Fugacity and fugacity coefficient of pure species and mixtures
Fugacity and fugacity coefficients of pure gases, compressed liquids (Poynting) and species in mixtures, from residual Gibbs energy and the virial equation.
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Why it matters
Phase equilibrium is the equality of chemical potentials, but chemical potential goes to minus infinity as pressure goes to zero and has no absolute value, which makes it awkward to compute. Fugacity is a "corrected pressure" that does the same job with ordinary numbers. High-pressure VLE in gas processing, flash calculations in simulators and the gas-phase side of every equilibrium-constant problem all run on fugacities and fugacity coefficients.
Key ideas
Definition for a pure species. For an ideal gas at constant T, dG = RT d ln P. For a real fluid we keep the same form and define fugacity fᵢ so that dGᵢ = RT d ln fᵢ at constant T, with the limit fᵢ/P → 1 as P → 0. Fugacity has units of pressure. The fugacity coefficient φᵢ = fᵢ/P is dimensionless; φ = 1 for an ideal gas, φ < 1 when attractive forces dominate, φ > 1 at very high pressure when repulsion dominates.
Link to residual properties. ln φᵢ = Gᵢ^R/RT, so ln φ follows from Z: ln φ = ∫(Z − 1) dP/P at constant T. Any equation of state or generalised correlation that gives Z gives φ. With the two-term virial equation, ln φ = BP/RT. With the Pitzer correlation, ln φ = (Pr/Tr)(B⁰ + ωB¹).
Fugacity of a pure liquid. Coexisting saturated phases have equal G, so f^l = f^v = φ^sat·P^sat at the saturation pressure. To go from P^sat to a higher pressure P, integrate dG = V^l dP for the nearly incompressible liquid. This gives the Poynting factor exp[V^l(P − P^sat)/RT], which is close to 1 unless the pressure difference is tens of bar or more. At low pressure f^l ≈ P^sat.
Effect of temperature and pressure. (∂ ln f/∂P)_T = V/RT, so fugacity always rises with pressure. (∂ ln f/∂T)_P = −H^R/RT².
Species in a mixture. The fugacity of species i in solution, f̂ᵢ, is defined by dμᵢ = RT d ln f̂ᵢ at constant T, with f̂ᵢ → yᵢP as P → 0. The fugacity coefficient of i in solution is φ̂ᵢ = f̂ᵢ/(yᵢP). In an ideal-gas mixture f̂ᵢ = yᵢP, the partial pressure. ln φ̂ᵢ is the partial molar property of ln φ of the mixture (with respect to G^R/RT), so the summability rule ln φ_mix = Σyᵢ ln φ̂ᵢ holds.
Virial mixtures. For a binary gas at moderate pressure, B_mix = y₁²B₁₁ + 2y₁y₂B₁₂ + y₂²B₂₂, and the species coefficients follow in closed form using δ₁₂ = 2B₁₂ − B₁₁ − B₂₂.
Criterion of phase equilibrium. Equal T, equal P and equal f̂ᵢ of each species in every phase. This is the starting point of the gamma-phi and phi-phi formulations of VLE.
Formulas
dGᵢ = R·T·d ln fᵢ (constant T)
φᵢ = fᵢ / P, lim(P→0) φᵢ = 1
ln φᵢ = Gᵢ^R/(R·T) = ∫₀^P (Zᵢ − 1) dP/P (constant T)
ln φᵢ = Bᵢᵢ·P/(R·T) (two-term virial)
ln φ = (Pr/Tr)·(B⁰ + ω·B¹) (Pitzer)
fᵢ^l = φᵢ^sat·Pᵢ^sat·exp[Vᵢ^l·(P − Pᵢ^sat)/(R·T)] (compressed liquid, Poynting)
f̂ᵢ = φ̂ᵢ·yᵢ·P
ln φ̂₁ = (P/RT)·(B₁₁ + y₂²·δ₁₂), ln φ̂₂ = (P/RT)·(B₂₂ + y₁²·δ₁₂), δ₁₂ = 2B₁₂ − B₁₁ − B₂₂
ln φ_mix = Σ yᵢ·ln φ̂ᵢ
f̂ᵢ^α = f̂ᵢ^β = … (phase equilibrium)
Symbols: fᵢ pure-species fugacity (Pa or bar); f̂ᵢ fugacity of i in solution (same units); φᵢ, φ̂ᵢ fugacity coefficients (dimensionless); P pressure; Pᵢ^sat vapour pressure; Vᵢ^l liquid molar volume (m³/mol); B virial coefficients (m³/mol); yᵢ vapour mole fraction; Tr, Pr reduced temperature and pressure; ω acentric factor; R = 8.314 J/(mol·K); T (K).
Worked examples
Example 1 (standard): fugacity from the virial equation. Given: a pure gas at 400 K and 10 bar with B = −300 cm³/mol. Find φ and f.
ln φ = B·P/(R·T)= (−300 × 10⁻⁶ m³/mol)(10 × 10⁵ Pa)/(8.314 × 400) = −300/3325.6 = −0.0902.- φ = e^(−0.0902) = 0.9137.
- f = φ·P = 0.9137 × 10 = 9.14 bar. Answer: φ = 0.914, f = 9.14 bar
Example 2 (GATE level): compressed liquid and a gas mixture. (a) Given: liquid water at 300 K compressed to 100 bar; P^sat = 0.0354 bar, V^l = 18.07 cm³/mol, φ^sat ≈ 1 (low pressure). Find f^l.
- Poynting exponent = V^l(P − P^sat)/RT = 18.07 × 10⁻⁶ × (100 − 0.0354) × 10⁵ / (8.314 × 300) = 180.6/2494.2 = 0.0724.
- Poynting factor = e^0.0724 = 1.0751.
- f^l = 1 × 0.0354 × 1.0751 = 0.0381 bar. Answer: f^l = 0.0381 bar, only 7.5% above P^sat even at 100 bar.
(b) Given: a binary gas at 300 K and 20 bar with y₁ = 0.4; B₁₁ = −50, B₂₂ = −150, B₁₂ = −80 cm³/mol. Find φ̂₁, φ̂₂ and f̂₁, f̂₂.
- δ₁₂ = 2(−80) − (−50) − (−150) = 40 cm³/mol.
- P/RT = 20 × 10⁵ / (8.314 × 300) = 801.9 mol/m³.
ln φ̂₁ = (P/RT)(B₁₁ + y₂²δ₁₂)= 801.9 × (−50 + 0.36 × 40) × 10⁻⁶ = 801.9 × (−35.6 × 10⁻⁶) = −0.02855, so φ̂₁ = 0.9719.ln φ̂₂ = (P/RT)(B₂₂ + y₁²δ₁₂)= 801.9 × (−150 + 0.16 × 40) × 10⁻⁶ = −0.11515, so φ̂₂ = 0.8912.- f̂₁ = 0.9719 × 0.4 × 20 = 7.78 bar; f̂₂ = 0.8912 × 0.6 × 20 = 10.69 bar.
- Check by summability: B_mix = 0.16(−50) + 0.48(−80) + 0.36(−150) = −100.4 cm³/mol, ln φ_mix = 801.9 × (−100.4 × 10⁻⁶) = −0.0805 = 0.4(−0.02855) + 0.6(−0.11515). Consistent. Answer: φ̂₁ = 0.972, φ̂₂ = 0.891; f̂₁ = 7.78 bar, f̂₂ = 10.69 bar
Common mistakes
- Writing f̂ᵢ = φᵢ·yᵢ·P with the pure-species φᵢ instead of the mixture value φ̂ᵢ (that shortcut is the Lewis-Randall rule, an approximation).
- Unit slips in BP/RT: B in cm³/mol must be converted to m³/mol when P is in Pa.
- Forgetting the Poynting factor at high pressure, or applying it with the vapour volume instead of the liquid volume.
- Assuming φ < 1 always; at high reduced pressure φ can exceed 1.
- Using the two-term virial result for a liquid or near the critical point.
For GATE CH
- NAT problems on φ and f from the virial equation or the Pitzer correlation, and on liquid fugacity with a Poynting correction.
- Mixture fugacity coefficients from given B₁₁, B₂₂ and B₁₂.
- Conceptual MCQs on the definition of fugacity, its limit at zero pressure, the equilibrium criterion and the meaning of φ greater or less than 1.
- Practise deriving ln φ from a simple equation of state such as Z = 1 + BP/RT or V = RT/P + b.
Quick check
- What is the limit of φ as P → 0?
- For a gas obeying V = RT/P + b, what is ln φ?
- Which correction converts the saturated-liquid fugacity to that of a compressed liquid?
- In an ideal-gas mixture, what is f̂ᵢ?
- What condition on fugacities defines phase equilibrium?
Answers: 1. 1. 2. bP/RT. 3. The Poynting factor exp[V^l(P − P^sat)/RT]. 4. The partial pressure yᵢP. 5. The fugacity of each species is equal in all phases at the same T and P.
Interview questions
All Chemical Engineering Thermodynamics interview questionsTry answering each one aloud before you open it.
1.What is fugacity in the context of chemical engineering thermodynamics?Concept
Fugacity is a thermodynamic property that is used to describe the 'escaping tendency' of a substance from a phase. It is analogous to pressure in an ideal gas but is applicable to real gases and liquids. Fugacity accounts for deviations from ideal behavior and is used to calculate the chemical potential of a species in a mixture.
2.Explain the concept of the fugacity coefficient and its significance.Concept
The fugacity coefficient (φ) is a dimensionless number that quantifies how much a real gas deviates from ideal gas behavior. It is defined as the ratio of the fugacity to the pressure of the gas. A fugacity coefficient of 1 indicates ideal behavior, while values different from 1 indicate non-ideal behavior. It is significant because it helps in calculating the fugacity of a gas when the pressure and temperature are known.
3.How is fugacity related to chemical potential?Concept
Fugacity is defined so that, at constant temperature, dμᵢ = RT d ln f̂ᵢ, mirroring the ideal-gas result dμ = RT d ln P. Integrating from a reference state gives μᵢ = Γᵢ(T) + RT ln f̂ᵢ. Because equal μᵢ in two phases at the same T means equal f̂ᵢ, fugacity replaces chemical potential in equilibrium calculations, with the advantage that it has finite, pressure-like values.
4.Why is fugacity used instead of pressure in real gas calculations?Application
Fugacity is used instead of pressure in real gas calculations because it accounts for the non-ideal interactions between gas molecules. While pressure is a measure of force per unit area, it does not account for molecular interactions that occur in real gases. Fugacity provides a corrected measure that reflects these interactions, allowing for more accurate thermodynamic calculations.
5.What happens to the fugacity coefficient as a gas approaches ideal behavior?Application
As a gas approaches ideal behavior, the fugacity coefficient approaches 1. This is because, in an ideal gas, the interactions between molecules are negligible, and the gas behaves according to the ideal gas law. Therefore, the fugacity becomes equal to the pressure, making the fugacity coefficient equal to 1.
6.How does temperature affect the fugacity of a pure substance?Application
At constant pressure, (∂ ln f/∂T)_P = −H^R/RT², where H^R is the residual enthalpy. For a gas at moderate pressure H^R is negative, so ln f, and the fugacity coefficient, increase with temperature: the gas becomes more nearly ideal and φ approaches 1. For a liquid, the fugacity rises steeply with temperature because it follows the vapour pressure.
7.Calculate the fugacity of a gas with a pressure of 5 MPa and a fugacity coefficient of 0.8.Numerical
To calculate the fugacity (f) of the gas, use the formula: f = φ × P, where φ is the fugacity coefficient and P is the pressure. Here, φ = 0.8 and P = 5 MPa. Therefore, f = 0.8 × 5 MPa = 4 MPa.
8.A gas has a fugacity of 3 MPa at a certain temperature and pressure. If the pressure is 4 MPa, what is the fugacity coefficient?Numerical
The fugacity coefficient (φ) can be calculated using the formula: φ = f / P, where f is the fugacity and P is the pressure. Here, f = 3 MPa and P = 4 MPa. Therefore, φ = 3 MPa / 4 MPa = 0.75.
9.Explain how fugacity is used in phase equilibrium calculations.Application
In phase equilibrium calculations, fugacity is used to ensure that the chemical potential of a species is the same in all phases at equilibrium. For a species to be in equilibrium between two phases, its fugacity must be equal in both phases. This allows for the determination of phase compositions and conditions under which phases coexist.
10.What role does fugacity play in the calculation of activity coefficients?Application
The activity coefficient of species i in a liquid solution is defined from fugacities: γᵢ = f̂ᵢ/(xᵢ·fᵢ), where f̂ᵢ is its fugacity in the solution and fᵢ the pure-liquid fugacity at the same T and P. The ideal-solution (Lewis-Randall) value is xᵢfᵢ, so γᵢ measures the departure from ideal-solution behaviour. At low pressure fᵢ ≈ Pᵢ^sat and f̂ᵢ ≈ yᵢP, giving γᵢ = yᵢP/(xᵢPᵢ^sat), which is how γ is obtained from VLE data.
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