vpt - V1 = 7857.5 - 7771 = 86.5 m/sec. At point 2 on orbit 2, the required spacecraft velocity is V2 = k2 = r1 3.986 ´ 1014 6.9 ´ 106 = 7600 m/sec At point 2 on the Hohmann transfer orbit, Vat = 2k 2 k2 = r1 a 2(3.986 ´ 1014 ) 6.9 ´ 106 - 3.986 ´ 1014 6.75 ´ 106 = 1.1554 ´ 108 - 0.5905 ´ 108 = 7516 m/sec At point 2, ΔV2 = V2 - Vat = 7600 - 7516 = 84 m/sec The total impulse required is ΔV = ΔV1 + ΔV2 = 86.5 + 84 = 170.5m/sec 102 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.16 From Problem 8.2, for Mars, k 2 = 4.27 ´ 1013 m3/sec2 k2 = r1 V1 = a = 4.27 ´ 1013 8 ´ 106 = 2310 m/sec r1 + r2 8 ´ 106 + 15 ´ 106 = = 11.5 ´ 106 m 2 2 2k 2 k2 = r1 a Vpt = 2(4.27 ´ 1013 8 ´ 106 - 4.27 ´ 1013 11.5 ´ 106 = 1.0675 ´ 107 - 0.3713 ´ 107 = 2638.6 m/sec At point 1, ΔV1 = Vpt - V1 = 2638.6 - 2310 = 328.6 m/sec At point 2 on orbit 2, k2 V2 = r2 4.27 ´ 1013 = 15 ´ 106 = 1687 m/sec At point 2 on the Hohmann transfer orbit, Vat = = 2k 2 r2 - k2 = a 2(4.27 ´ 1013 ) 15 ´ 106 - 4.27 ´ 1013 11.5 ´ 106 5.693 ´ 106 - 3.713 ´ 106 = 1407 m/sec ΔV2 = V2 - Vat = 1687 - 1407 = 280 m/sec. The total required impulse is ΔV = ΔV1 + ΔV2 = 328.6 + 280 = 608.6 m/sec 103 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.17 Relative to the center of mercury, at periapsis, rmin = 2, 440 + 200 = 2640 km rmax = 2, 440 + 15,193 = 17, 633 km The semi-major axis of the elliptical orbit is r +r 2640 + 17, 633 a = min max = = 10,137 km 2 2 = 1.0137 × 107 m m3 23 k 2 = GM = 6.67 × 10−11 (3.3 × 10 kg) 2 kg sec k 2 = 2.20 × 1013 m3 sec2 From Eq. 8.71 in the text: τ2 = 4 π 2 a3 k2 = 4 π 2 (1.0137 × 107 )3 2.20 × 1013 = 1.87 × 109 sec2 Hence, τ = 43243 sec Since 3600 sec = 1 hr, we have τ= 43243 = 12.01 hr 3600 8.18 From the solution of Problem 8.17, the semi-major axis is a = 1.0137 × 107m, and k2 = 2.20 × 1013 m3/sec2. At periapsis, rmin = 2640 km = 2.64 × 106 m. From the vis-viva equation, Eq. (8.78) in the text, V= 2k 2 k 2 − r a For r = rmin, the velocity at periapsis is V= 2(2.20 × 1013 ) 2.64 × 106 − 2.20 × 1013 1.0137 × 107 = 16.67 × 106 − 2.17 × 106 = 3809 m/sec = 3.809 km/sec For r = rmax, the velocity at apoapsis is V= 2(2.20 × 1013 ) 1.7633 × 10 7 − 2.17 × 106 = 2.495 × 106 − 2.17 × 106 = 570 m/sec = 0.57 km/sec 104 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 8.19 From the solution of Problem 8.18 and 8.19, at periapsis V = 3809 m/sec and rmin = 2.64 × 106m. Thus, θ = V 3809 = = 1.44 × 10−3 rad/sec rmin 2.64 × 106 The angular momentum per unit mass is h = r2 θ. Thus, h = (rmin )2 θ = (2.64 × 106 )2 (1.44 × 10−3 ) h = 1.00 × 1010 m 2 / sec The same value is obtained at the apoapsis, where V 570 = 3.2326 × 10 −5 rad/sec 1.7633 × 107 h = (rmax )2 θ = (1.7633 × 107 )2 (3.2326 × 10 −5 ) θ = rmax = h = 1.00 × 1010 m 2 / sec. This, of course, is simply verification that the angular momentum is constant for the orbit. 8.20 Eq. (8.63) is a= h 2 /k 2 1 − e2 or e = 1− h 2 /k 2 a From Problems 8.17 and 8.19, h2 k2 = (1.00 × 1010 )2 2.20 × 1013 e = 1− = 0.4545 × 107 0.4545 × 107 1.0137 × 107 = 1 − 0.448 = 0.743 8.21 Notice that the equations for a spacecraft’s trajectory in space as derived in Chapter 8 depend only on such quantities as momentum or energy per unit mass. The actual mass of the spacecraft plays a role only in the rocket booster burnout conditions at the end of launch, as shown in Section 9.10. Once the initial burnout conditions are achieved, the subsequent trajectory is governed only by the force of gravity and Newton’s second law, for which energy and momentum per unit mass are relevant. So, if you know the complete details of the orbit of a spacecraft, it is still not possible to back out the total mass of the spacecraft. 105 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 9 9.1 Following the nomenclature in the text; æ V ÷öγ p3 = ççç 2 ÷÷ = 6.751.4 = 13.0 çè V3 ÷ø p2 p3 = (13.0)(1.0) = 13.0 atm æ V ÷öγ -1 T3 = ççç 2 ÷÷ = (6.75)0.4 = 2.15 ÷ ç T2 è V3 ø T3 = (2.15)(285) = 613K The heat released per kg of fuel-air mixture is established in the text as 2.43 ´ 106 joule/kg. Hence, T4 = q + T3 where cv = 720 joule/kg°K cv 2.43 ´ 106 + 613 = 3988°K 720 p4 T = 4 p3 T3 T4 = æT ö æ 3988 ö÷ Thus, p4 = p3 ççç 4 ÷÷÷ = (13.0) çç ÷ = 84.6 atm ç çè T3 ÷ø è 613 ø÷ æ V öγ æ 1 ö÷1.4 p5 = ççç 4 ÷÷÷ = çç = 0.069 çè 6.75 ø÷÷ çè V5 ÷ø p4 p5 = (84.6)(0.069) = 5.84 atm Wcompression = p2V2 - p3V3 1- γ The volumes V2 and V3 can be obtained as follows ( x + 9.84) / x = 6.75, Thus, x = 1.71 cm Thus, V2 = π b2 4 (9.84 + 1.71) where b = bore = 11.1 cm V2 = 1118 cm3 = 1.118 ´ 10-3 m3 V3 = V2 / 6.75 = 1.118 ´ 10-3 / 6.75 = 1.66 ´ 10-4 m3 106 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Thus, p2V2 - p3V3 1-γ é (1.0)(1.118 ´ 10-3 ) - (13.0)(1.66 ´ 10-4 ) ù 1.01 ´ 105 ê úû = ë = 263 joule -0.4 p V - p4V4 = 5 5 1-γ é (5.84)(1.118 ´ 10-3 ) - (84.6)(1.66 ´ 10-4 ) ù 1.01 ´ 105 ê úû = ë -0.4 = 1897 joule Wcompression = Wpower Wpower W = Wpower - Wcomperssion = 1897 - 263 = 1634 joule 1 ηηmech (RPM) N W 120 (0.85)(0.83)(2800)(4)(1634) PA = = 1.076 ´ 105 watts 120 PA = PA = or 9.2 PA = 1.076 ´ 105 watts = 144 hp 746 watts/hp 1 ηηmech (RPM) Dpe 120 where D = π b2 4 s N= π (11.1)2 (984)(4) 4 D = 3809 cm = 3.809 ´ 10-3 m3 3 pe = pe = 120 PA ηη mech (RPM) D 120(1.076 ´ 105 ) (0.85)(0.83)(2800)(3.809 ´ 10-3 ) pe = 1.72 ´ 106 N/m 2 = 17 atm 107 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.3 First, calculate the mass flow through the engine. For simplicity, we will ignore the mass of the added fuel, and assume the mass flow from inlet to exit is constant. Evaluating conditions at the exit, ρe = pe 1.01 ´ 105 = = 0.469 kg/m3 RTe 287 (750) m = ρ eAeVe = (0.469)(0.45)(400) = 84 kg/sec At the inlet, assume standard sea level conditions. m = ρ¥ AV i i = 84 kg/sec Hence, Vj = m 84 = = 152 m/sec (1.225)(0.45) ρ¥ Ai Note: Even though the engine is stationary, it is sucking air into the inlet at such a rate that the streamtube of air entering the engine is accelerated to a velocity of 152 m/sec at the inlet. The Mach number at the inlet is approximately 0.45. Therefore, by making the assumption of standard sea level density at the inlet, we are making about a 10 percent error in the calculation of Vi . To obtain the thrust, T = m (Ve - V j ) + ( pe - p¥ ) Ae = 84(400 - 152) + (0) Ae = 20,832 N Since 1 lb = 4.448 N, we also have T = 9.4 20,832 = 4684 lb 4.448 At a standard altitude of 40,000 ft, p¥ = 393.12 lb/ft 2 ρ¥ = 5.8727 ´ 10-4 slug/ft 3 The free stream velocity is æ 88 ö V¥ = 530 çç ÷÷÷ = 777 ft/sec çè 60 ø Hence, m = ρ¥V¥ A j = (5.87 ´ 10-4 )(777)(13) = 5.93 slug/sec T = m (Ve - V¥ ) + ( pe - p¥ ) Ae T = (5.93)(1500 - 777) + (450 - 393)(10) T = 4287 + 570 = 4587 lb 108 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.5 Assume the Mach number at the end of the diffuser (hence at the entrance to the compressor) is close to zero, hence p2 can be assumed to be total pressure. M1 = V1 800 = = 0.716 1117 a1 γ /γ -1 æ p2 γ - 1 2 ÷ö M1 ÷÷ = çç1 + = [1 + (0.2)(0.616) 2 ]3.5 = 1.41 çè ø p1 2 Hence, p3 p p = 3 2 = (12.5)(1.41) = 17.6 p1 p2 p1 As demonstrated on the pressure-volume diagram for an ideal turbojet, the compression process is isentropic. Hence, æT ö p3 = ççç 3 ÷÷÷ çè T1 ø÷ p1 γ γ -1 æp ö t3 = t1 ççç 3 ÷÷÷ çè p1 ø÷ γ γ -1 = 519(17.6)0.286 = 1178° Combustion occurs at constant pressure. For each slug of air entering the combustor, 0.05 slug of fuel is added. Each slug of fuel releases a chemical energy (heat) of (1.4 ´ 107 )(32.3) = 4.51 s 108 ft lb/slug . Hence, the heat released per slug of fuel-air mixture is q = (4.51 ´ 108 )(0.05) = 2.15 ´ 107 ft lb/slug 1.05 Because the heat is added at constant pressure, q = c p (T4 - T3 ) q cp T4 = T3 + For air, c p = γR γ -1 = T4 = 1178 + 1.4(1716) ft lb = 6006 0.4 slug°R 2.15 ´ 107 = 1178 + 3580 = 4758° R 6006 Again, from the p-v diagram for an ideal turbojet, p6 p 1 = 1 = = 0.0568 17.6 p4 p3 γ Also, æ T öγ -1 p6 = ççç 6 ÷÷÷ çè T4 ø÷ p4 γ æ p öγ -1 T6 = T4 ççç 6 ÷÷÷ = 4758 (0.0568)0.286 = 2095° R çè p4 ø÷ Note: The temperatures calculated in this problem exceed those allowable for structural integrity. However, in real life, the losses due to heat conduction will decrease the temperature. Also, the fuel-air ratio would be decreased in order to lower the temperatures in an actual application. 109 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.6 T = m (Ve - V¥ ) + ( pe - p¥ ) Ae 1000 = m (2000 - 950) + 0 m = 0.952 slug/sec However, m = ρ ¥V¥ Ai m 0.952 Thus, Ai = = = 0.42 ft 2 (0.002377)(950) ρ¥V¥ 9.7 At 50 km, p¥ = 87.9 N/m 2 e + ( pe - p¥ ) Ae = (25)(4000) + (2 ´ 104 - 87.9)(2) T = mV = 100, 000 + 39,824 = 139,824 N Since 1 lb = 4.48 N 139824 = 31, 435 lb 4.448 T = 9.8 (a) At a standard altitude of 25km, p¥ = pe = 2527 N/m 2 I sp I sp 0.18 ù é æ 2527 ÷ö1.18 ú 2(1.18)(8314)(3756) êê ú ç ÷ ê 1 - ççè ú 6 ÷ø (0.18)(20) ´ 3.03 10 ê ú êë úû = 375sec 1 = g0 (b) From the isentropic relations, γ æ T öγ -1 pe = ççç e ÷÷÷ çè T0 ø÷ p0 γ -1 æp ö γ Te = T0 ççç e ÷÷÷ çè p0 ø÷ cp = æ 2527 ÷ö0.1525 = 3756 çç = 1274°K ÷ çè 3.03 ´ 106 ÷ø (1.18)(8314) γR = = 2725joule/kg°K γ -1 (0.18)(20) From the energy equation Ve = (c) pe = 2c p (T0 - Te ) = 2(2725)(3756 - 1274) = 3678 m/sec pe R 8314 joule where R = = = 415.7 20 kgK RTe M 2527 = 0.00477 kg/m3 (415.7)(1274) m = pe AeVe =(0.00477)(15)(3678)=263.5 kg/sec pe = 110 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (d) From the definition of specific impulse, T where w is the weight flow w 0 = (263.5)(9.8) = 2582 N/sec w = mg Hence, T = w Isp = (2582)(375) = 968, 250N I sp = 968250 = 217682 lb 4.448 or, T = (e) m = 263.5 = (γ +1) /(γ -1) p0 A* γ æç 2 ö÷ ÷÷ çç To R è γ + 1 ø÷ 12.11 1.18 çæ 2 ÷ö ÷ ç 415.7 çè 2.18 ø÷ (30(1.01 ´ 105 )) A* (3756)1/ 2 A* = 0.169 m 2 9.9 m = 87.6 / 32.2 = 2.72 slug/sec (γ +1) /(γ -1) p0 A* γ æç 2 ö÷ ç ÷÷ T0 R èç γ + 1 ø÷ m = p0(0.5) 6000 2.72 = 10.52 1.21 æç 2 ö÷ ÷÷ çç 2400 è 2.21 ø p0 = 31, 736 lb/ft 2 In terms of atmospheres, p0 = 9.10 Vb = g0 I sp n 9.11 31, 736 = 15 atm 2116 Mi = (9.8)(240) n 5.5 = 4009.6 m/sec Mf M f = Mi - M p Mi Mi = = Mf Mi - M p 1- 1 Mp Mi Mi V /g I = e b 0 sp = e(11,200) /(9.8)(360) = 23.9 Mf where escape velocity is 11.2 km/sec = 11,200 m/sec. 23.9 = 1Mp Mi 1 Mp Mi = 0.958 111 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.12 From Eq. (9.43) r = ap0n log r = log a + n log p0 At p0 = 500 lb/in 2: log (0.04) = log a + n log (500) log a = -1.3979 - 2.69897n or: (1) At p0 = 1000 lb/in 2: log (0.058) = log a + n log (1000) log a = -1.23657 - 3n or: (2) Solving Eqs. (1) and (1) for a and n, we have 0 = -0.16133 + 0.03103n 0.16133 n= = 0.5359 0.30103 log a = -1.23657 - 3(0.5359) = -2.84427 a = 0.0014313 Hence, the equation for the linear burning rate is r = 0.0014313 p00.5359 For p0 = 1500 lb/in 2: r = 0.0014313(1500)0.5359 = 0.0721 in/sec. In 5 seconds, the total distance receded by the burning surface is 0.0721 (5) = 0.36 in. 9.13 éM + M + M + M + M ù p1 s1 p2 s2 Lú Vb1 = g0 Isp n êê ú M s1 + M p2 + M s2 + M L êë úû 7200 + 800 + 5400 + 600 + 60 = (9.8)(275) n 800 + 5400 + 600 + 60 = 1934 m/sec éM + M + M ù p2 s2 Lú Vb2 - Vb1 = g0 Isp n êê ú + M M êë úû s2 L 5400 + 600 + 60 = (9.8)(275) n 600 + 60 = 5975 m/sec Hence: Vb2 = 5975 + 1934 = 7909 m/sec 9.14 The velocity of the jet relative to you is (Ve - V¥ ) . This is the velocity you feel of the "wind" left behind in the air after the device passes through your space. The energy it has is kinetic space. The energy it has is kinetic energy, which per unit mass is 1 (Ve - V¥ ) 2. 2 Hence, the kinetic energy deposited per unit time is 1 m (Ve - V¥ )2. 2 112 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.15 Power available = T V∞ (1) From Eq. (9.24), ignoring the pressure thrust term and assuming that m is essentially m aira T = m (Ve - V∞ ) (2) The total power generated by the propulsive device is the useful power plus the wasted power. Hence, Total power generated = T V∞ + 1 m (Ve - V∞ )2 2 (3) Thus, ηp = useful power available T V∞ = 1 2 total power generated T V∞ + m ( Ve - V∞ ) 2 (4) Substituting Eq. (2) into (4), ηp = m (Ve - V∞ ) V∞ 1 2 m (Ve - V∞ ) V∞ + m ( Ve - V∞ ) 2 (5) Dividing numerator and denominator by m (Ve - V¥ )V¥ , Eq. (5) becomes ηp = 1 1 = æ 1 Ve ö÷ 1ç 1 + (Ve - V¥ ) / V¥ ÷ 1 + ç 2 V¥ ø÷÷ 2 ççè or, ηp = 2 1 + Ve / V¥ 9.16 From Example 9.3, V¥ = 500 miles/hour = 733 ft/sec And Ve = 1600 ft/sec ηp = 2 = 1+Ve /V¥ 2 = 0.63 æ 1600 ö÷ 1 + çç ÷ çè 733 ø÷ 9.17 Briefly: (a) The flow velocity increase across the propeller is small, hence Ve is only slightly larger than V¥ , and η p is high. (b) The exit velocity of the gas from a rocket engine is supersonic. Hence, Ve is very high compared to the velocity of the rocket, V¥ , and η p is low. (c) The exit velocity from a gas turbine jet engine is usually a very high subsonic value, and sometimes a supersonic value just above one. Hence, it is less efficient than a propeller, but considerably more efficient than a rocket engine. 113 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.18 The temperature entering the compressor is T2 = 585oR. The temperature at the exit of the compressor, T3, is obtained from the isentropic relation γ −1 0.4 T3 p3 γ = = (11.7) 1.4 = (11.7)0.286 = 2.02 T2 p2 T3 = 2.02 T2 = 2.02 (585) = 1182° R Since the compressor does work, per unit mass of gas, wc, the energy equation (Eq. 4.42) is modified as V2 V2 C p T2 + 2 + Wc = C p T3 + 3 2 2 For V2 = V3, this becomes Wc = cp (T3 – T2) cp = γ R (1.4)(1716) ft lb = = 6006 γ −1 0.4 slug°R Wc = 6006 (1182 − 585) = 3.58 × 106 ft lb slug lb 200 slug = = 6.21 . sec 322 sec The total work done per second is The mass flow is 220 slug 6 ft lb 7 ft lb 6.201 3.58 × 10 = 2.22 × 10 sec slug sec Since one HP = 550 ft lb , the horsepower provided by the compressor is sec HP = 2.22 × 107 = 40,364 550 9.19 From the solution of Problem 9.18, the temperature at the entrance to the combustor is the same as the temperature at the exit of the compressor, namely T3 = 1182oR. The pressure is essentially constant through the combustor, so the total heat added per unit mass to the air (neglecting the small mass of fuel added) is q = c p (T4 − T3 ) = 6006(2110 − 1182) q = 5.57 × 106 ft lb/slug or, ft lb 1 slug ft lb q = 5.57 × 106 = 1.73 × 105 slug 32.2 lb m lb m Since the heat released per unit mass of fuel is given as 1.4 × 107 ft lb , lbm the amount of fuel mixed with each lbm of air is 1.73 × 105/1.4 × 107 = 0.0124 lbm. The mass flow of air given in Problem 9.18 is 200 lbm/sec. So the fuel rate is (0.0124)(200) = 2.48 lb m / sec 114 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.20 In the flow through the turbine, work wT is extracted from the gas and provided to driving the turbine, and hence to the compressor. From the energy equation, C p T4 + V2 V42 − WT = CPT5 + 5 2 2 Since V5 = V4, c p T5 = c p T4 − WT Since there are no mechanical losses, the work provided by the turbine is the same as the work done ft lb . Thus by the compressor, wT = wc. From the solution of Problem 9.18, wc = 3.58 × 106 slug c p T5 = c p T4 − 3.58 × 106 or, T5 = T4 − 3.58 × 106 3.58 × 106 = 2110 − 6006 cp T5 = 1514° R 9.21 First, calculate the pressure at the entrance to the nozzle, p5. From Problem 9.18, p3 = 11.7 p2 p3 = 11.7 p2 = 11.7 (2116) = 24, 757 lb ft 2 The pressure is constant through the combustor, p4 = p3 = 24,757 lb . The flow through the ft 2 turbine is isentropic. From the solution of Problem 9.20, T5 = 1514oR. Hence y 1.4 p5 T5 y −1 1514 0.4 = = = (0.71753)3.5 = 0.3129 2110 p4 T4 p5 = (0.3129) p4 = (0.3129)(24757) = 7746 lb ft 2 The expansion through the nozzle is isentropic. T6 p6 = T5 p5 y −1 y 0.4 2116 1.4 = = (0.273)0.286 = 0.690 7746 T6 = 0.690 T5 = (0.690)(1514) = 1045° R c p T5 + V52 V2 = c p T6 + 6 2 2 V62 = 2 c p (T5 − T6 ) + V52 = 2(6006)(1514 − 1045) + (1500)2 = 5.63 × 106 + 2.25 × 106 = 7.88 × 106 V6 = (7.88 × 106 )1/ 2 = 2807 ft/sec 115 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 9.22 From Problem 9.21, T6 = 1045oR and V6 = 2807 ft/sec a6 = γ RT6 = (1.4)(1716)(1045) = 1584 ft/sec M6 = 2807 = 1.77 1584 Comment: The flow at the exit of the engine is supersonic, and because of this the nozzle must be a convergent-divergent shape. Because the pressure ratio across the compressor given in Problem 9.18 is high, namely 11.7, this is a high performance turbojet engine suitable for use on supersonic airplanes, and a supersonic exit flow is a characteristic of such an engine. However, the result obtained here, namely M6 = 1.77 is a relatively high value, influenced by our assumption of no mechanical or aerodynamic losses that in real life detract from the engine performance. 9.23 From Eq. (9.25), the thrust from the engine is T = m (Ve − V∞ ) + ( pe − p∞ ) Ae . From Problem 9.18, m = 200 lb/sec. From the solution of Problem 9.21, Ve = 2807 ft/sec. Also, from Problem 9.21, pe = 2116 lb/ft2. At 36,000 ft, from App. B, T∞ = 390.53oR and p∞ = 476 lb/ft2. a6 = γ RT∞ = (1.4)(1716)(390.53) = 968.6 ft/sec At M ∞ = 2, V∞ = 2(968.6) = 1937 ft/sec The diameter of the exit is 28 inches = 2.33 ft. Hence Ae = πd2 4 = π (2.33)2 4 m = 200 lb/sec = = 4.26 ft 2 200 = 6.21 slug/sec. 32.2 Thus, from Eq. (9.25), T = (6.21)(2807 − 1937) + (2116 − 476)(4.26) = 5403 + 6986 = 12,389 lb . Comment: For the engine and the conditions treated in Problems 9.18 – 9.23, we find that the term (pe – p∞) Ae in the thrust equation is larger than the term (Ve – V∞). This is usually not the case forturbojet engines, but is the case here for the high compression ratio engine treated and the conditions chosen. 9.24 T W From Problem 9.23, T = 12,389 lb and the weight flow through the engine is 200 lb/sec (the same as the mass flow when the mass is expressed in pounds mass). Thus, Specific thrust = Specific thrust = 12,389 = 61.9 sec 200 116 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. Chapter 10 10.1 Since δ ∝ M2 , we have Re æ 20 ÷ö2 = 0.3(100) = 30 inches = 2.5ft çè 2 ÷÷ø δ M = 20 = (δ M = 2 ) çç This dramatically demonstrates that boundary layers at hypersonic Mach numbers can be very thick. 10.2 From Chapter 4 we have T0 γ -1 2 1.4 - 1 M¥ = 1 + (20)2 = 81. =1+ 2 2 T¥ At 59 km, T¥ = 258.1 K Thus: T0 = (81)(258.1) = 20,906 K Considering that the surface temperature of the sun is about 6000K, the above result is an extremely high temperature. This illustrates that hypersonic flows can be very high temperature flows. At such temperatures, the air becomes highly chemically reacting, and in reality the ratio of specific heats is no longer constant; in turn, the above equation, which assumes constant γ, is no longer valid. Because the dissociation of the air requires energy (essentially "absorbs" energy), the gas temperature at the stagnation point will be much lower than calculated above; it will be approximately 6000K. This is still quite high, and is sufficient to cause massive dissociation of the air. 10.3 Following the nomenclature of Example 10.1, φ = 57.3(s/R) = 57.3(6.12) = 28.65° θ = 90° − φ = 61.5° (a) é ù γ / γ -1 é 1 - γ + 2γ M 2 (γ + 1)2 M 2¥ ¥ ê ú ê = ê ú ê 2 p¥ γ +1 êë 4 γ M ¥ - 2(γ - 1) úû êë p0 2 ù ú ú úû é ù1.4 / 0.4 é 1 - 1.4 + 2(1.4)(18) 2 ù (2.4) 2 (18)2 ú ê ú = 417.6 = êê ú ê ú 2 2.4 ëê 4(1.4)(18) - 2(0.4) ûú ëê ûú C p, max = æ p0 ö 2 çç 2 - 1÷÷ = (417.6 - 1) = 1.836 ÷ ç 2 ç p ÷ γ M¥ è ¥ ø (1.4)(18) 2 2 (Note: This value of C p, max is only slightly smaller than the value calculated in Example 10.1, which was 1.838 for M ¥ = 25 . This is an illustration of the hypersonic Mach number independence principle, which states that pressure coefficient is relatively independent of Mach number at hypersonic speeds.) (b) From modified Newtonian: C p = C p, maxsin 2θ = (1.836 ) sin 2 ( 61.5° ) = 1.418 117 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. 10.4 From Eq. (10.11), CL = 2sin 2 α cos α dCL = (2sin 2 α )(- sin α ) + 4 cos 2 α sin α = 0 dα sin 2α = 2cos 2α = 2(1 - sin 2α ) α = 54.7° CL, max = 2 sin 2 (54.7) cos (54.7)=0.77 10.5 (a) CL = 2 sin 2α cos α CD = 2 sin 3 α + CD, 0 For small α , these become CL = 2α 2 (1) CD = 2α 3 + CD,0 (2) CL 2α 2 = CD 2 α 3 + C D, 0 (3) æC ö d ççç L ÷÷÷ (2 α 3 + C D, 0 ) 4α - 2α 2 (6α 2 ) çè CD ø÷ = =0 dα (2α 3 + CD, 0 ) 8α 4 + 4α CD, 0 - 12α 4 = 0 4α 3 = 4CD, 0 α = (CD, 0 )1/3 (4) Substituting Eq. (4) into Eq. (3): ö÷ 2(CD, 0 )2/3 2/3 0.67 ÷÷ = = = 1/3 ÷ C C 2 + (C D, 0 ) (CD, 0 )1.3 D ømax D, 0 D, 0 æC çç L ççè C Hence: æ L ÷ö çç ÷ = 0.67 /(CD, 0 )1/3 and it occurs at çè D ÷ø max α = (CD, 0 )1/ 3. 118 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission. (b) Repeating Eq.(2): CD = 2α 3 + CD, 0 (2) From the results of part (a), at (L/D)max we have α = (C, D, 0 )1/3 . Substituting this into Eq.(2), C D = 2 C D , 0 +C D , 0 = 3 C D , 0 Since CD =CD,0 +CD, 0 where CD,W is the wave drag, we have CD = CD,W + CD, 0 = 3CD,0 or, CD,W = 2 CD, 0 Wave drag = 2 (friction drag) when L/D is maximum. Or, another way of stating this is that friction drag is one-third the total drag. 119 PROPRIETARY MATERIAL. © 2012 The McGraw-Hill Companies, Inc. All rights reserved. No part of this Manual may be displayed, reproduced, or distributed in any form or by any means, without the prior written permission of the publisher, or used beyond the limited distribution to teachers and educators permitted by McGraw-Hill for their individual course preparation. A student using this manual is using it without permission.