Geochemistry. William M. White

Чтение книги онлайн.

Читать онлайн книгу Geochemistry - William M. White страница 49

Geochemistry - William M. White

Скачать книгу

      (2.88)equation

      It is also easy to show that images, so the internal energy of the system is:

      For 1 mole of substance, n is equal to the Avogadro number, NA. Since R = NAk, eqn. 2.89, when expressed on a molar basis, becomes:

      We should not be surprised to find that entropy is also related to Q. This relationship, the derivation of which is left to you (Problem 13), is:

      (2.91)equation

      Since the partition function is a sum over all possible states, it might appear that computing it would be a formidable, if not impossible, task. As we shall see, however, the partition function can very often be approximated to a high degree of accuracy by quite simple functions. The partition function and Boltzmann distribution will prove useful to us in subsequent chapters in discussing several geologically important phenomena such as diffusion and the distribution of stable isotopes between phases, as well as in understanding heat capacities, discussed below.

       2.8.4.3 Energy distribution in solids

      According to quantum theory, all modes of motion are quantized. Consider, for example, vibrations of atoms in a hydrogen molecule. Even at absolute zero temperature, the atoms will vibrate at a ground state frequency. The energy associated with this vibration will be:

      (2.92)equation

      where h is Planck's constant and ν0 is the vibrational frequency of the ground state. Higher quantum levels have higher frequencies (and hence higher energies) that are multiples of this ground state:

      where n is the quantum number (an integer ≥ 0).

      Now consider a monatomic solid, such as diamond, composed of N identical atoms arranged in a crystal lattice. For each vibration of each atom, we may write an atomic partition function, images. Since vibrational motion is the only form of energy available to atoms in a lattice, the atomic partition function may be written as:

      We can rewrite eqn. 2.94 as:

      The summation term can be expressed as a geometric series, 1 + x + x2 + x3 +..., where images. Such a series is equal to 1/(1 − x) if x < 1. Thus, eqn. 2.95 may be rewritten in a simpler form as:

      At high temperature, images, and we may approximate images in the denominator of eqn. 2.96 by images, so that at high temperature:

      (2.97)equation

      Using this relationship, and those between constant volume heat capacity and energy and between energy and the partition function, it is possible to show that:

      (2.98)equation

      Now consider the case where the temperature is very low. In this case, images and the denominator of eqn. 2.96; therefore, tends to 1, so that eqn. 2.96 reduces to:

      (2.99)equation

      The differential with respect to temperature of ln images is then simply:

      (2.100)equation

      If we insert this into eqn. 2.90 and differentiate U with respect to temperature, we find that the predicted heat capacity at T = 0 is 0! In actuality, only a perfectly crystalline solid would have 0 heat capacity near absolute zero. Real solids have a small but finite heat capacity.

      On a less mathematical level, the heat capacities of solids at low temperature are small because the spacings between the first few vibrational energy levels are large. As a result, energy transitions are large and therefore improbable. Thus, at low temperature, relatively little energy will go into vibrational motions.

      We can also see from eqn. 2.93 that the gaps between energy levels depend on the fundamental frequency, ν0. The larger the gap in vibrational frequency, the less likely will be the transition to higher energy states.

Скачать книгу