Thermal pressure explained

In thermodynamics, thermal pressure (also known as the thermal pressure coefficient) is a measure of the relative pressure change of a fluid or a solid as a response to a temperature change at constant volume. The concept is related to the Pressure-Temperature Law, also known as Amontons's law or Gay-Lussac's law.^[1]

In general pressure, (

) can be written as the following sum: . is the pressure required to compress the material from its volume to volume at a constant temperature . The second term expresses the change in thermal pressure . This is the pressure change at constant volume due to the temperature difference between and . Thus, it is the pressure change along an isochore of the material.

The thermal pressure

is customarily expressed in its simple form as $$\backslash gamma\_v\; =\backslash left(\backslash frac\; \backslash right)\_.$$

Thermodynamic definition

Because of the equivalences between many properties and derivatives within thermodynamics (e.g., see Maxwell Relations), there are many formulations of the thermal pressure coefficient, which are equally valid, leading to distinct yet correct interpretations of its meaning. Some formulations for the thermal pressure coefficient include:

$$\backslash left(\backslash frac\; \backslash right)\_\; =\; \backslash alpha\backslash kappa\_T\; =\; \backslash fracC\_V\; =\; \backslash frac$$

Where

is the volume thermal expansion, the isothermal bulk modulus, the Grüneisen parameter, the compressibility and the constant-volume heat capacity.^[2]

Details of the calculation:

$$\backslash left(\backslash frac\; \backslash right)\_\; =\; -\backslash left(\backslash frac\; \backslash right)\_\backslash left(\backslash frac\; \backslash right)\_\; =\; -\; (V\backslash alpha)\; \backslash left(\backslash frac\backslash right)\; =\; \backslash alpha\backslash kappa\_T$$

$$\backslash left(\backslash frac\; \backslash right)\_\; =\; \backslash frac\; =\; \backslash frac$$

The utility of the thermal pressure

The thermal pressure coefficient can be considered as a fundamental property; it is closely related to various properties such as internal pressure, sonic velocity, the entropy of melting, isothermal compressibility, isobaric expansibility, phase transition, etc. Thus, the study of the thermal pressure coefficient provides a useful basis for understanding the nature of liquid and solid. Since it is normally difficult to obtain the properties by thermodynamic and statistical mechanics methods due to complex interactions among molecules, experimental methods attract much attention.The thermal pressure coefficient is used to calculate results that are applied widely in industry, and they would further accelerate the development of thermodynamic theory.Commonly the thermal pressure coefficient may be expressed as functions of temperature and volume. There are two main types of calculation of the thermal pressure coefficient: one is the Virial theorem and its derivatives; the other is the Van der Waals type and its derivatives.^[3]

Thermal pressure at high temperature

As mentioned above,

is one of the most common formulations for the thermal pressure coefficient.Both and are affected by temperature changes, but the value of and of a solid much less sensitive to temperature change above its Debye temperature. Thus, the thermal pressure of a solid due to moderate temperature change above the Debye temperature can be approximated by assuming a constant value of and .^[4]

On the contrary, in the paper,^[5] authors demonstrated that, at ambient pressure, the pressure predicted of Au and MgO from a constant value of

deviates from the experimental data, and the higher temperature, the more deviation. In addition, the authors suggested a thermal expansion model to replace the thermal pressure model.

Thermal pressure in a crystal

The thermal pressure of a crystal defines how the unit-cell parameters change as a function of pressure and temperature. Therefore, it also controls how the cell parameters change along an isochore, namely as a function of $\backslash left(\backslash frac\; \backslash right)\_$. Usually, Mie-Grüneisen-Debye and other Quasi harmonic approximation (QHA) based state functions are being used to estimate volumes and densities of mineral phases in diverse applications such as thermodynamic, deep-Earth geophysical models and other planetary bodies. In the case of isotropic (or approximately isotropic) thermal pressure, the unit cell parameter remains constant along the isochore and the QHA is valid. But when the thermal pressure is anisotropic, the unit cell parameter changes so, the frequencies of vibrational modes also change even in constant volume and the QHA is no longer valid.

:$$\backslash varepsilon\_=\; \backslash alpha\_\; dT-\; \backslash beta\_\; dP$$

Where

is the volume thermal expansion tensor and is the compressibility tensor. The line in the P-T space which indicates that the strain is constant in a particular direction within the crystal is defined as:$$\backslash left(\backslash frac\; \backslash right)\_=\backslash frac$$

Which is an equivalent definition of the isotropic degree of thermal pressure.

See also

• Isochoric process
• Pressure
• Hydrostatic equilibrium

Notes and References

1. Web site: CHEMISTRY, CHAPTER 9, 9.2 RELATING PRESSURE, VOLUME, AMOUNT, AND TEMPERATURE: THE IDEAL GAS LAW. 2020-10-17. Press Books.
2. J.M.Haile (2002). "Lectures in Thermodynamics, Volume 1". Macatea Productions, Central, South Carolina, 53-67 177-184.
3. Gilbert Newton Lewi (1900). "A New Conception of Thermal Pressure and a Theory of Solutions". American Academy of Arts & Sciences. .
4. Angel, Ross J., Miozzi Francesca, and Alvaro Matteo (2019). "Limits to the Validity of Thermal-Pressure Equations of State". MDPI.
5. Yan, J., Yang, S. Thermal Pressure in the Thermal Equation of State for Solid and a Proposed Substitute. Int J Thermophys 43, 169 (2022). https://doi.org/10.1007/s10765-022-03089-8