PHYS-4420 THERMODYNAMICS & STATISTICAL MECHANICS SPRING 2006 Homework Solutions Assignment 1. Due Friday 1/27/06: 1-8, 1-11, 2-3, 2-8, 2-13, 3-3, 3-8, 3-11 1-8. E = aT + bT2 For the numbers given, 60 mv = a 200ºC + b (200ºC)2 40 mv = a 400ºC + b (400ºC)2 Multiply the top equation by 2. 120 mv = a 400ºC + b (400ºC)(200ºC) Now subtract the last two to eliminate a. – 80 mv = b (400ºC)(200ºC) = b 80000 (ºC) 2 b = – 1.0 ×10-3 mv/(ºC)2 From the first equation, 60 mv b(200C) 2 a 0.3 mv/ C b(200C) 0.3 mv/ C [1.0 103 mv/( C)2 ]( 200C) 200C a = 0.50 mv/(ºC) Then, E = [0.50 mv/(ºC)] T – [1.0 ×10-3 mv/(ºC)2] T2 For E = 30 mv, this becomes, 30 mv = [0.50 mv/(ºC)] T – [1.0 ×10-3 mv/(ºC)2] T2, or T2 – (500ºC)T + 30000 (ºC)2 = 0 This has solutions T 250C (250C)2 30000(C)2 250C 180.3C . The data shows that emf decreases as temperature increases, so only the positive sign makes sense. T = 430.3ºC 1-11. a) T(ºC) = T(K) – 273.15 K = 77.35 K – 273.15 K b) T(ºF) = (9/5)(T(ºC) + 32ºF = (9/5)(– 195.80ºC) + 32ºF c) T(R) = T(ºF) + 459.67 R = – 320.44ºF + 459.67 R T(ºC) = – 195.80ºC T(ºF) = – 320.44ºF T(R) = 139.23 R 2-3. a) P = Av, and from the ideal gas law, v RT RT P2 , so P A . Then, A . P P RT A P12 RT1 b) Pv A A , but P = Av, so T v 2 . Then, T1 v12 . R R R A A A Now, T2 v22 (2v1 ) 2 4 v12 4T1 4(200 K) T2 = 800 K R R R c) From the ideal gas law, T 1 v 2-8. a) v T P P a RT RTv T v v e From the cyclical relation , , and P . vb P T P v T R RTv RT RTv a P e e 2 vb T v v b RT v a a RT RTv RT RTv a P e e 2 2 vb v T (v b) RTv a a R RTv RT RTv a P a e e 1 2 vb vb v T v RT v RTv a a T a P RT RTv RT RTv a T P e e v b Rv 2 2 2 v T (v b ) vb RTv a a 1 1 v 1 RTv v T P v T a v b Rv 2 a 1 a a 1 2 2 1 v RTv v RTv T 1 a T 1 a 2 v b RTv 2 v b RTv b) For an ideal gas, v 1 v 1 RT RT , so v T P v T P P 1R R 1 . P v P RT T 2-13. The volume that will spill equals the increase in volume of the water. V = V0[1 + (T – T0)], so V= V – V0 = V0(T – T0). V= (250 cm³)(0.21 ×10-3 K-1)(50ºC – 20ºC) = (250 cm³)(0.21 ×10-3 K-1)(30 K) V= 1.575 cm³ = 1.58 cm³ 3-3. a) nRT nRT AV , and , and P = AV. Then, V V AV22 A(V1 / 2) 2 1 AV12 1 AV12 , and T2 T1 . T1 nR nR 4 nR 4 nR b) PV = nRT, so P T AV 2 . nR T2 = ¼ T1 V2 V 2 A c) W PdV A VdV A [V22 V12 ] V V 2 2 V nRT nRT From part b), A 2 2 1 . Since P = AV, V2 = ½ V1 . Then, V V1 V2 V2 1 1 1 2 nRT1 2 1 nRT1 3 A 2 nRT1 V1 2 2 W [V2 V1 ] V 1 V1 2 2 1 2 2V1 2 2 4 4 2V1 3 W nRT1 8 3-8. a) Ub – Ua = U = Qacb – Wacb U = 80 J – 30 J = 50 J Qadb = U + Wadb = 50 J + 10 J b) For this path, U = Ua – Ub = – 50 J Q = U + W = – 50 J – 20 J Qadb = 60 J Q = – 70 J c) Qad = Uad + Wad ; Uad = Ud – Ua = 40 J; Qad = Uad + Wad = 40 J + 10 J Wad = Wadb = 10 J, since Wdb = 0. Qad = 50 J Qdb = Udb + Wdb = Udb; Udb = (Ub – Ua) – (Ud – Ua) = 50 J – 40 J = 10 J Qdb = 10 J 3-11. a) V = AP + B, so V1 = AP1 + B and V2 = AP2 + B. Subtracting the two equations, V V 1 m3 1.8 m3 V1 – V2 = A(P1 – P2), so A 1 2 P1 P2 1 bar 12 bar A = – 1.6 m3/bar = – 1.6 ×10-5 m3/Pa V1 = AP1 + B, so B = V1 – AP1 = 1 m3 – (– 1.6 m3/bar)(1 bar) b) PV = nRT, so B = 2.6 m3 1 bar (1.8 m3 ) T 0.9 T 0.9(300 K) P1V1 T1 PV , so T2 2 2 T1 2 1 1 P2V2 T2 P1V (1 bar)(1 m3 ) T2 = 270 K V2 P2 c) W PdV , and V = AP + B, so dV = AdP. Then, W A PdP V1 P1 A 2 1.6 m /bar 1 P2 P12 [( 2 bar) 2 (1 bar) 2 ] 0.6 bar m3 2 2 3 5 W = (0.6 bar·m )(10 Pa/bar) = 6 ×104 N·m W = 6 ×104 J P2 W A PdP P1 3 d) Q = W + U = 6 ×104 J + (800 J/K)(270 K – 300 K) Q = 3.6 ×104 J