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23-Chem-A1 Process Balances and Chemical Thermodynamics · May 2016

Question 6 of 6: Gas-Phase Decomposition Equilibrium in a Rigid Vessel

Nivaar worked solution (AI-drafted; not reviewed by a licensed engineer)

Notes on this paper

National Exams — May 2016 — 04-Chem-A1 Process Balances and Chemical Thermodynamics. Three-hour, open-book exam; any non-communicating calculator permitted. Format: six questions in two parts — Part A (Q1–Q3, Process Mass & Energy Balances) and Part B (Q4–Q6, Chemical Thermodynamics). Candidates answer two from Part A and two from Part B; four equally-weighted questions (25 marks each) constitute a complete paper. All six are solved below for completeness. Property data are stated explicitly in each Given block.

Reference texts: Felder, Rousseau & Bullard, Elementary Principles of Chemical Processes (4th ed., Wiley) — combustion/metallurgical stoichiometry, tie-substance balances and reactive mass balances; Himmelblau & Riggs, Basic Principles and Calculations in Chemical Engineering (8th ed., Prentice Hall) — ore/metallurgical balances and heat-of-reaction bookkeeping; Smith, Van Ness, Abbott & Swihart, Introduction to Chemical Engineering Thermodynamics (8th ed., McGraw-Hill) — reaction equilibrium, van’t Hoff analysis and VLE with activity coefficients; supporting data from Perry’s Chemical Engineers’ Handbook (9th ed.) and the NIST Chemistry WebBook.

Question 6: Gas-Phase Decomposition Equilibrium in a Rigid Vessel (Part B — 25 marks)

Question text not reproduced: the examination questions are © Engineers and Geoscientists BC. Open the official past paper (linked at the top of this page) to read the question, then follow the worked solution below.

Given. Rigid (constant-$V$) vessel, pure A charged at $T_0=300$ K, $P_0=760$ mmHg (no dissociation yet, $\alpha_0=0$). Heating drives A(g) → B(g) + C(g), which increases the total moles. Measured $P=1114$ mmHg at 400 K and 1584 mmHg at 500 K. Ideal gas, so $n_0R/V=P_0/T_0=2.533$ mmHg/K is a fixed constant of the vessel.

Find. The total pressure at 600 K.

1.61.822.22.42.6234567ln Kp vs 1/T (endothermic)600 K: Kp=4781000/T (K⁻¹)ln Kp
Figure 5 — van’t Hoff plot of the extracted $K_p$ values. $\ln K_p$ rises with $1/T$ decreasing (endothermic decomposition); linear extrapolation to 600 K gives $K_p\approx478$, from which the pressure follows.

Approach. At each temperature the measured pressure gives the dissociation fraction $\alpha$ (since one mole of A makes two moles of products), hence $K_p$; two $K_p$ values fix a van’t Hoff line, which is extrapolated to 600 K and solved back for $\alpha$ and the pressure.

  1. Dissociation fraction from each pressure. Starting from $n_0$ moles of A, at fraction $\alpha$ the total moles are $n_0(1+\alpha)$, so $P=\dfrac{P_0}{T_0}(1+\alpha)T$ and $\alpha=\dfrac{P\,T_0}{P_0\,T}-1$: $$\alpha_{400}=\frac{1114}{2.533(400)}-1=0.099,\qquad \alpha_{500}=\frac{1584}{2.533(500)}-1=0.250.$$
  2. Equilibrium constant at 400 and 500 K. For A → B + C, $K_p=\dfrac{p_Bp_C}{p_A P^\circ}$; with mole fractions $\tfrac{\alpha}{1+\alpha}$ (B, C) and $\tfrac{1-\alpha}{1+\alpha}$ (A) this reduces to $K_p=\dfrac{P\,\alpha^2}{(1-\alpha^2)}$ (here $K_p$ carries mmHg units, i.e. $P^\circ=1$ mmHg; the unit choice cancels in the van’t Hoff ratio and in the back-calculation): $$K_{p,400}=\frac{1114(0.099)^2}{1-0.099^2}=11.1,\qquad K_{p,500}=\frac{1584(0.250)^2}{1-0.250^2}=106.$$
  3. van’t Hoff line and extrapolation to 600 K. $\ln\dfrac{K_{p,500}}{K_{p,400}}=-\dfrac{\Delta H}{R}\!\left(\dfrac1{500}-\dfrac1{400}\right)$ gives $-\Delta H/R=-4515$ K ($\Delta H\approx+37.5$ kJ/mol, endothermic). Extrapolating, $$\ln K_{p,600}=\ln K_{p,500}-4515\!\left(\tfrac1{600}-\tfrac1{500}\right)\;\Rightarrow\;K_{p,600}=478.$$
  4. Pressure at 600 K. At 600 K the vessel pressure is $P=\dfrac{P_0}{T_0}(1+\alpha)(600)=1520(1+\alpha)$, and $K_p=\dfrac{P\alpha^2}{1-\alpha^2}=\dfrac{1520\,\alpha^2}{1-\alpha}$. Setting this to 478: $$\frac{1520\,\alpha^2}{1-\alpha}=478\;\Rightarrow\;\alpha=0.425,\qquad P_{600}=1520(1+0.425)=\boxed{2166\ \text{mmHg}\ (2.85\ \text{atm}).}$$

The pressure rise (760 → 2166 mmHg over 300 → 600 K) far outpaces simple thermal expansion (which alone would give 1520 mmHg) because the endothermic decomposition keeps generating extra moles as the temperature climbs — a nice illustration of Le Chatelier’s principle acting through both temperature and the mole-increasing reaction.

TemperaturePressure (mmHg)$\alpha$$K_p$
300 K (charge)7600—
400 K11140.09911.1
500 K15840.250106
600 K (estimate)2166 (2.85 atm)0.425478
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