Calorimetry

Calorimetry requires that a reference material that changes temperature have known definite thermal constitutive properties. The classical rule, recognized by Clausius and Kelvin, is that the pressure exerted by the calorimetric material is fully and rapidly determined solely by its temperature and volume; this rule is for changes that do not involve phase change, such as melting of ice. There are many materials that do not comply with this rule, and for them, the present formula of classical calorimetry does not provide an adequate account. Here the classical rule is assumed to hold for the calorimetric material being used, and the propositions are mathematically written:

The thermal response of the calorimetric material is fully described by its pressure ${\displaystyle p\ }$ as the value of its constitutive function ${\displaystyle p(V,T)\ }$ of just the volume ${\displaystyle V\ }$ and the temperature ${\displaystyle T\ }$. All increments are here required to be very small. This calculation refers to a domain of volume and temperature of the body in which no phase change occurs, and there is only one phase present. An important assumption here is continuity of property relations. A different analysis is needed for phase change

When a small increment of heat is gained by a calorimetric body, with small increments, ${\displaystyle \delta V\ }$ of its volume, and ${\displaystyle \delta T\ }$ of its temperature, the increment of heat, ${\displaystyle \delta Q\ }$, gained by the body of calorimetric material, is given by

${\displaystyle \delta Q\ =C_{T}^{(V)}(V,T)\,\delta V\,+\,C_{V}^{(T)}(V,T)\,\delta T}$

where

${\displaystyle C_{T}^{(V)}(V,T)\ }$ denotes the latent heat with respect to volume, of the calorimetric material at constant controlled temperature ${\displaystyle T}$. The surroundings' pressure on the material is instrumentally adjusted to impose a chosen volume change, with initial volume ${\displaystyle V\ }$. To determine this latent heat, the volume change is effectively the independently instrumentally varied quantity. This latent heat is not one of the widely used ones, but is of theoretical or conceptual interest.

${\displaystyle C_{V}^{(T)}(V,T)\ }$ denotes the heat capacity, of the calorimetric material at fixed constant volume ${\displaystyle V\ }$, while the pressure of the material is allowed to vary freely, with initial temperature ${\displaystyle T\ }$. The temperature is forced to change by exposure to a suitable heat bath. It is customary to write ${\displaystyle C_{V}^{(T)}(V,T)\ }$ simply as ${\displaystyle C_{V}(V,T)\ }$, or even more briefly as ${\displaystyle C_{V}\ }$. This latent heat is one of the two widely used ones.[3][4][5][6][7][8][9]

The latent heat with respect to volume is the heat required for unit increment in volume at constant temperature. It can be said to be 'measured along an isotherm', and the pressure the material exerts is allowed to vary freely, according to its constitutive law ${\displaystyle p=p(V,T)\ }$. For a given material, it can have a positive or negative sign or exceptionally it can be zero, and this can depend on the temperature, as it does for water about 4 C.[10][11][12][13] The concept of latent heat with respect to volume was perhaps first recognized by Joseph Black in 1762.[14] The term 'latent heat of expansion' is also used.[15] The latent heat with respect to volume can also be called the 'latent energy with respect to volume'. For all of these usages of 'latent heat', a more systematic terminology uses 'latent heat capacity'.

The heat capacity at constant volume is the heat required for unit increment in temperature at constant volume. It can be said to be 'measured along an isochor', and again, the pressure the material exerts is allowed to vary freely. It always has a positive sign. This means that for an increase in the temperature of a body without change of its volume, heat must be supplied to it. This is consistent with common experience.

Quantities like ${\displaystyle \delta Q\ }$ are sometimes called 'curve differentials', because they are measured along curves in the ${\displaystyle (V,T)\ }$ surface.

Constant-volume calorimetry is calorimetry performed at a constant volume. This involves the use of a constant-volume calorimeter. Heat is still measured by the above-stated principle of calorimetry.

This means that in a suitably constructed calorimeter, called a bomb calorimeter, the increment of volume ${\displaystyle \delta V\ }$ can be made to vanish, ${\displaystyle \delta V=0\ }$. For constant-volume calorimetry:

${\displaystyle \delta Q=C_{V}\delta T\ }$

where

${\displaystyle \delta T\ }$ denotes the increment in temperature and

${\displaystyle C_{V}\ }$ denotes the heat capacity at constant volume.

From the above rule of calculation of heat with respect to volume, there follows one with respect to pressure.[3][7][16][17]

In a process of small increments, ${\displaystyle \delta p\ }$ of its pressure, and ${\displaystyle \delta T\ }$ of its temperature, the increment of heat, ${\displaystyle \delta Q\ }$, gained by the body of calorimetric material, is given by

${\displaystyle \delta Q\ =C_{T}^{(p)}(p,T)\,\delta p\,+\,C_{p}^{(T)}(p,T)\,\delta T}$

where

${\displaystyle C_{T}^{(p)}(p,T)\ }$ denotes the latent heat with respect to pressure, of the calorimetric material at constant temperature, while the volume and pressure of the body are allowed to vary freely, at pressure ${\displaystyle p\ }$ and temperature ${\displaystyle T\ }$;

${\displaystyle C_{p}^{(T)}(p,T)\ }$ denotes the heat capacity, of the calorimetric material at constant pressure, while the temperature and volume of the body are allowed to vary freely, at pressure ${\displaystyle p\ }$ and temperature ${\displaystyle T\ }$. It is customary to write ${\displaystyle C_{p}^{(T)}(p,T)\ }$ simply as ${\displaystyle C_{p}(p,T)\ }$, or even more briefly as ${\displaystyle C_{p}\ }$.

The new quantities here are related to the previous ones:[3][7][17][18]

${\displaystyle C_{T}^{(p)}(p,T)={\frac {C_{T}^{(V)}(V,T)}{\left.{\cfrac {\partial p}{\partial V}}\right|_{(V,T)}}}}$

${\displaystyle C_{p}^{(T)}(p,T)=C_{V}^{(T)}(V,T)-C_{T}^{(V)}(V,T){\frac {\left.{\cfrac {\partial p}{\partial T}}\right|_{(V,T)}}{\left.{\cfrac {\partial p}{\partial V}}\right|_{(V,T)}}}}$

where

${\displaystyle \left.{\frac {\partial p}{\partial V}}\right|_{(V,T)}}$ denotes the partial derivative of ${\displaystyle p(V,T)\ }$ with respect to ${\displaystyle V\ }$ evaluated for ${\displaystyle (V,T)\ }$

and

${\displaystyle \left.{\frac {\partial p}{\partial T}}\right|_{(V,T)}}$ denotes the partial derivative of ${\displaystyle p(V,T)\ }$ with respect to ${\displaystyle T\ }$ evaluated for ${\displaystyle (V,T)\ }$.

The latent heats ${\displaystyle C_{T}^{(V)}(V,T)\ }$ and ${\displaystyle C_{T}^{(p)}(p,T)\ }$ are always of opposite sign.[19]

It is common to refer to the ratio of specific heats as

${\displaystyle \gamma (V,T)={\frac {C_{p}^{(T)}(p,T)}{C_{V}^{(T)}(V,T)}}}$ often just written as ${\displaystyle \gamma ={\frac {C_{p}}{C_{V}}}}$.[20][21]

An early calorimeter was that used by Laplace and Lavoisier, as shown in the figure above. It worked at constant temperature, and at atmospheric pressure. The latent heat involved was then not a latent heat with respect to volume or with respect to pressure, as in the above account for calorimetry without phase change. The latent heat involved in this calorimeter was with respect to phase change, naturally occurring at constant temperature. This kind of calorimeter worked by measurement of mass of water produced by the melting of ice, which is a phase change.

For a time-dependent process of heating of the calorimetric material, defined by a continuous joint progression ${\displaystyle P(t_{1},t_{2})\ }$ of ${\displaystyle V(t)\ }$ and ${\displaystyle T(t)\ }$, starting at time ${\displaystyle t_{1}\ }$ and ending at time ${\displaystyle t_{2}\ }$, there can be calculated an accumulated quantity of heat delivered, ${\displaystyle \Delta Q(P(t_{1},t_{2}))\,}$ . This calculation is done by mathematical integration along the progression with respect to time. This is because increments of heat are 'additive'; but this does not mean that heat is a conservative quantity. The idea that heat was a conservative quantity was invented by Lavoisier, and is called the 'caloric theory'; by the middle of the nineteenth century it was recognized as mistaken. Written with the symbol ${\displaystyle \Delta \ }$, the quantity ${\displaystyle \Delta Q(P(t_{1},t_{2}))\,}$ is not at all restricted to be an increment with very small values; this is in contrast with ${\displaystyle \delta Q\ }$.

One can write

${\displaystyle \Delta Q(P(t_{1},t_{2}))\ }$

${\displaystyle =\int _{P(t_{1},t_{2})}{\dot {Q}}(t)dt}$

${\displaystyle =\int _{P(t_{1},t_{2})}C_{T}^{(V)}(V,T)\,{\dot {V}}(t)\,dt\,+\,\int _{P(t_{1},t_{2})}C_{V}^{(T)}(V,T)\,{\dot {T}}(t)\,dt}$.

This expression uses quantities such as ${\displaystyle {\dot {Q}}(t)\ }$ which are defined in the section below headed 'Mathematical aspects of the above rules'.

The use of 'very small' quantities such as ${\displaystyle \delta Q\ }$ is related to the physical requirement for the quantity ${\displaystyle p(V,T)\ }$ to be 'rapidly determined' by ${\displaystyle V\ }$ and ${\displaystyle T\ }$; such 'rapid determination' refers to a physical process. These 'very small' quantities are used in the Leibniz approach to the infinitesimal calculus. The Newton approach uses instead 'fluxions' such as ${\displaystyle {\dot {V}}(t)=\left.{\frac {dV}{dt}}\right|_{t}}$, which makes it more obvious that ${\displaystyle p(V,T)\ }$ must be 'rapidly determined'.

In terms of fluxions, the above first rule of calculation can be written[22]

${\displaystyle {\dot {Q}}(t)\ =C_{T}^{(V)}(V,T)\,{\dot {V}}(t)\,+\,C_{V}^{(T)}(V,T)\,{\dot {T}}(t)}$

where

${\displaystyle t\ }$ denotes the time

${\displaystyle {\dot {Q}}(t)\ }$ denotes the time rate of heating of the calorimetric material at time ${\displaystyle t\ }$

${\displaystyle {\dot {V}}(t)\ }$ denotes the time rate of change of volume of the calorimetric material at time ${\displaystyle t\ }$

${\displaystyle {\dot {T}}(t)\ }$ denotes the time rate of change of temperature of the calorimetric material.

The increment ${\displaystyle \delta Q\ }$ and the fluxion ${\displaystyle {\dot {Q}}(t)\ }$ are obtained for a particular time ${\displaystyle t\ }$ that determines the values of the quantities on the righthand sides of the above rules. But this is not a reason to expect that there should exist a mathematical function ${\displaystyle Q(V,T)\ }$. For this reason, the increment ${\displaystyle \delta Q\ }$ is said to be an 'imperfect differential' or an 'inexact differential'.[23][24][25] Some books indicate this by writing ${\displaystyle q\ }$ instead of ${\displaystyle \delta Q\ }$.[26][27] Also, the notation đQ is used in some books.[23][28] Carelessness about this can lead to error.[29]

The quantity ${\displaystyle \Delta Q(P(t_{1},t_{2}))\ }$ is properly said to be a functional of the continuous joint progression ${\displaystyle P(t_{1},t_{2})\ }$ of ${\displaystyle V(t)\ }$ and ${\displaystyle T(t)\ }$, but, in the mathematical definition of a function, ${\displaystyle \Delta Q(P(t_{1},t_{2}))\ }$ is not a function of ${\displaystyle (V,T)\ }$. Although the fluxion ${\displaystyle {\dot {Q}}(t)\ }$ is defined here as a function of time ${\displaystyle t\ }$, the symbols ${\displaystyle Q\ }$ and ${\displaystyle Q(V,T)\ }$ respectively standing alone are not defined here.

The above rules refer only to suitable calorimetric materials. The terms 'rapidly' and 'very small' call for empirical physical checking of the domain of validity of the above rules.

The above rules for the calculation of heat belong to pure calorimetry. They make no reference to thermodynamics, and were mostly understood before the advent of thermodynamics. They are the basis of the 'thermo' contribution to thermodynamics. The 'dynamics' contribution is based on the idea of work, which is not used in the above rules of calculation.

For measurements at experimentally controlled volume, one can use the assumption, stated above, that the pressure of the body of calorimetric material is can be expressed as a function of its volume and temperature.

For measurement at constant experimentally controlled volume, the isochoric coefficient of pressure rise with temperature, is defined by

${\displaystyle \alpha _{V}(V,T)\ ={\frac {\left.{\cfrac {\partial p}{\partial V}}\right|_{(V,T)}}{p(V,T)}}}$.[30]

For measurements at experimentally controlled pressure, it is assumed that the volume ${\displaystyle V\ }$ of the body of calorimetric material can be expressed as a function ${\displaystyle V(T,p)\ }$ of its temperature ${\displaystyle T\ }$ and pressure ${\displaystyle p\ }$. This assumption is related to, but is not the same as, the above used assumption that the pressure of the body of calorimetric material is known as a function of its volume and temperature; anomalous behaviour of materials can affect this relation.

The quantity that is conveniently measured at constant experimentally controlled pressure, the isobaric volume expansion coefficient, is defined by

${\displaystyle \beta _{p}(T,p)\ ={\frac {\left.{\cfrac {\partial V}{\partial T}}\right|_{(T,p)}}{V(T,p)}}}$.[30][31][32][33][34][35][36]

For measurements at experimentally controlled temperature, it is again assumed that the volume ${\displaystyle V\ }$ of the body of calorimetric material can be expressed as a function ${\displaystyle V(T,p)\ }$ of its temperature ${\displaystyle T\ }$ and pressure ${\displaystyle p\ }$, with the same provisos as mentioned just above.

The quantity that is conveniently measured at constant experimentally controlled temperature, the isothermal compressibility, is defined by

${\displaystyle \kappa _{T}(T,p)\ =-{\frac {\left.{\cfrac {\partial V}{\partial p}}\right|_{(T,p)}}{V(T,p)}}}$.[31][32][33][34][35][36]

The quantity ${\displaystyle C_{T}^{(V)}(V,T)\ }$, the latent heat with respect to volume, belongs to classical calorimetry. It accounts for the occurrence of energy transfer by work in a process in which heat is also transferred; the quantity, however, was considered before the relation between heat and work transfers was clarified by the invention of thermodynamics. In the light of thermodynamics, the classical calorimetric quantity is revealed as being tightly linked to the calorimetric material's equation of state ${\displaystyle p=p(V,T)\ }$. Provided that the temperature ${\displaystyle T\,}$ is measured in the thermodynamic absolute scale, the relation is expressed in the formula

${\displaystyle C_{T}^{(V)}(V,T)=T\left.{\frac {\partial p}{\partial T}}\right|_{(V,T)}\ }$.[47]

Advanced thermodynamics provides the relation

${\displaystyle C_{p}(p,T)-C_{V}(V,T)=\left[p(V,T)\,+\,\left.{\frac {\partial U}{\partial V}}\right|_{(V,T)}\right]\,\left.{\frac {\partial V}{\partial T}}\right|_{(p,T)}}$.

From this, further mathematical and thermodynamic reasoning leads to another relation between classical calorimetric quantities. The difference of specific heats is given by

${\displaystyle C_{p}(p,T)-C_{V}(V,T)={\frac {TV\,\beta _{p}^{2}(T,p)}{\kappa _{T}(T,p)}}}$.[31][37][48]