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Updated June 2013 8e SOLUTION MANUAL CHAPTER 14 Fundamentals of Thermodynamics Borgnakke Sonntag Borgnakke Sonntag Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. CONTENT CHAPTER 14 SUBSECTION PROB NO. In-Text-Concept-Questions a-g Concept-Study Guide Problems 1-17 Equilibrium and Phase Equilibrium 18-21 Chemical Equilibrium, Equilibrium Constant 22-74 Simultaneous Reaction 75-86 Gasification 87-93 Ionization 94-99 Applications 100-108 Review Problems 109-117 English Unit Problems 118-144 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. In-Text Concept Questions Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.a For a mixture of O2 and O the pressure is increased at constant T; what happens to the composition? An increase in pressure causes the reaction to go toward the side of smaller total number of moles, in this case toward the O2 . 14.b For a mixture of O2 and O the temperature is increased at constant P; what happens to the composition? A temperature increase causes more O2 to dissociate to O. 14.c For a mixture of O2 and O I add some argon keeping constant T, P; what happens to the moles of O? Diluting the mixture with a non-reacting gas has the same effect as decreasing the pressure, causing the reaction to shift toward the side of larger total number of moles, in this case the O. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.d When dissociations occur after combustion, does T go up or down? Dissociation reactions of combustion products lower the temperature. 14.e For nearly all the dissociations and ionization reactions what happens with the composition when the pressure is raised? The reactions move towards the side with fewer moles of particles, that is ions and electrons towards the monatomic side and monatomic species combine to form the molecules (diatomic or more) Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.f How does the time scale for NO formation change when P is lower at same T? Look at the expression for the time scale in Eq.14.40. As P is lowered the time scale becomes larger. The formation rates drops, and the effect is explained by the larger distance between the molecules/atoms (density lower), the same T essentially means that they have the same characteristic velocity. 14.g Which atom in air ionizes first as T increases? What is the explanation? Using Fig. 14.11, we note that as temperature increases, atomic N ionizes to N+, becoming significant at about 6-8000 K. N has a lower ionization potential compared to O or Ar. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. Concept-Study Guide Problems Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.1 Is the concept of equilibrium limited to thermodynamics? Equilibrium is a condition in which the driving forces present are balanced, with no tendency for a change to occur spontaneously. This concept applies to many diverse fields of study – one no doubt familiar to the student being that of mechanical equilibrium in statics, or engineering mechanics. 14.2 How does Gibbs function vary with quality as you move from liquid to vapor? There is no change in Gibbs function between liquid and vapor. For equilibrium we have gg = gf. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.3 How is a chemical equilibrium process different from a combustion process? Chemical equilibrium occurs at a given state, T and P, following a chemical reaction process, possibly a combustion (which is a chemical reaction process) together with several reactions amongst the combustion products. Whereas the combustion is a one-way process (irreversible) the chemical equilibrium is a reversible process that can proceed in both directions. 14.4 Must P and T be held fixed to obtain chemical equilibrium? No, but we commonly evaluate the condition of chemical equilibrium at a state corresponding to a given temperature and pressure. If T and P changes in a process it means that the chemical composition adjusts towards equilibrium and the composition changes along with the process. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translationof this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.5 The change in Gibbs function ∆Go for a reaction is a function of which property? The change in Gibbs function for a reaction ∆G is a function of T and P. The change in standard-state Gibbs function ∆Go is a function only of T. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.6 In a steady flow burner T is not controlled, which properties are? The pressure tends to be constant, only minor pressure changes due to acceleration of the products as density decreases velocity must increase to have the same mass flow rate. The product temperature depends on heat losses (radiation etc.) and any chemical reactions that may take place generally lowering the temperature below the standard adiabatic flame temperature. 14.7 In a closed rigid combustion bomb which properties are held fixed? The volume is constant. The number of atoms of each element is conserved, although the amounts of various chemical species change. As the products have more internal energy but cannot expand the pressure increases significantly. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.8 Is the dissociation of water pressure sensitive? Yes, since the total number of moles on the left and right sides of the reaction equation(s) is not the same. 14.9 At 298 K, K = exp(−184) for the water dissociation, what does that imply? This is an extremely small number, meaning that the reaction tends to go strongly from right to left – in other words, does not tend to go from left to right (dissociation of water) at all. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.10 If a reaction is insensitive to pressure prove that it is also insensitive to dilution effects at a given T. Assume the standard reaction we used to develop the expression for the equilibrium constant: νA A + νB B ⇔ νC C + νD D let us assume we add an inert component E so the total moles become: ntot = nA + nB + nC + nD + n E This will now lower the mole fractions of A, B, C, and D. If the reaction is pressure insensitive then: νA + νB = νC + νD and the equilibrium equation becomes: K = y νC C y νD D y νA A y νB B P Po νC + νD − νA − νB = C y νD D y νA A y νB B y νC Since each yi = ni / ntot we get: K = y νC C y νD D y νA A y νB B = (nC/ntot) νC (nD/ntot) νD (nA/ntot) νA (nB/ntot) νB = n νC C n νD D n νA A n νB B ntot νA + νB − νC − νD = C n νD D n νA A n νB B n νC Now we see that the total number of moles that includes nE does not enter the equation and thus will not affect any progress of the reaction. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.11 For a pressure sensitive reaction an inert gas is added (dilution), how does the reaction shift? Assume the standard reaction we used to develop the expression for the equilibrium constant: νA A + νB B ⇔ νC C + νD D let us assume we add an inert component E so the total moles become: ntot = nA + nB + nC + nD + n E This will now lower the mole fractions of A, B, C, and D. If the reaction is pressure sensitive then: νA + νB ≠ νC + νD and the equilibrium equation becomes: K = y νC C y νD D y νA A y νB B P Po νC + νD − νA − νB Since each yi = ni / ntot we get: K = (nC/ntot) νC (nD/ntot) νD (nA/ntot) νA (nB/ntot) νB P Po νC + νD − νA − νB = n νC C n νD D n νA A n νB B P Po ntot νC + νD − νA − νB As ntot is raised due to nE it acts as if the pressure P is lowered thus pushing the reaction towards the side with a larger number of moles. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.12 In a combustion process is the adiabatic flame temperature affected by reactions? The adiabatic flame temperature is lower due to dissociation reactions of the products as those products absorb some of the energy, i.e. 2 O atoms have more energy, h = 2(249 170 + ∆h) than a single O2 molecule, h = ∆h, see Table A.9. The temperature is also influenced by other reactions like the water gas reaction. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.13 In equilibrium Gibbs function of the reactants and the products is the same; how about the energy? The chemical equilibrium mixture at a given T, P has a certain total internal energy. There is no restriction on its division among the constituents. The conservation of energy from the reactants to the products will determine the temperature so if it takes place in a fixed volume (combustion bomb) then U is constant whereas if it is in a flow (like a steady flow burner) then H is constant. When this is combined with chemical equilibrium it is actually a lengthy procedure to determine both the composition and the temperature in the actual process. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profitbasis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.14 Does a dissociation process require energy or does it give out energy? Dissociation reactions require energy and is thus endothermic. Notice from Table A.9 that all the atoms (N, O, H) has a much higher formation enthalpy than the diatomic molecules (which have formation enthalpy equal to zero). Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.15 If I consider the non-frozen (composition can vary) specific heat, but still assume all components are ideal gases, does that C become a function of temperature? of pressure? The non-frozen mixture heat capacity will be a function of both T and P, because the mixture composition depends on T and P, while the individual component specific heat capacities depend only on T. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.16 What is K for the water gas reaction in Example 14.4 at 1200 K? Using the result of Example 14.4 and Table A.11 ln K = 1 2 ( ln KI – ln KII ) = 0.5 [–35.736 – (–36.363)] = + 0.3135 , K = 1.3682 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.17 What would happen to the concentrations of the monatomic species like O, N if the pressure is higher in Fig. 14.11 Since those reaction are pressure sensitive (more moles on RHS than on LHS) the higher pressure will push these reactions to the left and reduce the concentrations of the monatomic species. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. Equilibrium and Phase Equilibrium Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.18 Carbon dioxide at 15 MPa is injected into the top of a 5-km deep well in connection with an enhanced oil-recovery process. The fluid column standing in the well is at a uniform temperature of 40°C. What is the pressure at the bottom of the well assuming ideal gas behavior? Z 1 Z 2 CO 2 cb (Z1 − Z2) = 5000 m, P1 = 15 MPa T = 40 oC = constant Equilibrium at constant T −wREV = 0 = ∆g + ∆PE = RT ln (P2/P1) + g(Z2 − Z1) = 0 ln (P2/P1) = 9.807×5000 1000×0.188 92×313.2 = 0.8287 P2 = 15 MPa exp(0.8287) = 34.36 MPa Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.19 Consider a 2-km-deep gas well containing a gas mixture of methane and ethane at a uniform temperature of 30oC. The pressure at the top of the well is 14 MPa, and the composition on a mole basis is 90% methane, 10% ethane. Each component is in equilibrium (top to bottom) with dG + g dZ = 0 and assume ideal gas, so for each component Eq.14.10 applies. Determine the pressure and composition at the bottom of the well. Z 1 Z 2 mixture cb Gas A + B (Z1 − Z2) = 2000 m, Let A = CH4, B = C2H6 P1 = 14 MPa, yA1 = 0.90, yB1 = 0.10 T = 30 oC = constant From section 14.1, for A to be at equilibrium between 1 and 2: WREV = 0 = nA(G - A1 − G - A2) + nA MA g (Z1 − Z2) Similarly, for B: WREV = 0 = nB(G - B1 − G - B2) + nB MB g (Z1 − Z2) Using eq. 14.10 for A: R- T ln (PA2/PA1) = MA g (Z1 − Z2) with a similar expression for B. Now, ideal gas mixture, PA1 = yA1P, etc. Substituting: ln yA2P2 yA1P1 = MAg(Z1-Z2) R- T and ln yB2P2 yB1P1 = MBg(Z1-Z2) R- T ln (yA2 P2) = ln(0.9×14) + 16.04×9.807(2000) 1000×8.3145×303.2 = 2.6585 => yA2 P2 = 14.2748 ln (yB2P2) = ln(0.1×14) + 30.07×9.807(2000) 1000×8.3145×303.2 = 0.570 43 => yB2 P2 = (1 − yA2) P2 = 1.76903 Solving: P2 = 16.044 MPa & yA2 = 0.8897 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.20 A container has liquid water at 20oC , 100 kPa in equilibrium with a mixture of water vapor and dry air also at 20oC, 100 kPa. How much is the water vapor pressure and what is the saturated water vapor pressure? From the steam tables we have for saturated liquid: Pg = 2.339 kPa, vf = 0.001002 m 3/kg The liquid is at 100 kPa so it is compressed liquid still at 20oC so from Eq.14.15 at constant T gliq – gf = ⌡⌠ v dP = vf (P – Pg) The vapor in the moist air is at the partial pressure Pv also at 20 oC so we assume ideal gas for the vapor gvap – gg = ⌡⌠ v dP = RT ln Pg Pv We have the two saturated phases so gf = gg ( q = hfg = Tsfg ) and now for equilibrium the two Gibbs function must be the same as gvap = gliq = RT ln Pv Pg + gg = vf (P – Pg) + g f leaving us with ln Pv Pg = vf (P – Pg)/ RT = 0.001002 (100 - 2.339) 0.4615 × 293.15 = 0.000723 Pv = Pg exp(0.000723) = 2.3407 kPa.This is only a minute amount above the saturation pressure. For the moist air applications in Chapter 11 we neglected such differences and assumed the partial water vapor pressure at equilibrium (100% relative humidity) is Pg. The pressure has to be much higher for this to be a significant difference. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.21 Using the same assumptions as those in developing Eq. d in Example 14.1, develop an expression for pressure at the bottom of a deep column of liquid in terms of the isothermal compressibility, βT. For liquid water at 20 oC, βT = 0.0005 [1/MPa]. Use the result of the first question to estimate the pressure in the Pacific ocean at the depth of 3 km. d gT = v° (1 − βTP) dPT d gT + g dz = 0 v° (1 − β EEA⌡⌠v°(1-β AT AP) dP AT AEA = − g A⌡⌠dzE TP) dPT + g dz = 0 and integrate EEEA ⌡ ⌠ P A0 A E P (1-β ATAP) dP AT AEA = + A g v° EA A⌡ ⌠ 0 +HdzE A => P - P A0 EA - β ATE A A 1 2EA [P A 2 E A − PA0 EAA 2 E A] = A g v° EA H P (1 − A 1 2EA β ATE A P) = P A0 EA − A 1 2EAβATE A P A0 EAA 2 E A + A g v°EA H v° = vAf 20°CEA = 0.001002; H = 3000 m, g = 9.80665 m/s A 2 E A; β ATE A = 0.0005 1/MPa P (1 − A12 EA × 0.0005 P) = 0.101 − A 1 2 EA × 0.0005 × 0.101A 2 E A + [9.80665 × 3000/0.001002] × 10A-6E = 29.462 MPa, which is close to P Solve by iteration or solve the quadratic equation P = 29.682 MPa Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. Chemical Equilibrium, Equilibrium Constant Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.22 Which of the reactions listed in Table A.11 are pressure sensitive? Check if: νAAE A + ν AB EA ≠ ν ACE A + νAD E Reaction Check P sensitive? HA2 EA ⇔ 2H 1 < 2 yes OA2 EA ⇔ 2O 1 < 2 yes NA2 EA ⇔ 2N 1 < 2 yes 2 HA2 EAO ⇔ 2 HA2 EA + 1 OA2 EA 2 < 3 yes 2 HA2 EAO ⇔ 2 HA2 EA + 2 OH 2 < 4 yes 2 COA2 EA ⇔ 2 CO + 1 OA2 EA 2 < 3 yes NA2 EA + OA2 EA ⇔ 2 NO 2 = 2 no NA2 EA + 2OA2 EA ⇔ 2 NOA2 EA 3 > 2 yes Most of them have more moles on RHS and thus will move towards the RHS if the pressure is lowered. Only the last one has the opposite and will move towards the LHS if the pressure is lowered. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.23 Calculate the equilibrium constant for the reaction OA2 EA ⇔ 2O at temperatures of 298 K and 6000 K. Verify the result with Table A.11. Reaction OA2 EA ⇔ 2O At 25 Ao EAC (298.15 K): ∆HA0 EA = 2Ah-E AA0f OE A − 1Ah -E AA 0 f O2 E A = 2(249 170) − 1(0) = 498 340 kJ/kmol ∆S A0 EA = 2As-E AA0OEA − 1As -E AA 0 O2 EA = 2(161.059) − 1(205.148) = 116.97 kJ/kmol K ∆GA0 EA = ∆HA0 EA − T∆S A0 EA = 498 340 − 298.15×116.97 = 463 465 kJ/kmol ln K = − A ∆G0 ER- TE A = − A 463 465 8.3145×298.15EA = −186.961 At 6000 K: ∆HA0 EA = 2(249 170 + 121 264) − (0 + 224 210) = 516 658 kJ/kmol ∆S A0 EA = 2(224.597) −1(313.457) = 135.737 kJ/kmol K ∆GA0 EA = 516 658 − 6000×135.737 = −297 764 kJ/kmol ln K = A +297 764 8.3145×6000E A = +5.969 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.24 Calculate the equilibrium constant for the reaction HA2 EA ⇔ 2H at a temperature of 2000 K, using properties from Table A.9. Compare the result with the value listed in Table A.11. From Table A.9 at 2000 K we find: E∆h - HA2 A = 52 942 kJ/kmol; E s - HA2 A = 188.419 kJ/kmol K; Ah −o EfE A = 0 ∆h - H = 35 375 kJ/kmol; s - H = 154.279 kJ/kmol K; Ah −o EfE A = 217 999 kJ/kmol ∆GA0 EA = ∆H − T∆S = HARHSE A − HALHSE A – T (S A 0 E AARHSE A − S A 0 E AALHSE A) = 2 × (35 375 + 217 999) – 52943 – 2000(2×154.279 - 182.419) = 213 528 kJ/kmol ln K = −∆GA0 EA/AR -E AT = −213 528 / (8.3145 × 2000) = −12.8407 Table A.11 ln K = −12.841 OK Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.25 For the dissociation of oxygen, OA2 EA ⇔ 2O, around 2000 K we want a mathematical expression for the equilibrium constant K(T). Assume constant heat capacity, at 2000 K, for OA2 EA and O from Table A.9 and develop the expression from Eqs. 14.12 and 14.15. From Eq.14.15 the equilibrium constant is K = exp( − A ∆G0 ER−TE A ) ; ∆GA0 EA = ∆HA0 EA – T ∆S A0 E and the shift is ∆GA0 EA = 2 h-O - h - O2 - T(2s -o O – s -o O2) Substitute the first order approximation to the functions Ah-E A and As-o EA as Ah-E A = h-2000 K + C − p (T – 2000) ; As -o E A = s-o2000 K + C − p ln A T 2000E The properties are from Table A.9 and AR− E A = 8.3145 kJ/kmol K Oxygen OA2 EA: h - 2000 K = 59 176 kJ/kmol, s -o 2000 K = 268.748 kJ/kmol K C−p = h-2200 K − h - 2200 K 2200 - 1800 = A 66 770 − 51 674 400E A = 37.74 kJ/kmol K Oxygen O: h-2000 K = 35 713 + 249 170 = 284 883 kJ/kmol, s-o2000 K = 201.247 kJ/kmol K C−p = h-2200 K − h - 2200 K 2200 - 1800 = A 39 878 − 31 547 400E A = 20.8275 kJ/kmol K Substitute and collect terms A ∆G0 ER−TE A = A ∆Η0 ER−TE A – A ∆S0 ER− E A = A ∆Η 0 2000 ER−TE A + A ∆C−p 2000 ER− E A [ AT − 2000TE A – ln A T2000EA] – A ∆S02000ER− E Now we have ∆HA02000E A/ AR − E A = (2 × 284 883 – 59 176)/8.3145 = 61 409.6 K ∆AC−p 2000EA/ AR − E A = (2 × 20.8275 – 37.74)/8.3145 = 0.470864 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. ∆S A02000EA/ AR − E A = (2 × 201.247 – 268.748)/8.3145 = 16.08587 so we get A ∆G0 ER−TE A = A 61 409.6 TE A + 0.470864 [ A T − 2000 TE A – ln A T 2000EA ] – 16.08587 = A 60 467.9 TE A – 15.615 – 0.470864 ln A T 2000E Now the equilibrium constant K(T) is approximated as K(T) = exp [ 15.615 – A60 467.9TE A + 0.470864 ln A T 2000EA ] Remark: We could have chosen to expand the function ∆GA0 EA/ AR− E AT as a linear expression instead or even expand the whole exp(-∆GA0 EA/ AR− E AT) in a linear function. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.26 Find K for: COA2 EA ⇔ CO + 1/2OA2 EA at 3000 K using A.11 The elementary reaction in A.11 is : 2COA2 EA ⇔ 2CO + OA2 E so the wanted reaction is (1/2) times that so K = K1/2A.11 = A exp(-2.217)E A = A 0.108935EA = 0.33 or ln K = 0.5 ln KA.11 = 0.5 (−2.217) = −1.1085 K = exp(−1.1085) = 0.33 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.27 Plot to scale the values of ln K versus 1/T for the reaction 2 COA2 EA ⇔ 2 CO + OA2 EA. Write an equation for ln K as a function of temperature. 2 COA2 EA ⇔ 2 CO + 1 OA2 E T(K) 10A4 EA × A 1 TE ln K T(K) 10A4 EA × A 1 TE ln K 2000 5.000 -13.266 4000 2.500 3.204 2400 4.167 -7.715 4500 2.222 4.985 2800 3.571 -3.781 5000 2.000 6.397 3200 3.125 -0.853 5500 1.818 7.542 3600 2.778 1.408 6000 1.667 8.488 For the range below ~ 5000 K, ln K ≈ A + B/T Using values at 2000 K & 5000 K A = 19.5056 B = -65 543 K 8 4 0 -4 -8 -12 1 2 3 4 5 0 1 almost linear 10 T _ x 4 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.28 Consider the reaction 2 COA2 EA ⇔ 2 CO + OA2 EA obtained after heating 1 kmol COA2 EA to 3000 K. Find the equilibrium constant from the shift in Gibbs function and verify its value with the entry in Table A.11. What is the mole fraction of CO at 3000 K, 100 kPa? From Table A.9 we get: ∆h - CO = 93 504 Ah -E AA 0 f COE A = -110 527 s - CO = 273.607 E∆h - COA2 A = 152 853 Ah-E AEA 0 f COA2 AEA = -393 522E s - COA2 A = 334.17 E∆h - OA2 A = 98 013 E s - OA2 A = 284.466 ∆GA0 EA = ∆H - T∆S = 2 HACOEA + HEAOA2 AE A – 2 HEACOA2 AE A- T (2s - CO +E s - OA2 A - E2s - COA2 A ) = 2 (93 504 – 110 527) + 98 013 + 0 – 2(152 853 - 393 522) -3000(2×273.607 + 284.466 - 2×334.17) = 55 285 ln K = -∆GA0 EA/ AR -E AT = -55 285/ (8.31451×3000) = -2.2164 Table A.11 ln K = -2.217 OK At 3000 K, 2 COA2 EA ⇔ 2 CO + 1 OA2 E ln K = -2.217 Initial 1 0 0 K = 0.108935 Change -2z +2z +z Equil. 1-2z 2z z We have P = P Ao EA = 0.1 MPa, and nAtotEA = 1 + z, so from Eq.14.29 K = A yCOE 2 yO2 yCO2 2 E A (A P P0 E A) = A 2z 1 - 2z 2 E A A z 1 + z E A (1) = 0.108935 ; 4 zA3 EA = 0.108935 (1 – 2z)A2 EA(1 + z) => z = 0.22 yACOEA = 2z / (1 + z) = 0.36 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.29 Carbon dioxide is heated at 100 kPa. What should the temperature be to see a mole fraction of CO as 0.25? For that temperature, what will the mole fraction of CO be if the pressure is 200 kPa? 2 COA2 EA ⇔ 2 CO + 1 OA2 E Initial 1 0 0 Change -2z +2z +z Equil. 1-2z 2z z We have P = P Ao EA = 0.1 MPa, and nAtotEA = 1 + z, so from Eq.14.29 yACOEA = A 2z 1 + z EA = 0.25 => z = 1/7 K = A yCOE 2 yO2 yCO2 2 E A (A P P0 E A) = A 2z 1 - 2z 2 E A A z 1 + z E A (1) = A 2 7 - 2 2 E A A 1 7 + 1E A = 0.02 ln K = - 3.912 from A.11 T = 2785 K K = 0.02 = A yCOE 2 yO2 yCO2 2 E A (A P P0 E A) = A 2z 1 - 2z 2 E A A z 1 + z E A (2) => zA3 EA = 0.0025 (1 – 2z)A2 EA(1 + z) => z = 0.11776 yACOEA = A 2z 1 + z EA = 0.2107 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.30 Assume a diatomic gas like OA2 EA or NA2 EA dissociate at a pressure different from P Ao EA. Find an expression for the fraction of the original gas that has dissociated at any T assuming equilibrium. Look at initially 1 mol Oxygen and shift reaction with x OA2 EA ⇔ 2 O Species OA2 E O Initial 1 0 Change –x 2x Equil. 1–x 2x nAtotEA = 1 – x + 2x = 1 + x yAOEA = A 2x 1 + xEA and yAO2 EA = A 1 – x 1 + xE Substitute this into the equilibrium equation as KATE A = A yOE 2 y02 E A (A PPo E A)A2-1EA = A 4x 2 E(1 + x)2EA A 1 + x 1 – x E A (A P Po E A) = A 4x 2 E1 – x2E A (A P Po E A) Now solve for x as xA2 EA = (1 – x A2 EA) KTPo 4P x = KT 4(P/Po) + KT Borgnakke and Sonntag Excerpts from this work may be reproduced by instructorsfor distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.31 Hydrogen gas is heated from room temperature to 4000 K, 500 kPa, at which state the diatomic species has partially dissociated to the monatomic form. Determine the equilibrium composition at this state. HA2 EA ⇔ 2 H Equil. nAH2 EA = 1 - x -x +2x nAH EA = 0 + 2x n = 1 + x K = A (2x)2 E(1-x)(1+x)EA (A P P0 E A) A2-1EA at 4000 K: ln K = 0.934 => K = 2.545 A 2.545 4×(500/100)EA = 0.127 25 = A x2 E1-x2E A Solving, x = 0.3360 nAH2 EA = 0.664, nAH EA = 0.672, ntot = 1.336 yAH2 EA = 0.497, yAH EA = 0.503 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.32 Consider the dissociation of oxygen, OA2 EA ⇔ 2 O, starting with 1 kmol oxygen at 298 K and heating it at constant pressure 100 kPa. At which temperature will we reach a concentration of monatomic oxygen of 10%? Look at initially 1 mol Oxygen and shift reaction with x OA2 EA ⇔ 2 O Species OA2 E O Initial 1 0 Change -x 2x Equil. 1-x 2x nAtotEA = 1 - x + 2x = 1 + x yAOEA = A 2x 1 + xEA = 0.1 ⇒ x = 0.1/(2 – 0.1) = 0.0526, yAO2 EA = 0.9 K = A yOE 2 y02 E A (A PPo E A)A2-1EA = A0.1 2 E0.9E A 1 = 0.01111 ⇒ ln K = –4.4998 Now look in Table A.11: T = 2980 K Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.33 Redo Problem 14.32 for a total pressure of 40 kPa. Look at initially 1 mol Oxygen and shift reaction with x OA2 EA ⇔ 2 O Species OA2 E O Initial 1 0 Change -x 2x Equil. 1-x 2x nAtotEA = 1 - x + 2x = 1 + x yAOEA = A 2x 1 + xEA = 0.1 ⇒ x = 0.1/(2 – 0.1) = 0.0526, yAO2 EA = 0.9 K = A yOE 2 y02 E A (A PPo E A)A2-1EA = A0.1 2 E0.9E A 0.4 = 0.004444 ⇒ ln K = –5.4161 Now look in Table A.11: T = 2856 K Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.34 Redo Problem 14.32, but start with 1 kmol oxygen and 1 kmol helium at 298 K, 100 kPa. Look at initially 1 mol Oxygen and shift reaction with x OA2 EA ⇔ 2 O Species OA2 E O He Initial 1 0 1 Change -x 2x Equil. 1-x 2x 1 nAtotEA = 1 - x + 2x + 1 = 2 + x yAOEA = A 2x 2 + xEA = 0.1 ⇒ x = 0.2/(2 – 0.1) = 0.10526, yAO2 EA = (1 – x)/(2 + x) = 0.425 K = A yOE 2 y02 E A (A PPo E A)A2-1EA = A 0.1 2 E0.425 EA 1 = 0.023529 ⇒ ln K = –3.7495 Now look in Table A.11: T = 3094 K Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.35 Calculate the equilibrium constant for the reaction:2COA2 EA ⇔ 2CO + OA2 EA at 3000 K using values from Table A.9 and compare the result to Table A.11. From Table A.9 we get: kJ/kmol kJ/kmol kJ/kmol K ∆h - CO = 93 504 Ah -E AA o f COE A = -110 527 s - CO = 273.607 E∆h - COA2 A = 152 853 Ah-E AEA o f COA2 AEA = -393 522E s - COA2 A = 334.17 E∆h - OA2 A = 98 013 Ah-E AEA o f OA2 AEA = 0 E s - OA2 A = 284.466 ∆GA0 EA = ∆H - T∆S = 2 HACOEA + HEAOA2 AE A – 2 HEACOA2 AE A- T (2s - CO +E s - OA2 A - E2s - COA2 A ) = 2 (93 504 – 110 527) + 98 013 + 0 – 2(152 853 - 393 522) -3000(2×273.607 + 284.466 - 2×334.17) = 55 285 kJ/kmol ln K = -∆GA0 EA/ AR -E AT = -55 285/ (8.31451×3000) = -2.2164 Table A.11 ln K = -2.217 OK Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.36 Find the equilibrium constant for: CO + 1/2OA2 EA ⇔ COA2 EA at 2200 K using Table A.11 The elementary reaction in A.11 is: 2 COA2 EA ⇔ 2CO + OA2 E The wanted reaction is therefore (−0.5) times that so K = K−1/2A.11 = 1 / A exp(-10.232)E A = 1 / A 0.000036EA = 166.67 or ln K = −0.5 ln KA.11 = −0.5 (−10.232) = 5.116 K = exp(5.116) = 166.67 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.37 Pure oxygen is heated from 25°C to 3200 K in an steady flow process at a constant pressure of 200 kPa. Find the exit composition and the heat transfer. The only reaction will be the dissociation of the oxygen OA2 EA ⇔ 2O ; From A.11: K(3200) = exp(-3.069) = 0.046467 Look at initially 1 mol Oxygen and shift reaction with x nAO2 EA = 1 - x; nAOEA = 2x; nAtotEA = 1 + x; yAi EA = nAi EA/nAtotE K = A yOE 2 y02 E A (A PPo E A)A2-1EA = A 4x 2 E(1 + x)2 E A A 1 + x 1 - xE A 2 = A 8x2 E1 - x2E xA2 EA = A K/8 1 + K/8EA ⇒ x = 0.07599; yA02 EA = A 1 – x 1 + xEA = 0.859; yA0 EA = 1– yA02 EA = 0.141 Aq-E A = nA02ex EAAh-E AA02ex EA + nA0exEAAh -E AAOex EA - Ah -E AA02in EA = (1 + x)(yA02 EAAh-E AA02 EA + yA0 EAAh -E AAOEA) - 0 Ah-E AA02 EA = 106 022 kJ/kmol; Ah-E AAOEA = 249 170 + 60 767 = 309 937 kJ/kmol ⇒ Aq-E A = 145 015 kJ/kmol OA2 E q = Aq-E A/32 = 4532 kJ/kg ( = 3316.5 if no reaction) Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distributionon a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.38 Nitrogen gas, N2, is heated to 4000 K, 10 kPa. What fraction of the N2 is dissociated to N at this state? NA2 EA <=> 2 N @ T = 4000 K, lnK = -12.671 Initial 1 0 K = 3.14x10-6 Change -x 2x Equil. 1-x 2x ntot = 1 - x + 2x = 1 + x yAN2 EA = A 1 - x 1 + xE A , yAN EA = A 2x 1 + xEA K = y2N yN2 A P Po 2-1 AEE; => 3.14x10-6 = A 4x2 E1 - x2 E A A 10 100 E A => x = 0.0028 yN2 = A 1 - x 1 + xEA = 0.9944, yN = A 2x 1 + xEA = 0.0056 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.40 One kilomole Ar and one kilomole O2 are heated up at a constant pressure of 100 kPa to 3200 K, where it comes to equilibrium. Find the final mole fractions for Ar, OA2 EA, and O. The only equilibrium reaction listed in the book is dissociation of OA2 EA. So assuming that, we see in Table A.11: ln(K) = -3.072 Ar + OA2 EA ⇒ Ar + (1 - x) OA2 EA + 2x O The atom balance already shown in above equation can also be done as Species Ar OA2 EA O Start 1 1 0 Change 0 -x 2x Total 1 1-x 2x The total number of moles is n AtotEA = 1 + 1-x + 2x = 2 + x so yAArE A = 1/(2 + x); yAO2 EA = 1 - x/(2 + x); yAOEA = 2x/(2 + x) and the definition of the equilibrium constant (P AtotEA = P Ao EA) becomes K = eA-3.072EA = 0.04633 = A yOE 2 y02 E A = A 4x2 E(2 + x)(1 - x)E The equation to solve becomes from the last expression (K + 4)x A2 EA + Kx - 2K = 0 If that is solved we get x = -0.0057 ± 0.1514 = 0.1457; x must be positive yAOEA = 0.1358; yA02EA = 0.3981; yAArE A = 0.4661 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.41 Air (assumed to be 79% nitrogen and 21% oxygen) is heated in a steady state process at a constant pressure of 100 kPa, and some NO is formed. At what temperature will the mole fraction of NO be 0.001? 0.79 NA2 EA + 0.21 OA2 EA heated at 100 kPa, forms NO NA2 EA + OA2 EA ⇔ 2 NO nAN2 EA = 0.79 - x -x -x +2x nAO2 EA = 0.21 - x nANOEA = 0 + 2x ntot = 1.0 At exit, yANOEA = 0.001 = A 2x 1.0EA ⇒ x = 0.0005 ⇒ nAN2 EA = 0.7895, nAO2 EA = 0.2095 K = A y2NO EyN2yO2 E A (A P P0 E A) A0 EA = A 10 -6 E0.7895×0.2095EA = 6.046×10A -6E A or ln K = -12.016 From Table A.11, T = 1444 K Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.42 Pure oxygen is heated from 25°C, 100 kPa to 3200 K in a constant volume container. Find the final pressure, composition, and the heat transfer. As oxygen is heated it dissociates OA2 EA ⇔ 2O ln KAeq EA = -3.069 from table A.11 C. V. Heater: UA2 EA - UA1 EA = A1 EAQA2 EA = HA2 EA - HA1 EA - P A2 EAv + P A1 EAv Per mole OA2 EA: A1 EAAq -E AA2 EA = Ah -E AA2 EA - Ah -E AA1 EA + AR -E A[TA1 EA - (n A2 EA/nA1 EA)TA2 EA] Shift x in reaction 1 to have final composition: (1 - x)OA2 EA + 2xO n A1 EA = 1 nA2 EA = 1 - x + 2x = 1 + x yAO2 E A = (1 - x)/(1 + x) ; yAO EA = 2x/(1 + x) Ideal gas and VA2 EA = VA1 EA ⇒ P A2 EA = P A1 EAnA2 EATA2 EA/n A1 EATA1 EA ⇒ P A2 EA/PAo EA = (1 + x)TA2 EA/TA1 E Substitute the molefractions and the pressure into the equilibrium equation KAeq EA = eA -3.069E A = A yOE 2 y02 E A (A P2 EPoE A) = (A 2x1 + xEA)A 2 E A (A 1 + x 1 - xE A) (A 1 + x 1E A) (A T2 ET1E A) ⇒ A 4x2 E1 - xEA = A T1 ET2E A eA-3.069EA = 0.00433 ⇒ x = 0.0324 The final pressure is then P A2 EA = P Ao EA(1 + x)A T2 ET1E A = 100 (1 + 0.0324) × A 3200 298.2EA = 1108 kPa (nAO2 E A) = 0.9676, (nAO EA) = 0.0648, n A2 EA = 1.0324 A1 EAAq -E AA2 EA = 0.9676 × 106022 + 0.0648 (249170 + 60767) - 0 + 8.3145 (298.15 - 1.0324 × 3200) = 97681 kJ/kmolO A2 E yAO2 E A = A 0.9676 1.0324 E A= 0.937; yAO EA = A 0.0648 1.0324E A = 0.0628 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.43 Find the equilibrium constant for the reaction 2NO + OA2 EA ⇔ 2NOA2 EA from the elementary reactions in Table A.11 to answer which of the nitrogen oxides, NO or NOA2 EA, is the more stable at ambient conditions? What about at 2000 K? 2 NO + OA2 EA ⇔ 2 NOA2 EA (1) But NA2 EA + OA2 EA ⇔ 2 NO (2) NA2 EA + 2 OA2 EA ⇔ 2 NOA2 EA (3) Reaction 1 = Reaction 3 - Reaction 2 ⇒ ∆GA01 E A = ∆GA 0 3 E A - ∆GA 0 2 EA => ln KA1 EA = ln KA3 EA - ln KA2 E At 25 Ao EAC, from Table A.11: ln KA1 EA = -41.355 - (-69.868) = +28.513 or KA1 EA = 2.416×10A 12E an extremely large number, which means reaction 1 tends to go very strongly from left to right. At 2000 K: ln KA1 EA = -19.136 - (-7.825) = - 11.311 or KA1 EA = 1.224 × 10A -5E meaning that reaction 1 tends to go quite strongly from right to left. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.44 Assume the equilibrium mole fractions of oxygen and nitrogen are close to those in air, find the equilibrium mole fraction for NO at 3000 K, 500 kPa disregarding dissociations. Assume the simple reaction to make NO as: NA2 EA + OA2 EA ⇔ 2 NO Ar nAN2 EA = 0.78 - x 0.78 0.21 0 0.01 nAO2 EA = 0.21 - x -x -x +2x nANOEA = 2x, nAarE A = 0.01 0.78–x 0.21–x 2x 0.01 ntot = 1.0From A.11 at 3000 K, ln K = -4.205, K = 0.014921 K = A 4x2 E(0.78 – x)(0.21 – x)EA ( A P P0 E A) A0 EA A x2 E(0.78 – x)(0.21 – x)E A = A 0.014921 4E A = 0.00373 and 0 < x < 0.21 Solve for x: x = 0.0230 yANOEA = A 2x 1.0EA = 0.046 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.45 The combustion products from burning pentane, C A5 EAHA12EA, with pure oxygen in a stoichiometric ratio exists at 2400 K, 100 kPa. Consider the dissociation of only COA2 EA and find the equilibrium mole fraction of CO. C A5 EAHA12EA + 8 OA2 EA → 5 COA2 EA + 6 HA2 EAO At 2400 K, 2 COA2 EA ⇔ 2 CO + 1 OA2 E ln K = -7.715 Initial 5 0 0 K = 4.461 × 10A-4E Change -2z +2z +z Equil. 5-2z 2z z Assuming P = P Ao EA = 0.1 MPa, and ntot = 5 + z + 6 = 11 + z K = A yCOE 2 yO2 yCO2 2 E A (A P P0 E A) = A 2z 5 - 2z 2 E A A z 11 + z E A (1) = 4.461 × 10 A -4E A ; Trial & Error (compute LHS for various values of z): z = 0.291 nACO2 E A = 4.418; nACOEA = 0.582; nAO2 E A = 0.291 => yACOEA = 0.0515 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.46 A mixture flows with 2 kmol/s COA2 EA, 1 kmol/s argon and 1 kmol/s CO at 298 K and it is heated to 3000 K at constant 100 kPa. Assume the dissociation of carbon dioxide is the only equilibrium process to be considered. Find the exit equilibrium composition and the heat transfer rate. Reaction 2 COA2 E ⇔ 2 CO + OA2 E Ar initial 2 1 0 1 change -2x +2x +x equil. 2 - 2x 1 + 2x x 1 From Table A.11: K = exp( -2.217) = 0.108935 = A y2CO yO2 Ey2CO2 E A ( A PPo EA) A 3-2E A = A (1 + 2x)2 E(4 + x)2 E A A x 4 + xEA A (4 + x)2 E(2 - 2x)2 E A (1)A1 EA = Ax4EA A (1 + 2x)2 E4 + xE A A 1 (1 - x)2E then 0.43574 (4 + x) (1 – x)A2 EA = x (1 + 2x)A2 E trial and error solution gives x = 0.32136 The outlet has: 1.35728 COA2 EA + 1.64272 CO + 1 Ar + 0.32136 OA2 E Energy equation gives from Table A.9 and A.5 (for argon C Ap EAΔT) AQ .E A = ∑ n. ex h-ex - ∑ n. in h-in = 1.35728 (152853 – 393522) + 1.64272 (93504 – 110527) + 1 (39.948 ×0.52 × (3000 – 298)) + 0.32136 (98013) – 2 (-393522) – 1(-110527) – 1 (0) = 630 578 kW Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.47 A mixture of 1 kmol carbon dioxide, 2 kmol carbon monoxide, and 2 kmol oxygen, at 25°C, 150 kPa, is heated in a constant pressure steady state process to 3000 K. Assuming that only these same substances are present in the exiting chemical equilibrium mixture, determine the composition of that mixture. initial mix: 1 COA2 EA, 2 CO, 2 OA2 E Constant pressure reactor Q Equil. mix: COA2 EA, CO, OA2 EA at T = 3000 K, P = 150 kPa Reaction 2 COA2 E ⇔ 2 CO + OA2 E initial 1 2 2 change -2x +2x +x equil. (1 - 2x) (2 + 2x) (2 + x) nAtotEA = 1 – 2x + 2 + 2x + 2 + x = 5 + x so y = n/ n AtotE From A.11 at 3000 K: K = exp(−2.217) = 0.108935 For each n > 0 ⇒ −1 < x < +A12 E K = A y2COyO2 Ey2CO2 E A (A P P0 E A) A1 EA = 4 ( A 1 + x1 - 2xEA) A 2 E A ( A2 + x5 + xEA) (A 150 100EA) = 0.108935 or ( A 1 + x1 - 2xE A) A 2 E A ( A2 + x5 + x EA) = 0.018 156, Trial & error: x = −0.521 A nCO2 = 2.042 EnCO = 0.958 nO2 = 1.479 ntot = 4.479 E A A yCO2 = 0.4559 EyCO = 0.2139 yO2 = 0.3302 E Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.48 Acetylene gas Acetylene gas, C A2 EAHA2 EA, is burned with stoichiometric air in a torch. The reactants are supplied at the reference conditions P A0 EA, TA0 EA. The products come out from the flame at 2800 K after a small heat loss by radiation. Consider the dissociation of COA2 EA into CO and OA2 EA and no others. Find the equilibrium composition of the products. Are there any other reactions that should be considered? Combustion: C A2 EAHA2 EA + 2.5 (OA2 EA + 3.76NA2 EA) → 2 COA2 EA + 1 HA2 EAO + 9.4 NA2 E At 2800 K, 2 COA2 EA ⇔ 2 CO + 1 OA2 EA HA2 EAO NA2 E ln K = -3.781 Initial 2 0 0 1 9.4 K = 0.0228 Change -2z +2z +z 0 0 Equil. 2-2z 2z z 1 9.4 Assuming P = P Ao EA = 0.1 MPa, and ntot = 2 + z + 1 + 9.4 = 12.4 + z K = A yCOE 2 yO2 yCO2 2 E A (A P P0 E A) = A 2z 2 - 2z 2 E A A z 12.4 + z E A (1) = 0.0228; Solve: zA3 EA = 0.0228 (1 – z)A2 EA(12.4 + z) => z = 0.4472 yACOEA = A 2z 12.4 + z E A = 0.0696; yACO2 EA = A 2 - 2z 12.4 + z EA = 0.086; yAO2 EA = A z 12.4 + z E A = 0.0348 yAH2OEA = A 1 12.4 + z EA = 0.0778; yAN2 EA = A 9.4 12.4 + z EA = 0.7317 Looking in A.11 there will be no dissociation of nitrogen and only a small dissociation of water and oxygen which could be included. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.49 Consider combustion of methane with pure oxygen forming carbon dioxide and water as the products. Find the equilibrium constant for the reaction at 1000 K. Use an average heat capacity of Cp = 52 kJ/kmol K for the fuel and Table A.9 for the other components. For the reaction equation, CHA4 EA + 2 OA2 EA ⇔ COA2 EA + 2 HA2 EAO At 1000 K from Table A.9 and A.10 for the fuel at 298 K ∆HA01000 KE A = 1(−393 522 + 33 397) + 2(−241 826 + 26 000) − 1[−74 873 + 52(1000 – 298.2)] − 2(0 + 22 703) = − 798 804 kJ/kmol ∆S A01000 KEA = 1×269.299 + 2×232.739 – 1(186.251+ ln A 1000 298.2EA ) - 2×243.579 = 487.158 kJ/kmol K ∆GA01000 KE A = ∆HA 0 1000 KEA - T ∆S A 0 1000 KE = − 798 804 – 1000 × 487.158 = − 1 285 962 kJ/kmol ln K = − A ∆G0 ER- TE A = A + 1 285 962 8.3145×1000EA = + 154.665 , K = 1.4796 E 67 This means the reaction is shifted totally to the right. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.50 Water from the combustion of hydrogen and pure oxygen is at 3800 K and 50 kPa. Assume we only have HA2 EAO, OA2 EA and HA2 EA as gases find the equilibrium composition. With only the given components we have the reaction 2 HA2 EAO ⇔ 2HA2 EA + OA2 E which at 3800 K has an equilibrium constant from A.11 as ln K = −1.906 Assume we start with 2 kmol water and let it dissociate x to the left then Species HA2 EAO HA2 EA OA2 EA Initial 2 0 0 Change -2x 2x x Final 2 − 2x 2x x Tot: 2 + x Then we have K = exp(−1.906) = A yH2 E 2 yO2 yH2O 2 E A A P P0 2+1-2E A = A 2x 2 + x 2 x2 + x 2 - 2x 2 + x 2 50 E100E which reduces to 0.148674 = A 1 (1- x)2 4x3 E2 + x 1 4 1 2EA or x A 3 E A = 0.297348 (1 – x)A2 EA (2 + x) Trial and error to solve for x = 0.54 then the concentrations are yAH2OEA = A 2 - 2x 2 + xE A = 0.362; yAO2 EA = A x 2 + xEA = 0.213; yAH2 EA = A 2x 2 + xEA = 0.425 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.51 Repeat problem 14.47 for an initial mixture that also includes 2 kmol of nitrogen, which does not dissociate during the process. This problem has a dilution of the reactant with nitrogen. initial mix: 1 COA2 EA, 2 CO, 2 OA2 EA, 2 NA2 E Constant pressure reactor Q Equilibrium mix: COA2 EA, CO, OA2 EA and NA2 EA at T = 3000 K, P = 150 kPa Reaction 2 COA2 E ⇔ 2 CO + OA2 E initial 1 2 2 change -2x +2x +x equil. (1-2x) (2+2x) (2+x) From A.11 at 3000 K: K = exp(−2.217) = 0.108935 For each n > 0 ⇒ −1 < x < +A12 E Equilibrium: nACO2 EA = (1 – 2x), nACOEA = (2 + 2x), n AO2 EA = (2 + x), n AN2 EA = 2 so then n AtotEA = 7 + x K = A y2COyO2 Ey2CO2 E A (A P P0 E A) A1 EA = 4 ( A 1 + x1 - 2xEA) A 2 E A ( A2 + x7 + xEA) (A 150 100EA) = 0.108935 or ( A 1 + x1 - 2xEA) A 2 E A ( A2 + x7 + xEA) = 0.018167 Trial & error: x = −0.464 A nCO2 = 1.928 EnCO = 1.072 nO2 = 1.536 nN2 = 2.0 nTOT = 6.536 E A A yCO2 = 0.295 EyCO = 0.164 yO2 = 0.235 yN2 = 0.306 E Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.52 Catalytic gas generators are frequently used to decompose a liquid, providing a desired gas mixture (spacecraft control systems, fuel cell gas supply, and so forth). Consider feeding pure liquid hydrazine, NA2 EAHA4 EA, to a gas generator, from which exits a gas mixture of NA2 EA, HA2 EA, and NHA3 EA in chemical equilibrium at 100°C, 350 kPa. Calculate the mole fractions of the species in the equilibrium mixture. Initially, 2 NA2 EAHA4 EA → 1 NA2 EA + 1 HA2 EA + 2 NHA3 E Reaction: NA2 E + 3 HA2 E ⇔ 2 NHA3 E initial 1 1 2 change -x -3x +2x equil. (1-x) (1-3x) (2+2x) nATOTALE A = (4-2x) K = A y2NH3 EyN2y 3 H2 E A ( A P P0 E A) A-2EA = A(2 + 2x) 2(4 - 2x)2 E(1 - x)(1 - 3x)3E A ( A350100EA) A -2E At 100 Ao EAC = 373.2 K, for NHA3 EA use A.5 AC -E AAP0EA = 17.03×2.130 = 36.276 Ah-E AA0NH3 E A = −45 720 + 36.276(373.2 − 298.2) = −42 999 kJ/kmol As-E AA0NH3 EA = 192.572 + 36.276 ln A 373.2 298.2EA = 200.71 kJ/kmol K Using A.9, ∆HA0100 CE A = 2(−42 999) − 1(0+2188) − 3(0+2179) = −94 723 kJ ∆S A0100 CEA = 2(200.711) − 1(198.155) − 3(137.196) = −208.321 kJ/K ∆GA0100 CE A = ∆HA 0 E A − T∆S A0 EA = −94 723 − 373.2(−208.321) = −16 978 kJ ln K = − A ∆G0 ER−TE A = A +16 978 8.3145×373.2EA = 5.4716 => K = 237.84 Therefore, [A(1 + x)(2 - x) E(1 - 3x)E A]A 2 E A A 1 (1 - x)(1 - 3x)EA = A 237.84×3.52 E16E A = 182.096 By trial and error, x = 0.226 A nN2 = 0.774 EnH2 = 0.322 nNH3 = 2.452 nTOT = 3.518 E A A yN2 = 0.2181 EyH2 = 0.0908 yNH3 = 0.6911 E Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.53 Complete combustion of hydrogen and pure oxygen in a stoichiometric ratio at P Ao E A, TAo EA to form water would result in a computed adiabatic flame temperature of 4990 K for a steady state setup. How should the adiabatic flame temperature be found if the equilibrium reaction 2HA2 EA + OA2 EA ⇔ 2 HA2 EAO is considered? Disregard all other possible reactions (dissociations) and show the final equation(s) to be solved. 2HA2 EA + OA2 EA ⇔ 2HA2 EAO Species HA2 EA OA2 EA HA2 EAO Initial 2 1 0 Shift −2x −x 2x Final 2 − 2x 1 −x 2x Keq = A yH2O E 2 yH2 2 yO2 E A (A P P0 E A)A-1EA, nAtotEA = 2 − 2x + 1 − x + 2x = 3 − x Energy Eq.: HAP EA = HAREA = HAPE o E A + ∆HAP EA = HARE o E A = 0 HAPEA = (1 − x)(2∆Ah -E AAH2 EA + ∆Ah-E AAO2 EA) + 2x(Ah-E AAfH2OE o E A + ∆Ah-E AAH2OEA) = 0 (1) Equilibrium constant: KAeq EA = A 4x2 E(3-x)2 E A A (3 - x)2 E(2 - 2x)2 E A A 3 - x 1 - xEA = A x2(3 - x) E(1 - x)3 E A = KAT EA (2) A.10: Ah-E AAfH2OE o E A = −241 826 kJ/kmol; A.11: ln (KAT EA ) A.9: ∆Ah-E AAH2 EA(T), ∆Ah-E AAO2 EA(T), ∆Ah-E AAH2O EA(T), Trial and error (solve for x, T) using Eqs. (1) and (2). Guess T = 3600 K: K = exp(1.996) = 7.35956, x = 0.53986 HAPEA = (1 − 0.53986)(2 × 111 367 + 122 245) + 2 × 0.53986 × (−241 826 + 160 484) = 70 912 high Guess T = 3400 K: K = exp(3.128) = 22.8283, x = 0.648723 HAPEA = (1 − 0.648723)(2 × 103 736 + 114 101) + 2 × 0.648723 × (−241 826 + 149 073) = −7381 low Now do a linear interpolationto get HAPEA = 0: T = 3400 + 200 × 7381/(70 912 + 7381) = 3419 K, K = 20.50 x = 0.63905, yAO2 E A = 0.153; yAH2 E A = 0.306; yAH2OE A = 0.541 Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.54 Consider the water gas reaction in Example 14.4. Find the equilibrium constant at 500, 1000, 1200 and 1400 K. What can you infer from the result? As in Example 14.4, III HA2 EA + COA2 EA ⇔ HA2 EAO + CO I 2 COA2 EA ⇔ 2 CO + OA2 E II 2 HA2 EAO ⇔ 2 HA2 EA + OA2 EA Then, ln KAIIIEA = 0.5 (ln KAI EA − ln KAII EA ) At 500 K, ln KAIIIEA = 0.5 (−115.234 – (−105.385)) = − 4.9245 , K = 0.007 266 At 1000 K, ln KAIIIEA = 0.5 (−47.052 – (− 46.321)) = − 0.3655 , K = 0.693 85 At 1200 K, ln KAIIIEA = 0.5 (−35.736 – (−36.363)) = + 0.3135 , K = 1.3682 At 1400 K, ln KAIIIEA = 0.5 (−27.679 – (−29.222)) = + 0.7715 , K = 2.163 It is seen that at lower temperature, reaction III tends to go strongly from right to left, but as the temperature increases, the reaction tends to go more strongly from left to right. If the goal of the reaction is to produce more hydrogen, then it is desirable to operate at lower temperature. Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.55 A piston/cylinder contains 0.1 kmol hydrogen and 0.1 kmol Ar gas at 25°C, 200 kPa. It is heated up in a constant pressure process so the mole fraction of atomic hydrogen is 10%. Find the final temperature and the heat transfer needed. When gas is heated up HA2 EA splits partly into H as HA2 EA ⇔ 2H and the gas is diluted with Ar Component HA2 EA Ar H Initial 0.1 0.1 0 Shift -x 0 2x Final 0.1-x 0.1 2x Total = 0.2 + x yAHEA = 0.1 = 2x /(0.2 + x) ⇒ 2x = 0.02 + 0.1x ⇒ x = 0.010526 ⇒ nAtotEA = 0.21053 yAH2 EA = 0.425 = [(0.1 - x)/(0.2 + x)]; yAArE A = 1 – rest = 0.475 Do the equilibrium constant: K(T) = A y2H EyH2E A ( A P P0 E A) A2-1EA = ( A 0.010.425EA) × (A 200 100EA) = 0.047059 ln (K) = −3.056 so from Table A.11 interpolate to get T = 3110 K To do the energy eq., we look up the enthalpies in Table A.9 at 3110 K h AH2 EA = 92 829.1; hAHEA = hAfE A + ∆h = 217 999 + 58 447.4 = 276 445.4 hAArE A = 0 + C AP EA(3110 – 298.15) = 20.7863 × (3110-298.13) = 58 447.9 (same as ∆h for H) Now get the total number of moles to get nAHEA = 0.021053; nAH2 EA = nAtotEA × A 1-x 2+xE A = 0.08947; n AArE A = 0.1 Since pressure is constant W = P∆V and Q becomes differences in h Q = n∆h = 0.08947 × 92 829.1 – 0 + 0.021053 × 276 446.4 – 0 + 0.1 × 58 447.9 = 19 970 kJ Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.56 The van't Hoff equation d ln K = A ∆Ho R−T2E A dTAPoE relates the chemical equilibrium constant K to the enthalpy of reaction ∆Ho. From the value of K in Table A.11 for the dissociation of hydrogen at 2000 K and the value of ∆Ho calculated from Table A.9 at 2000 K use van’t Hoff equation to predict the constant at 2400 K. HA2 EA ⇔ 2H ∆H° = 2 × (35 375 + 217 999) – 52 942 = 453 806 kJ/kmol ln KA2000EA = −12.841; Assume ∆H° is constant and integrate the Van’t Hoff equation lnKA2400EA − lnKA2000EA = A ⌡ ⌠ 2400 2000 ∆Ho R−T2 dTE A = − EA ∆H° AR− AE A (EA 1 TA2400AE A − EA 1 TA2000AE A) lnKA2400EA = lnKA2000EA + ∆H° (EA 1 TA2400AE A − EA 1 TA2000AE A) / AR− E = −12.841 + 453 806 (A 6-5 12000 EA) / 8.31451 = −12.841 + 4.548 = −8.293 Table A.11 lists –8.280 (∆H° not exactly constant) Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.57 A gas mixture of 1 kmol carbon monoxide, 1 kmol nitrogen, and 1 kmol oxygen at 25°C, 150 kPa, is heated in a constant pressure process. The exit mixture can be assumed to be in chemical equilibrium with COA2 EA, CO, OA2 EA, and NA2 EA present. The mole fraction of COA2 EA at this point is 0.176. Calculate the heat transfer for the process. initial mix: 1 CO, 1 OA2 EA, 1 NA2 E Constant pressure reactor Q Equil. mix: COA2 EA, CO, OA2 EA, NA2 E yACO2 EA = 0.176 P = 150 kPa reaction 2 COA2 E ⇔ 2 CO + OA2 E also, NA2 E initial 0 1 1 1 change +2x -2x -x 0 equil. 2x (1-2x) (1-x) 1 yACO2 EA = 0.176 = A 2x 3-xEA ⇒ x = 0.242 65 A nCO2 = 0.4853 EnCO = 0.5147 nO2 = 0.7574 nN2 = 1 E A A yCO2 = 0.176 EyCO = 0.1867 yO2 = 0.2747 E K = A y2COyO2 Ey2CO2 E A ( A P P0 E A) A1 EA = A0.1867 2×0.2747 E0.1762 E A ( A150100EA) = 0.4635 From A.11, TAPRODEA = 3213 K From A.10, HAREA = -110 527 kJ HAP EA = 0.4853(-393 522 + 166 134) + 0.5147(-110 527 + 101 447) + 0.7574(0 + 106 545) + 1(0 + 100 617) = +66 284 kJ QACVEA = HAP EA - HAREA = 66 284 - (-110 527) = +176 811 kJ Borgnakke and Sonntag Excerpts from this work may be reproduced by instructors for distribution on a not-for-profit basis for testing or instructional purposes only to students enrolled in courses for which the textbook has been adopted. Any other reproduction or translation of this work beyond that permitted by Sections 107 or 108 of the b1976 United States Copyright Act without the permission of the copyright owner is unlawful. 14.58 A tank contains 0.1 kmol hydrogen and 0.1 kmol of argon gas at 25 Ao EAC, 200 kPa and the tank keeps constant volume. To what T should it be heated to have a mole fraction of atomic hydrogen, H, of 10%? For the reaction HA2 EA ⇔ 2H , K = A yHE 2 yH2 E A (A P Po E A)A2-1E Assume the dissociation shifts right with an amount x then we get reaction HA2 E ⇔ 2 H also, Ar initial 0.1 0 0.1 change -x 2x 0 equil. 0.1 - x 2x 0.1 Tot: 0.2 + x yAHEA = A 2x 0.2 + xEA = 0.10 ⇒ x = 0.010526 We need to find T so K will take on the proper value, since K depends on P we need to evaluate P first. P A1 EAV = nA1 EAAR − E ATA1 EA; P A2 EAV = nA2 EAAR − E ATA2 EA
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