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(a) −30 °C and 2000 kPa
(b) −60 °C and 1000 kPa
(c) −60 °C and 100 kPa
(d) 20 °C and 1500 kPa
(e) 0 °C and 100 kPa
(f) 20 °C and 100 kPa
at 1500 kPa: at −45 °C, at −10 °C;
at 500 kPa: at −58 °C
If we place a sample of water in a sealed container at 25 °C, remove the air, and let the vaporization-condensation equilibrium establish itself, we are left with a mixture of liquid water and water vapor at a pressure of 0.03 atm. A distinct boundary between the more dense liquid and the less dense gas is clearly observed. As we increase the temperature, the pressure of the water vapor increases, as described by the liquid-gas curve in the phase diagram for water ( [link] ), and a two-phase equilibrium of liquid and gaseous phases remains. At a temperature of 374 °C, the vapor pressure has risen to 218 atm, and any further increase in temperature results in the disappearance of the boundary between liquid and vapor phases. All of the water in the container is now present in a single phase whose physical properties are intermediate between those of the gaseous and liquid states. This phase of matter is called a supercritical fluid , and the temperature and pressure above which this phase exists is the critical point ( [link] ). Above its critical temperature, a gas cannot be liquefied no matter how much pressure is applied. The pressure required to liquefy a gas at its critical temperature is called the critical pressure. The critical temperatures and critical pressures of some common substances are given in [link] .
Substance | Critical Temperature (K) | Critical Pressure (atm) |
---|---|---|
hydrogen | 33.2 | 12.8 |
nitrogen | 126.0 | 33.5 |
oxygen | 154.3 | 49.7 |
carbon dioxide | 304.2 | 73.0 |
ammonia | 405.5 | 111.5 |
sulfur dioxide | 430.3 | 77.7 |
water | 647.1 | 217.7 |
Observe the liquid-to-supercritical fluid transition for carbon dioxide.
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