Geochemistry. William M. White

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Geochemistry - William M. White

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      Since the total energy of the two systems is fixed, system B will have some fixed energy EB when A is in state a with energy EA, and:

equation

      where E is the total energy of the system. As we mentioned earlier, Ω is multiplicative, so the number of states available to the total system, A + B, is the product of the number of states available to A times the states available to B:

equation

      If we stipulate that A is in state a, then ΩA is 1 and the total number of states available to the system in that situation is just ΩB:

equation

      Thus, the probability of finding A in state a is equal to the probability of finding B in one of the states associated with energy EB, so that:

      (2.78)equation

      We can expand images as a Taylor series about E:

      (2.79)equation

      and since B is much larger than A, E > EA, higher-order terms may be neglected.

      Substituting β for ∂lnΩ(E)/dE (eqn. 2.48), we have:

equation

      and

      (2.80)equation

      Since the total energy of the system, E, is fixed, Ω(E) must also be fixed, so:

      Substituting 1/kT for β (eqn. 2.53), we have:

equation

      We can deduce the value of the constant C by noting that images, that is, the probabilities over all energy levels must sum to one (because the system must always be in one of these states). Therefore:

      (2.82)equation

      so that

      (2.83)equation

      Generalizing our result, the probability of the system being in state i corresponding to energy εi is:

       2.8.4.2 The partition function

      The denominator of eqn. 2.84, which is the probability normalizing factor or the sum of the energy distribution over all accessible states, is called the partition function and is denoted Q:

      The partition function is a key variable in statistical mechanics and quantum physics. It is related to macroscopic variables with which we are already familiar, namely energy and entropy. Let's examine these relationships.

      We can compute the total internal energy of a system, U, as the average energy of the atoms times the number of atoms, n. To do this we need to know how energy is distributed among atoms. Macroscopic systems have a very large number of atoms (∼1023, give or take a few in the exponent). In this case, the number of atoms having some energy εi is proportional to the probability of one atom having this energy. So to find the average, we take the sum over all possible energies of the product of energy times the possibility of an atom having that energy. Thus, the internal energy of the system is just:

Graph depicts the occupation of vibrational energy levels calculated from the Boltzmann distribution. The probability of an energy level associated with the vibrational quantum number n is shown as a function of n for a hypothetical diatomic molecule at 273 K and 673 K.

      The derivative of Q with respect to temperature (at constant volume) can be obtained from eqn. 2.85:

      (2.87)equation

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