Liquefaction of Gases
Liquefaction of gases is the process by which a gas is converted into its liquid state by applying pressure, reducing temperature, or a combination of both. Unlike solids and liquids, gases can be compressed significantly, but there exists a fundamental limit — a specific temperature above which no amount of pressure can liquefy a gas. Understanding this limit is critical to industrial applications such as the production of liquid nitrogen, liquid oxygen for rocketry, and refrigeration systems. The pioneering experimental work of Irish physicist Thomas Andrews in 1869 on carbon dioxide revealed that the gas–liquid transition is far more nuanced than previously believed. By carefully measuring pressure–volume relationships at various fixed temperatures, Andrews produced a family of curves called isotherms that showed a distinct boundary separating regions where liquefaction is possible from regions where it is not. His work gave chemistry two of its most important constants: the critical temperature (T_c) and the critical pressure (P_c). At or above the critical temperature, a gas cannot be liquefied regardless of applied pressure, because the kinetic energy of molecules is too great for intermolecular attractive forces to hold them in the liquid phase. Below T_c, compression causes the gas to condense, and a liquid phase appears. These concepts underpin the van der Waals equation of state and are essential for understanding real gas behaviour, departures from ideal gas laws, and the existence of a supercritical fluid — a phase with properties intermediate between gas and liquid.
- What Is an Isotherm?
- Andrews' Experimental Isotherms for CO₂
- The Critical Temperature (T_c)
- The Critical Pressure (P_c)
- The Two-Phase Envelope and the Dome
- Linde's Method — Industrial Liquefaction
What Is an Isotherm?
An isotherm is a curve on a pressure–volume (P–V) graph drawn at a constant temperature. For an ideal gas, every isotherm is a smooth hyperbola described by PV = nRT. For a real gas such as CO₂, the isotherms deviate significantly from this ideal behaviour, especially at lower temperatures and higher pressures.
Andrews' Experimental Isotherms for CO₂
Thomas Andrews sealed CO₂ in a glass tube and measured pressure as he reduced the volume at several fixed temperatures. At high temperatures (e.g. 48 °C), the isotherm resembles an ideal gas curve — smooth and continuously decreasing. At 31.1 °C (the critical isotherm), the curve develops a horizontal inflection point. Below 31.1 °C (e.g. at 21 °C or 13 °C), the isotherm shows a distinct flat, horizontal plateau — a region where volume decreases but pressure stays constant. This plateau corresponds to the coexistence of liquid and gas (the two-phase region), where the gas is condensing into liquid at constant pressure.
The Critical Temperature (T_c)
The critical temperature T_c is the temperature above which a gas cannot be liquefied by pressure alone, no matter how high that pressure is. At T_c, the density of the liquid and the gas phases become identical — the meniscus (liquid–gas boundary) disappears. For CO₂, T_c = 31.1 °C (304.2 K). For nitrogen, T_c = −147 °C (126 K), meaning nitrogen must be cooled below −147 °C before it can be liquefied. This is why early attempts to liquefy gases like O₂ and N₂ failed — scientists were working above their critical temperatures.
The Critical Pressure (P_c)
The critical pressure P_c is the minimum pressure required to liquefy a gas exactly at its critical temperature T_c. For CO₂, P_c = 73.8 atm. For water, P_c = 218 atm and T_c = 374 °C. At pressures above P_c and temperatures above T_c, the substance enters the supercritical fluid region, where it has characteristics of both liquid and gas — it can diffuse through solids like a gas but dissolve substances like a liquid. Supercritical CO₂ is used industrially to decaffeinate coffee and extract essential oils.
The Two-Phase Envelope and the Dome
On a P–V diagram, the flat horizontal segments of sub-critical isotherms have endpoints that, when connected, trace out a dome-shaped curve called the saturation envelope or coexistence curve. Inside the dome, gas and liquid coexist in equilibrium. The left boundary of the dome is the bubble-point curve (all liquid), and the right boundary is the dew-point curve (all vapour). The very top of the dome is the critical point, defined by coordinates (V_c, P_c, T_c). For CO₂: T_c = 304.2 K, P_c = 73.8 atm, V_c = 94 cm³ mol⁻¹.
Linde's Method — Industrial Liquefaction
Carl von Linde exploited Andrews' findings to liquefy air in 1895. His process uses the Joule–Thomson effect: when a real gas expands adiabatically through a small nozzle (throttling), it cools if the temperature is below the inversion temperature. The cooled gas then pre-cools incoming compressed gas in a heat exchanger, creating a feedback loop that progressively cools the gas until it liquefies. Nitrogen (bp = −196 °C) and oxygen (bp = −183 °C) are separated from liquid air by fractional distillation.
The Key Equation
- P — Pressure (Pa or atm): The measured pressure of the real gas.
- a — Van der Waals constant (attraction) (Pa·m⁶·mol⁻²): Accounts for intermolecular attractive forces; larger a means stronger attraction (e.g. CO₂: a = 0.3658 Pa·m⁶·mol⁻²).
- V_m — Molar volume (m³·mol⁻¹): Volume occupied per mole of the gas.
- b — Van der Waals constant (volume exclusion) (m³·mol⁻¹): Represents the volume excluded due to finite molecular size (e.g. CO₂: b = 4.27 × 10⁻⁵ m³·mol⁻¹).
- R — Universal gas constant (8.314 J·mol⁻¹·K⁻¹): Relates energy to temperature per mole.
- T — Absolute temperature (K): Temperature in Kelvin; must be below T_c for liquefaction to be possible.
Worked Example
Problem. The van der Waals constants for CO₂ are a = 3.658 L²·atm·mol⁻² and b = 0.04286 L·mol⁻¹. Using the relations derived from the van der Waals equation at the critical point, calculate the critical temperature (T_c) and critical pressure (P_c) of CO₂. (R = 0.08206 L·atm·mol⁻¹·K⁻¹)
Answer. Critical temperature T_c ≈ 308 K (≈ 35 °C); Critical pressure P_c ≈ 73.8 atm
Origins · 1 minThomas Andrews and how this was discovered
Andrews conducted meticulous experiments on CO₂ between 1861 and 1869, mapping pressure–volume isotherms that revealed the critical temperature and critical pressure. His 1869 Bakerian Lecture to the Royal Society, 'On the Continuity of the Gaseous and Liquid States of Matter,' established the concept of the critical point and demonstrated that gas and liquid are not fundamentally different states but continuous forms of matter. His work directly inspired van der Waals' Nobel Prize–winning equation of state. Andrews originally trained as a medical doctor and practised medicine alongside his chemistry research. He was Vice-President of Queen's College Belfast (now Queen's University Belfast) and conducted his famous CO₂ experiments in his own private laboratory funded out of his personal income.
Related Concepts
- Real Gases and the Van der Waals Equation — The van der Waals equation quantitatively explains why real gases deviate from ideal behaviour and predicts T_c and P_c from molecular constants a and b.
- Joule–Thomson Effect — The Joule–Thomson effect describes the temperature change of a real gas during free expansion and is the physical basis of industrial liquefaction processes such as Linde's method.
- Vapour Pressure and Boiling Point — Vapour pressure is the pressure exerted by a gas in equilibrium with its liquid phase; understanding it is essential to interpreting the horizontal plateaus (phase-coexistence regions) in Andrews isotherms.
- Kinetic Molecular Theory of Gases — KMT explains why temperature governs whether intermolecular forces can overcome molecular kinetic energy to hold molecules in the liquid state — the molecular basis of the critical temperature.
- Intermolecular Forces (van der Waals Forces) — The strength of dispersion, dipole–dipole, and hydrogen-bonding forces determines the value of T_c; gases with stronger intermolecular forces have higher critical temperatures and are easier to liquefy.