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Critical Points

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Encyclopedia of Geochemistry

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

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Definition

The point in phase space where the distinction between liquid and vapor disappears.

Elaboration

If you heat water in a closed volume, the temperature and pressure are initially fixed by equilibrium between a liquid and vapor. Beyond a certain temperature and pressure, however, the meniscus that separates the two phases disappears, and they become indistinguishable. If one draws a curve in P-V space that identifies the region where both a liquid and vapor coexist, the critical point lies at the maximum where the slope is zero:

$$ {\left(\frac{\partial P}{\partial V}\right)}_{T={T}_c}=0 \mathrm{and} {\left(\frac{\partial^2 P}{\partial {V}^2}\right)}_{T={T}_c}=0 $$
(1)

As this point is approached, the two phases, gas and liquid, begin to closely resemble one another on a molecular scale. The critical point for pure water is at 374.2 °C and 218.3 atm.

Near the critical point, the structure of these phases is very sensitive to small changes in temperature and pressure, and these...

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References

  • Sverjensky DA, Harrison B, Azzolini D (2014) Water in the deep earth: the dielectric constant and the solubilities of quartz and corundum to 60 kb and 1200 °C. Geochim Cosmochim Acta 129:125–145

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Correspondence to William H. Casey .

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© 2016 Springer International Publishing AG

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Casey, W.H., Rock, P.A. (2016). Critical Points. In: White, W. (eds) Encyclopedia of Geochemistry. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-39193-9_10-1

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  • DOI: https://doi.org/10.1007/978-3-319-39193-9_10-1

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