Читать книгу Geochemistry - William M. White - Страница 49

We have now introduced all the fundamental variables of thermodynamics, T, S, U, P and V. Everything else can be developed and derived from these functions. Thermodynamicists have found it convenient to define several other state functions, the first of which is called enthalpy. Enthalpy is a composite function and is the sum of the internal energy plus the product PV:

(2.59)

As is the case for most thermodynamic functions, it is enthalpy changes rather than absolute enthalpy that are most often of interest. For a system going from state 1 to state 2, the enthalpy change is:

(2.60)

The first law states:

so:

If pressure is constant, then:

(2.61)

(we use the subscript P in ΔQ_P to remind us that pressure is constant). If the change takes place at constant pressure and P–V work is the only work done by the system, then the last two terms cancel and enthalpy is simply equal to the heat gained or lost by the system:

or in differential form:

(2.62)

H is a state function because it is defined in terms of state functions U, P, and V. Because enthalpy is a state function, dQ must also be a state function under the conditions of constant pressure and the only work done being P–V work.

More generally, the enthalpy change of a system may be expressed as:

or at constant pressure as:

(2.63)

In terms of its characteristic variables, it may also be expressed as:

(2.64)

From this it can be shown that H will be at a minimum at equilibrium when S and P are prescribed:

(2.65)

The primary value of enthalpy is measuring the energy consumed or released in changes of state of a system. For example, how much energy is given off by the reaction:

To determine the answer, we could place hydrogen and oxygen in a well-insulated piston-cylinder maintaining constant pressure. We would design it such that we could easily measure the temperature before and after reaction. Such an apparatus is known as a calorimeter. By measuring the temperature before and after the reaction and knowing the heat capacity of the reactants and our calorimeter, we could determine the enthalpy of this reaction. This enthalpy value is often also called the heat of reaction or heat of formation and is designated ΔH_r (or ΔH_ƒ). Similarly, we might wish to know how much heat is given off when NaCl is dissolved in water. Measuring temperature before and after reaction would allow us to calculate the heat of solution. The enthalpy change of a system that undergoes melting is known as the heat of fusion or heat of melting, ΔH_m (this quantity is sometimes denoted ΔH_f; we will use the subscript m to avoid confusion with heat of formation); that of a system undergoing boiling is known as the heat of vaporization, ΔH_v. As eqn. 2.65 suggests, measuring enthalpy change is also a convenient way of determining the entropy change.

At this point, it might seem that we have wandered rather far from geochemistry. However, we shall shortly see that functions such as entropy and enthalpy and measurements of such things as heats of solution and melting are essential to predicting equilibrium geochemical systems.