FLOW IN A CONSTANT-AREA DUCT WITH HEAT EXCHANGE (Combustion Chambers, Heat Exchangers) Frictionless Flow in a Constant Area Duct with Heat Exchange Q/dm h1, s1 , Rx= 0 h2 , s2 , Quasi-one-dimensional flow affected by: area change, friction, heat transfer, shock C O N S T A N T Governing Equations • Cons. of mass • Cons. of mom. • Cons. of energy • 2nd Law of Thermo. Ideal Gas/Const. cp,cv • p = RT • h2-h1 = cp(T2 – T1) • s = cpln(T2/T1) - Rln(p2/p1) {1-D, Steady, FBx=0 only pressure work} A R E A H N E O A T F R E I X C C T H I A O N G CH E 12-4 Quasi-One-Dimensional, Steady, FBx = 0, dWs/dt = 0, dWshear/dt = 0, dW/dtother = 0, effects of gravity = 0, ideal gas*, cv, cp is constant Cons. Of Mass Cons. of Momentum Cons. of Energy 2nd Law of Thermodynamics Property relations for ideal gas with cv and cp constant Constant area, frictionless, heat exchange = Rayleigh Flow No Rx Constant area, frictionless, heat exchange = Rayleigh Flow If know: p 1, 1, T1, s1, h1, V1 and Q/dm Can find: p2, 2, T2, s2, h2, V2 breath TS curve C O N S T A N T N O A R E A F R I C T I O N H E A T E X C H A N G E Frictional, Constant Area, Adiabatic Flow Frictionless, Constant Area with Heat Transfer T ? Rayleigh Isentropic Flow Line s Isentropic Flow Fanno Line dA0 No Frictional, Changing Area, Adiabatic Flow s2-s1 = cpln(T1/T2)-Rln(p2/p1) Need p2/p1 in terms of T2 and T1 After manipulation eqs 12.30a – 12.30g T s Rayleigh Line For the same mass flow, each point on the curve corresponds to a different value of q added or taken away. T x s FLASHBACK - FANNO LINE, ADIABATIC & CONSTANT AREA BUT FRICTION To h1 + V12/2 = h2 + V22/2 hO1 = hO2 x T1, s1 cpTO1 = cpTO2 TO1 = TO2 s-s1 = cvln(T/T1) + ½Rln [(To-T2)/(To-T1)] RALEIGH LINE, NOT ADIABATIC & CONSTANT AREA BUT NO FRICTION q+h1+V12/2 = h2+V22/2 q = hO2 – hO1 q = cp(TO2-TO1) The effect of heat addition is to directly change the stagnation (total) temperature of the flow TS curve properties where is sonic ? C O N S T A N T A R E A N O F R I C T I O N H E A T E X C H A N G E T Rayleigh Line B dT/ds = 0 s Properties: at A – highest s at B – highest T A ds/dT = 0 Want differential form of governing equations. V = ( + )(V + V) pA – (p+ p)A = ( + ) A(V + V)2 - AV2 -p A= V A(V + V) - AV2 -p A= V A V dp/ = -VdV Momentum: dp/ = -VdV Ideal gas: p = RT dp = Rd(T) + RTd() dp/p = dT/T+ d/ Continuity: V = constant d/ + dV/V = 0 ds/dT = 0 dp/ = -VdV Tds = du + pdv (1.10a) du = d(h-pv) = dh – pdv –vdp Tds = dh – vdp = dh – dp/ Ideal gas: dh = cpdT Tds = cpdT – dp/ Tds = cpdT +VdV ds/dT = cp/T + (V/T)(dV/dT) ds/dT = cp/T + (V/T)(dV/dT) Momentum: dp/ = -VdV Ideal gas: dp/p =d/ + dT/T Continuity: d/ + dV/V = 0 -VdV/p = d/ + dT/T p = RT -VdV/(RT) = d/ + dT/T -VdV/(RT) = d/ + dT/T -VdV/(RT) = -dV/V + dT /T dV( 1/V – V/[RT]) = dT/T dV/dT = (1/T)/(1/V –V/RT) = 1 / (T/V – V/R) ds/dT = cp/T + (V/T)(dV/dT) dV/dT = 1 / (T/V – V/R) ds/dT = cp/T + (V/T) ( 1/ (T/V – V/R)) ds/dT = 0 = cp/T + (VA/T) ( 1/ (T/VA – VA/R)) -cp = VA / ([T/VA –VA/R]) -cpT/VA + cpVA/R = VA VA (1 – cp/R) = -cpT/VA VA2 = -cpT / (1 - cp/R) = cpT / (cp/R - 1) VA2 = cpRT / (cp – R) R = cp – cv; cp/cv = k VA2 = kRT so MA = VA/(kRT)1/2 = 1 At A ds/dt = 0 A T s MA = 1 At B ds/dt = 0 B T s MB = ? dT/ds = 1/ (ds/dT) dT/ds = 1/{cp/T + (V/T) ( 1/ (T/V – V/R))} 0 = (TB /VB - VB /R)/[cp/VB – cpVB/(RTB) + VB/TB] 0 = TB /VB - VB /R TB /VB = VB /R VB = (RTB)1/2 MB = VB / (kRTB) = (RTB)1/2 / (kRTB)1/2 MB = (1/k)1/2 (~ 0.715 < 1) At B ds/dt = 0 MB= (1/k)1/2 MB < 1 B T s Subsonic on top. Supersonic on bottom. What happens as you add heat? subtract heat? breath TS curve properties how does s change with q ? C O N S T A N T A R E A N O F R I C T I O N H E A T E X C H A N G E T S = rev Q/T s Entropy, s, always increases with heating and decreases with cooling. If continue to heat at A, can’t stay on Rayleigh line since s must increase, so mass flow must change, get new (lower mass flow) Rayleigh line. EFFECTS OF HEATING / COOLING ON FLUID PROPERTIES FOR RAYLEIGH FLOW Heat addition increases disorder and hence always increases entropy, whereas cooling decreases disorder and hence decreases entropy. Independent of Ma. cp ( To2 – To1 ) Heat addition increases stagnation temperature, cooling decreases stagnation temperature. Independent of Ma. TS curve properties how does V change with q ? C O N S T A N T A R E A N O F R I C T I O N H E A T E X C H A N G E To learn more about Rayleigh flow we need to also consider the energy equation. How does velocity change with Q? How does temperature change with Q? How does Mach number change with Q? q = h + dh + (V + dV)2/2 – h – V2/2 q = dh + 2VdV/2 = dh + VdV Ideal gas: dh = cpdT q = cpdT + VdV q/(cpT) = dT/T + VdV/(Tcp) Ideal gas: cp = Rk/(k-1) q/(cpT) = dT/T + (k-1)VdV/(RkT) q/(cpT) = dV/V{[V/dV][dT/T] + (k-1)V2/(RkT)} dV/V = {q/(cpT)} {[V/dV][dT/T] + (k-1)V2/(RkT)}-1 dV/V = {q/(cpT)} {[V/dV][dT/T] + (k-1)V2/(RkT)}-1 dT/dV = T/V – V/R (slide 19) [V/dV][dT/T] + (k-1)V2/(RkT) = (V/T)[T/V – V/R] + V2/(RT) – V2/(kRT) = (V/T)[T/V – V/R + V/R] – Ma = 1 - Ma dV/V = {q/(cpT)}[1 – Ma]-1 RAYLEIGH – LINE FLOW dV/V = {q/(cpT)}[1 – Ma]-1 ~0.715 A B s is + Ts diagram for frictionless flow in a constant-area duct with heat exchange s is - breath TS curve properties how does T change with q ? C O N S T A N T A R E A N O F R I C T I O N H E A T E X C H A N G E To learn more about Rayleigh flow we need to also consider the energy equation. How does velocity change with Q? How does temperature change with Q? How does Mach number change with Q? RAYLEIGH – LINE FLOW A B ? How does T change with q ? Ts diagram for frictionless flow in a constant-area duct with heat exchange RAYLEIGH – LINE FLOW T increasing with q A B Note, between A and B heating the fluid results in reducing the temperature! Not surprising if consider stagnation temperature and fluid velocity changes in this region. Ts diagram for frictionless flow in a constant-area duct with heat exchange (from Rayleigh Line) For supersonic flow, temperature increases with heating and decreases with cooling. For subsonic flow and M < 1/(k)1/2, temperature increases with heating and decreases with cooling. For subsonic flow and 1/(k)1/2 < M < 1, temperature decreases with heating and increases with cooling. breath TS curve properties how does M change with q ? C O N S T A N T N O A R E A F R I C T I O N H E A T E X C H A N G E To learn more about Rayleigh flow we need to also consider the energy equation. M = V/c How does velocity change with Q? How does temperature change with Q? How does Mach number change with Q? (from Rayleigh Line) For supersonic flow, M decreases with heating and increases with cooling. For subsonic flow, M increases with heating and decreases with cooling. <1 M = V/(kRT)1/2 breath TS curve properties how does p change with q ? C O N S T A N T A R E A N O F R I C T I O N H E A T E X C H A N G E To investigate how p depends on heat transfer, first go back to: (1st and 2nd laws, ideal gas, constant specific heats) s2 – s1 = cpln(T2/T1) – Rln(p2/p1) Keeping p constant T = Toe(s-so)/cp (from Rayleigh Line) For supersonic flow, pressure increases with heating and decreases with cooling. For subsonic flow, pressure decreases with heating and increases with cooling. (from Rayleigh Line) For supersonic flow, stagnation pressure decreases with heating and increases with cooling. For subsonic flow, stagnation pressure decreases with heating and increases with cooling. For supersonic flow, pressure increases with heating and decreases with cooling. For subsonic flow, pressure decreases with heating and increases with cooling. + p1A + (dm/dt)V1 = p2A + (dm/dt)V2 For supersonic flow, velocity decreases with heating and increases with cooling. For subsonic flow, velocity increases with heating and decreases with cooling. For supersonic flow, velocity decreases with heating and increases with cooling. For subsonic flow, velocity increases with heating and decreases with cooling. + 1V1 = 2V2 For supersonic flow, density increases with heating and decreases with cooling. For subsonic flow, density decreases with heating and increases with cooling. Rayleigh Flows Influences can propagate upstream M<1 Influences can not propagate upstream M=1 M=1 M>1 SUBSONIC SUPERSONIC NORMAL SHOCK T Rayleigh – Line Flow s Steady, frictionless flow of air through a constant area pipe. T1 = 52oC; p1 = 60 kPa (abs); T2 = 45oC; M2 = 1.0 D = 100mm; dm/dt = 1.42 kg/sec Find: 1, po1,To1,V1, M1, s2 – s1, 2, po2,To2,V2, Q/dm Know: T1 = 52oC; p1 = 60 kPa (abs); T2 = 45oC; M2 = 1.0; D = 100mm; dm/dt = 1.42 kg/sec Find: 1 (= 0.643 ) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = VA M = V/c; c = (kRT)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 2 1)/2}M Know: T1 = 52oC; p1 = 60 kPa (abs); T2 = 45oC; 1 = 0.643 kg/m3; M2 = 1.0; D = 100mm; dm/dt = 1.42 kg/sec Find: V1 (= 281 m/s) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 1V1A M = V/c; c = (kRT)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 2 1)/2}M Know: T1 = 52oC; p1 = 60 kPa (abs); T2 = 45oC; V1 = 281 m/s 1 = 0.643 kg/m3; M2 = 1.0; D = 100mm; dm/dt = 1.42 kg/sec Find: M1 (= 0.778 < 1) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 1V1A M1 = V1/c1; c1 = (kRT1)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 2 1)/2}M T1 = 52oC; p1 = 60 kPa (abs); M1=0.78; T2 = 45oC; V1 = 281 m/s To1 = 364K, 1 = 0.643 kg/m3; M2 = 1.0; dm/dt = 1.42 kg/sec Find: To1 (= 364o K) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 1V1A M1 = V1/c1; c1 = (kRT1)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To1/T1 = 1 + {(k – 2 1)/2}M1 T1 = 52oC; p1 = 60 kPa (abs); M1=0.78; T2 = 45oC; V1 = 281 m/s To1 = 364K, 1 = 0.643 kg/m3; M2 = 1.0; dm/dt = 1.42 kg/sec Find: po1 (= 89.5 kPa) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 1V1A M1 = V1/c1; c1 = (kRT1)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po1/p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) To1/T1 = 1 + {(k – 2 1)/2}M1 T1 = 52oC; p1 = 60 kPa (abs); M1=0.78; T2 = 45oC; V1 = 281 m/s, po1 = 89.5 Pa To1 = 364K, 1 = 0.643 kg/m3; M2 = 1.0; dm/dt = 1.42 kg/sec Find: V2 (= 357 m/s) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 1V1A M2 = V2/c2; c2 = (kRT2)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po1/p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) To1/T1 = 1 + {(k – 2 1)/2}M1 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s Find: 2 (= 0.51 kg/m3) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p1 = 1RT1 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po1/p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) To1/T1 = 1 + {(k – 2 1)/2}M1 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s Find: p2 (= 46.2 kPa) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po1/p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) To1/T1 = 1 + {(k – 2 1)/2}M1 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa Find: To2 (= 382oK) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po1/p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) To2/T2 = 1 + {(k – 2 1)/2}M2 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa, To2=382oK Find: po2 (= 87.5 kPa) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 2 1)/2}M2 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa, To2=382oK, po2 =87.5 kPa Find: Q/dm (=?) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 2 1)/2}M2 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa, To2=382oK, po2 =87.5 kPa Find: Q/dm (= 18 kJ/kg) Calculating Equations: h1 + V12/2 + Q/dm = h2 + V22/2 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2; h1 = cpT1; h2 = cpT2 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 2 1)/2}M2 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa, To2=382oK, po2 =87.5 kPa Find: Q/dm (= 18 kJ/kg) h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2; h01 = cpT01; h02 = cpT02 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 1)/2}M22 T1=52oC; p1=60 kPa (abs); M1=0.78; T2= 45oC; V1=281 m/s, po1= 89.5Pa, 2=0.51 kg/m3, To1=364K, 1=0.643 kg/m3; M2=1.0; dm/dt =1.42 kg/sec; V2=357m/s, p2 = 46.kPa, To2=382oK, po2 =87.5 kPa; Q/dm = 18 kJ/kg Find: s2-s1 (= 0.0532 kJ/kg-K) h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2; h01 = cpT01; h02 = cpT02 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 1)/2}M22 T s To reduce labor in solving problems, it is convenient to derive flow functions for property ratios in terms of local Mach numbers and the reference state, where the local Mach number is 1. For example p/p* = f(M), /* = f(M) Momentum equation Use critical state, M=1, as reference Want to develop expressions like p/p*, t/T*, ect.. pA –p*A = (dm/dt) (V* - V) pA + (dm/dt)V = p*A + (dm/dt)V* p +AVV/A = p* + *A*V*V*/A p + V2 = p* + *V*2 p {1 + V2/p} = p*{1 + *V*2/p*} Momentum equation Use critical state, M=1, as reference Want to develop expressions like p/p*, t/T*, ect.. p {1 + V2/p} = p*{1 + *V*2/p*} p = RT; /p = 1/RT V2/p = V2/(RT) = kV2/(kRT) = kM2 p* = *RT*; */p* = 1/RT* *V*2/p* = V2/(RT*) = kV*2/(kRT*) = k p {1 + kM2} = p*{1 + k} p/p* = {1 + kM2}/{1 + k} p/p* = (1 + k) / (1 + kM2) Continuity equation */ = V/V* = (Mc)/(M*c*) = Mc/c* = M[T/T*]1/2 Ideal gas T/T* = (p/p*)(*/) T/T* = {(1 + k)/(1 + kM2)}{M[T/T*]1/2} {T/T*}2 = {(1 + k)/(1 + kM2)}2 {M}2{T/T*} T/T* = {M(1 + k)/(1 + kM2)}2 T/T* = {M(1 + k)/(1 + kM2)}2 */ = M[T/T*]1/2 = M2(1 + k)/(1 + kM2) Local Isentropic Stagnation Properties for Ideal Gas po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 1)/2}M2 2 k/(k-1) o/ = [ 1 + {(k – 1)/2}M ] Local Isentropic Stagnation Properties for Ideal Gas po/p = [ 1 + {(k – 2 To/T = 1 + {(k – 1)/2}M 2 k/(k-1) 1)/2}M ] p*o/p* = [ 1 + {(k – 1)/2}]k/(k-1) k/(k-1) p*/p*o = 1 / [(k+1)/2] T*o/T* = 1 + {(k – 1)/2} T*/T*o = 1 / [(k+1)/2] p/p* = (1 + k) / (1 + kM2) 2 T /T = 1 + {(k – 1)/2}M o T/T* = {M(1 + k)/(1 + kM2)}2 T*/T* o = 1 / [(k+1)/2] 2 2 */ = M (1 + k)/(1 + kM ) Dimensionless stagnation temperature: To/To* = (To/T) (T/T*) (T*/To *) = (1 + {(k – 1)/2}M2)({M(1 + k)/(1 + kM2)}2) x (1 / [(k+1)/2]) = {2(k+1)M2(1+ M2 (k-1)/2)} / {(1+kM2)2} p/p* = (1 + k) / (1 + kM2) T/T* = {M(1 + k)/(1 + kM2)}2 */ = M2(1 + k)/(1 + kM2) po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) p*/p*o = 1 / [(k+1)/2]k/(k-1) Dimensionless stagnation pressure: po/po* = (po/p) (p/p*) (p*/po *) = ([1 + {(k – 1)/2}M2]k/(k-1)) ((1 + k)/(1 + kM2)) x (1 / [(k+1)/2]k/(k-1) ) = {(1+k)/(1+kM2)}{(2/(k+1))(1+ M2 (k-1)/2)}k/(k-1) example Equations for Rayleigh Flow (steady, one-dimensional, frictionless, ideal gas, constant specific heats) p/p* = (1 + k) / (1 + kM2) T/T* = {M(1 + k)/(1 + kM2)}2 */ = M2(1 + k)/(1 + kM2) po/po* = {(1+k)/(1+kM2)}{(2/(k+1))(1+ M2 (k-1)/2)}k/(k-1) To/To* = {2(k+1)M2(1+ M2 (k-1)/2)} / {(1+kM2)2} po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 1)/2}M2 M = V/c; c = (kRT)1/2; p = RT; h = cpT s2 – s1 = cpln (T2/T1) – Rln(p2/p1) h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 Equations for Rayleigh Flow (steady, one-dimensional, frictionless, ideal gas, constant specific heats) M2 = 0.90 To1 = 333K p2 = ? p1 = 1.1 Mpa (abs) M1 = 0.5 h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 dm/dt = 2V2A M2 = V2/c2; c2 = (kRT2)1/2 p2 = 2RT2; h01 = cpT01; h02 = cpT02 s2 – s1 = cpln (T2/T1) – Rln(p2/p1) po2/p2 = [ 1 + {(k – 1)/2}M22]k/(k-1) To2/T2 = 1 + {(k – 1)/2}M22 Equations for Rayleigh Flow (steady, one-dimensional, frictionless, ideal gas, constant specific heats) To1 = 333K p1 = 1.1 Mpa (abs) M1 = 0.5 M2 = 0.90 p2 = (p2/p*) (p*/p1)(p1) p2 = (2.4/2.134)(1.35/2.4)(1.1 Mpa) p2 = 696 kPa p2/p* = (1 + k) / (1 + kM22) p1/p* = (1+k) / (1 + kM12) p*/p1 = (1 + kM12) / (1 + k) To1 = 333K p1 = 1.1 Mpa (abs) M1 = 0.5 M2 = 0.90 p2 = 696 kPa example Find: T2, p2, 2, M2, po2, To2 and Q/dt First find: T1, p1, 1, M1, po1, To1, And T*, p*, *, To*, po* Find: T2, p2, 2, M2, po2, To2 and Q/dt p/p* = (1 + k) / (1 + kM2) T/T* = {M(1 + k)/(1 + kM2)}2 */ = M2(1 + k)/(1 + kM2) po/po* = {(1+k)/(1+kM2)}{(2/(k+1))(1+ M2 (k-1)/2)}k/(k-1) To/To* = {2(k+1)M2(1+ M2 (k-1)/2)} / {(1+kM2)2} po/p = [ 1 + {(k – 1)/2}M2]k/(k-1) To/T = 1 + {(k – 1)/2}M2 M = V/c; c = (kRT)1/2; p = RT; h = cpT s2 – s1 = cpln (T2/T1) – Rln(p2/p1) h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 Given: T1, p1, M1, V2, Area Find: T2, p2, 2, M2, po2, To2 and Q/dt First find: T1, p1, 1, M1, V1, po1, To1, T*, p*, V*, To*, po* 1 = p1/(RT1) = 0.661 lbm/ft3 V1 = M1c1 = M1(kRT1)1/2 = 420.6 ft/sec To1/T1 = 1 + {(k – 1)/2}M12 ; To1 = 832.7o R po1 /p1 = [ 1 + {(k – 1)/2}M12]k/(k-1) ; po1 = 212.9 psia Given: T1, p1, M1, V2, Area Find: T2, p2, 2, M2, po2, To2 and Q/dt First find: T1, p1, 1, M1, V1, po1, To1, T*, p*, V*, To*, po* p1 /p* = (1 + k) / (1 + kM12); p* = 93.8 psia T1/T* = {M1(1 + k)/(1 + kM12)}2; T* = 2001oR */1 = M2(1 + k)/(1 + kM2) {get from 2 = 1(V1/V2)} V1 /V* = M12(1 + k)/(1 + kM12) ; V* = 2193 ft/sec po1 /po* = {(1+k)/(1+kM12)}{(2/(k+1))(1+ M12(k-1)/2)}k/(k-1) po* = 177.6 psia To1/T0* = {2(k+1)M12(1+ M12(k-1)/2)} / {(1+kM12)2} To* = 2400o R Given: T1, p1, M1, V2, Area Find: T2, p2, 2, M2, po2, To2 and Q/dt Found: T1, p1, 1, M1, V1, po1, To1, T*, p*, V*, To*, po* Find: M2,T2, p2, 2, po2, To2 and Q/dt V2 /V* = M22(1 + k)/(1 + kM22) ; M2= 0.9 T2/T* = {M2(1 + k)/(1 + kM22)}2; T2 = 2049o R p2 /p* = (1 + k) / (1 + kM22); p2 = 105.5 psia po2 /po* = {(1+k)/(1+kM22)}{(2/(k+1))(1+ M22(k-1)/2)}k/(k-1) po2 = 178.3 psia To2/T0* = {2(k+1)M22(1+ M22(k-1)/2)} / {(1+kM22)2} To2 = 2381o R 2 = 1(V1/V2) = 0.139 lbm/ft3 Given: T1, p1, M1, V2, Area Find: T2, p2, 2, M2, po2, To2 and Q/dt Found: T1, p1, 1, M1, V1, po1, To1, T*, p*, V*, To*, po* Find: M2,T2, p2, 2, po2, To2 and Q/dt Q/dt = (dm/dt)(Q/dm) = (1V1A )(Q/dm) h1 + V12/2 + Q/dm = h2 + V22/2 Q/dm = h02 – ho1 = cp(To2 – T01) Q/dt = 0.66[lbm/ft2]x420.6[ft/sec]x0.5[ft2] x[0.24[BTU/lbm-R]x(2380-833)[R] =5.16x104[BTU/sec] p1 = 200 psia, T1 = 818o R, M1 = 0.3, T01 = 832.7o R, Po1 = 212.9 psia p2 = 106 psia, T2 = 2050o R, M2 = 0.9, T02 = 2380o R, Po2 = 1777.6 psia