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23-Chem-A1 Process Balances and Chemical Thermodynamics · December 2018

Question 5 of 6: Equilibrium Composition of Three Pentane Isomers

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

Notes on this paper

Paper format. National Exam 16-Chem-A1, December 2018 — open-book, 3 hours. Two parts: Part A (Process Balances, Q1–Q3) and Part B (Chemical Thermodynamics, Q1–Q3). Candidates answer TWO from each part; each question is of equal value. All six questions are solved in full below.

Reference texts: Felder, Rousseau & Bullard, Elementary Principles of Chemical Processes (4th ed., Wiley) — degree-of-freedom analysis, separation trains, humidity and condensation energy balances, recycle systems; Himmelblau & Riggs, Basic Principles and Calculations in Chemical Engineering (8th ed.) — psychrometrics and recycle-ratio calculations; Smith, Van Ness, Abbott & Swihart, Introduction to Chemical Engineering Thermodynamics (8th ed., McGraw-Hill) — residual properties from a real-gas EOS, reaction equilibrium from ΔG°, and generalized/EOS fugacity coefficients; supporting critical-property data from Poling, Prausnitz & O’Connell, The Properties of Gases and Liquids (5th ed.).

Part A — Process Balances

Question B2: Equilibrium Composition of Three Pentane Isomers (Part B — equal value)

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. Three simultaneous formation equilibria from graphite and $H_2$ at $T=400$ K, $P=1$ atm, with standard Gibbs energies of formation $\Delta G^\circ_{f,i}$ (kJ/mol): n 40.195, iso 34.415, neo 37.640.

Find. The equilibrium mole fractions of the three isomers in the gas phase.

Approach. The three isomers share the identical formation reaction ($5C+6H_2\to$ isomer), so the graphite and hydrogen activities are common to all three; the isomer partial pressures therefore follow a Boltzmann-type weighting $\propto\exp(-\Delta G^\circ_{f,i}/RT)$, and normalizing gives the composition.

  1. Equilibrium constant for each isomer. For $5C(s)+6H_2\leftrightarrow C_5H_{12}$, with graphite at unit activity, $$K_i=\frac{p_i}{p_{H_2}^{6}}=\exp\!\left(-\frac{\Delta G^\circ_{f,i}}{RT}\right).$$
  2. Ratio of isomers eliminates the common terms. Dividing any two equilibria, the identical $p_{H_2}^{6}$ (and graphite) cancel, so $$\frac{p_i}{p_j}=\exp\!\left(-\frac{\Delta G^\circ_{f,i}-\Delta G^\circ_{f,j}}{RT}\right)\;\Rightarrow\; y_i\propto\exp\!\left(-\frac{\Delta G^\circ_{f,i}}{RT}\right).$$
  3. Boltzmann weights at 400 K. With $RT=8.314(400)=3325.6$ J/mol, the unnormalized weights $w_i=\exp(-\Delta G^\circ_{f,i}/RT)$ are in the ratio $$w_{\text{n}}:w_{\text{iso}}:w_{\text{neo}}=\exp(-12.087):\exp(-10.349):\exp(-11.319),$$ i.e. $1.000:5.686:2.156$ after dividing through by $w_{\text{n}}$.
  4. Normalize to mole fractions. Dividing by the sum $1.000+5.686+2.156=8.842$: $$\boxed{y_{\text{n}}=0.113,\quad y_{\text{iso}}=0.643,\quad y_{\text{neo}}=0.244.}$$

Isopentane, having the lowest Gibbs energy of formation, is the most stable and dominates the mixture; neopentane is intermediate and n-pentane the least favoured. The result is independent of the total pressure because every isomer is formed by the same mole-change reaction, so the pressure factors cancel in the ratios.

IsomerEquilibrium mole fraction
Isopentane0.643
Neopentane0.244
n-Pentane0.113