Chemistry · Ch 6 — Gaseous State
Pressure-Volume isotherms of Carbon dioxide
Pressure-Volume isotherms of Carbon dioxide
Thomas Andrews produced the first complete experimental picture of how a real substance's pressure, volume and temperature relate to each other across both its gaseous and liquid states, by plotting a family of pressure-volume isotherms for carbon dioxide (Figure 6.12).
At a low fixed temperature, say , the isotherm starts as a smoothly falling curve as pressure rises and volume falls -- CO is purely gaseous along this stretch. At some point, liquid CO begins to separate out, and the isotherm flattens into a horizontal plateau: along this flat stretch, liquid and gas coexist side by side, and pressure stays constant even as volume keeps shrinking (more and more of the gas is simply converting to liquid at fixed pressure). Once the conversion is complete and only liquid remains, the isotherm turns sharply steep -- liquids are far less compressible than gases, so squeezing the now-fully-liquid CO produces only a very small further decrease in volume even for a large increase in pressure.
Higher-temperature isotherms show exactly the same three-stage shape, but the flat coexistence plateau grows progressively shorter. At , the plateau has shrunk all the way down to a single point -- CO passes directly from gas to liquid with no visible two-phase region at all. This special temperature is called the critical temperature (or liquefaction temperature) of CO, and the pressure at that point is 73 atm. Above this temperature, no amount of pressure -- however large -- can liquefy CO; it remains a gas at every pressure. This same qualitative picture, it turns out, holds for essentially every real gas, each with its own characteristic critical temperature, pressure and volume.
These are formalised as the critical constants:
- Critical temperature (): the temperature above which a gas cannot be liquefied, no matter how high the pressure.
- Critical pressure (): the minimum pressure needed to liquefy exactly 1 mole of the gas, at its critical temperature. …
What this figure shows. Pressure (atm, y-axis, roughly 40 to 100) plotted against volume (cm, x-axis, roughly 40 to 280) for five isotherms of CO at 13, 21, 31, 35.5 and 48 degrees Celsius. The lowest, 13 C isotherm falls along a curve A to A (gas only), flattens into a horizontal plateau A to B (actually drawn B to B, the liquid-gas coexistence region, at constant pressure) and then rises steeply C to C (liquid only, nearly incompressible). Successive isotherms (21 C, then 31 C) show the same shape but with a progressively shorter flat plateau. At 31 C (the book's 31.1 C critical isotherm) the plateau has shrunk to a single inflection point P, marked as the 'Critical point' -- above this temperature (35.5 C, 48 C) the isotherms are smooth falling curves with no flat region at all, meaning CO cannot be liquefied by pressure alone once above 31.1 C. A shaded dome labelled 'Condensation region' is drawn under the plateau points of all the sub-critical isotherms, bounded on the left by the liquid-b …
| Name of the Gas | Critical Temperature (T) in K | Critical Pressure (P) in atm | Critical Volume (V) cm mol |
|---|---|---|---|
| Helium (He) | 5.2 | 2.26 | 57.8 |
| Carbon dioxide (CO) | 304.2 | 72.9 | 94.0 |
| Oxygen (O) | 154.8 | 50.14 | 78.0 |
| Nitrogen (N) | 126.3 | 33.54 | 90.1 |
| Hydrogen (H) | 33.2 | 12.80 | 65 |
| Water (HO) | 647.4 | 218.3 | 55.3 |
| Ammonia (NH) | 405.5 | 111.3 | 72.5 |
| Hydrogen Chloride (HCl) | 324.7 | 81.5 | 81.0 |