Geochemistry. William M. White

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Geochemistry - William M. White

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alt="Schematic illustration of the two copper blocks at different temperatures which are separated by an insulator. When the insulator is removed and the blocks brought in contact, the blocks come to thermal equilibrium. Entropy increases in this process."/> Schematic illustration of the six possible ways to distribute six energy units so that the left block has one unit and the right block has five units.

      Here we use Ω(e) to denote the function that describes the number of states accessible to the system for a given value of e. In this particular example, “states accessible to the system” refers to a given distribution of energy units between the two blocks. According to eqn. 2.36 there are 20 ways of distributing our six units of energy so that each block has three. There is, of course, only one way to distribute energy so that the left block has all of the energy and only one combination where the right block has all of it.

      According to the basic postulate, any of the 64 possible distributions of energy are equally likely. The key observation, however, is that there are many ways to distribute energy for some values of e and only a few for other values. Thus the chances of the system being found in a state where each block has three units is 20/64 = 0.3125, whereas the chances of the system being in the state with the original distribution (one unit to the left, five to the right) are only 6/64 = 0.0938. So it is much more likely that we will find the system in a state where energy is equally divided than in the original state.

      Of course, two macroscopic blocks of copper at any reasonable temperature will have far more than 6 quanta of energy. Let's take a just slightly more realistic example and suppose that they have a total of 20 quanta and compute the distribution. There will be 220 possible distributions, far too many to consider individually, so let's do it the easy way and use eqn. 2.36 to produce a graph of the probability distribution. Equation 2.36 gives the number of identical states of the system for a given value of e. The other thing that we need to know is that the chances of any one of these states occurring is simply (1/2)20. So to compute the probability of a particular distinguishable distribution of energy occurring, we multiply this probability by Ω. More generally, the probability, P, will be:

      (2.39)equation

      Figure 2.8b shows Ω as a function of e, the number of energy units in the left block. Comparing the two, as well as eqn. 2.38, we see that the most probable distribution of energy between the blocks corresponds to the situation where the system has the maximal number of states accessible to it (i.e., to where Ω(e) is maximum).

      According to our earlier definition of equilibrium, the state ultimately reached by this system when we removed the constraint (the insulation) is the equilibrium one. We can see here that, unlike the ball on the hill, we cannot determine whether this system is at equilibrium or not simply from its energy: the total energy of the system remained constant. In general, for a thermodynamic system, whether the system is at equilibrium depends not on its total energy but on how that energy is internally distributed.

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