Lecture 13. Thermodynamic Potentials (Ch. 5) So far, we have been using the total internal energy U and, sometimes, the enthalpy H to characterize various.

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Lecture 13. Thermodynamic Potentials (Ch. 5) So far, we have been using the total internal energy U and, sometimes, the enthalpy H to characterize various macroscopic systems. These functions are called the thermodynamic potentials: all the thermodynamic properties of a system can be found by taking partial derivatives of the TP. PotentialVariables U (S,V,N)S, V, N H (S,P,N)S, P, N F (T,V,N)V, T, N G (T,P,N)P, T, N When considering different types of processes, we will be interested in two main issues: what determines the stability of a system and how the system evolves towards an equilibrium; how much work can be extracted from a system. Today we’ll introduce the other two thermodynamic potentials: the Helmholtz free energy F and Gibbs free energy G. Depending on the type of a process, one of these four thermodynamic potentials provides the most convenient description (and is tabulated). All four functions have units of energy. For each TP, a set of so-called “natural variables” exists:

Isolated Systems, independent variables S and V Since these two equations for dU must yield the same result for any dS and dV, the corresponding coefficients must be the same: The combination of parameters on the right side is equal to the exact differential of U. This implies that the natural variables of U are S, V, N, Again, this shows that among several macroscopic variables that characterize the system (P, V, T, , N, etc.), only three are independent, the other variables can be found by taking partial derivatives of the TP with respect to its natural variables. Considering S, V, and N as independent variables: Earlier, by considering the total differential of S as a function of variables U, V, and N, we arrived at the thermodynamic identity for quasistatic processes : Advantages of U : it is conserved for an isolated system (it also has a simple physical meaning – the sum of all the kin. and pot. energies of all the particles). In particular, for an isolated system  Q=0, and dU =  W.

Equilibrium in Isolated Systems Suppose that the system is characterized by a parameter x which is free to vary (e.g., the system might consist of ice and water, and x is the relative concentration of ice). By spontaneous processes, the system will approach the stable equilibrium (x = x eq ) where S attains its absolute maximum. While this constraint is always in place, the system might be out of equilibrium (e.g., we move a piston that separates two sub-systems, see Figure). If the system is initially out of equilibrium, then some spontaneous processes will drive the system towards equilibrium. In a state of stable equilibrium no further spontaneous processes (other than ever-present random fluctuations) can take place. The equilibrium state corresponds to the maximum multiplicity and maximum entropy. All microstates in equilibrium are equally accessible (the system is in one of these microstates with equal probability). This implies that in any of these spontaneous processes, the entropy tends to increase, and the change of entropy satisfies the condition S xx eq For a thermally isolated system  Q = 0. If the volume is fixed, then no work gets done (  W = 0) and the internal energy is conserved: U A, V A, S A U B, V B, S B

Enthalpy (independent variables S and P) The total differential of H in terms of its independent variables : Comparison yields the relations: - the internal energy of a system plus the work needed to make room for it at P=const. The volume V is not the most convenient independent variable. In the lab, it is usually much easier to control P than it is to control V. To change the natural variables, we can use the following trick: In general, if we consider processes with “other” work: H (the enthalpy) is also a thermodynamic potential, with its natural variables S, P, and N. Legendre Trans.:

Processes at P = const,  W other = 0 For the processes with P = const and  W other = 0, the enthalpy plays the same part as the internal energy for the processes with V = const and  W other = 0. For such processes, the change of enthalpy is equal to the thermal energy (“heat”) received by a system. Example: the evaporation of liquid from an open vessel is such a process, because no effective work is done. The heat of vaporization is the enthalpy difference between the vapor phase and the liquid phase. Let’s consider the P = const processes with purely “expansion” work (  W other = 0), At this point, we have to consider a system which is not isolated: it is in a thermal contact with a thermal reservoir.

Systems in Contact with a Thermal Reservoir (a)the energy in the system is no longer fixed (it may flow between the system and reservoir); (b)in order to investigate the stability of an equilibrium, we need to consider the entropy of the combined system (= the system of interest+the reservoir) – according to the 2 nd Law, this total entropy should be maximized. What should be the system’s behavior in order to maximize the total entropy? There are two complications: Reservoir R U R - U s System S U s

Helmholtz Free Energy (independ. variables T and V) The natural variables for F are T, V, N: Let’s do the trick (Legendre transformation) again, now to exclude S : can be rewritten as: The first term – the “energy” pressure – is dominant in most solids, the second term – the “entropy” pressure – is dominant in gases. (For an ideal gas, U does not depend on V, and only the second term survives).

The Minimum Free Energy Principle (V,T = const) UsUs UsUs S R+s FsFs reservoir +system system gain in S s due to transferring U s to the system loss in S R due to transferring U s to the system system’s parameters only stable equilibrium Reservoir R U R - U s System S U s

Processes at T = const The total work performed on a system at T = const in a reversible process is equal to the change in the Helmholtz free energy of the system. In other words, for the T = const processes the Helmholtz free energy gives all the reversible work. For the processes at T = const (in thermal equilibrium with a large reservoir): In general, if we consider processes with “other” work: Problem: Consider a cylinder separated into two parts by an adiabatic piston. Compartments a and b each contains one mole of a monatomic ideal gas, and their initial volumes are V ai =10l and V bi =1l, respectively. The cylinder, whose walls allow heat transfer only, is immersed in a large bath at 0 0 C. The piston is now moving reversibly so that the final volumes are V af =6l and V bi =5l. How much work is delivered by (or to) the system? The process is isothermal : The work delivered to the system: For one mole of monatomic ideal gas: U A, V A, S A U B, V B, S B

Gibbs Free Energy (independent variables T and P) - the thermodynamic potential G is called the Gibbs free energy. Considering T, P, and N as independent variables: Comparison yields the relations: Let’s rewrite dU in terms of independent variables T and P : Let’s do the trick of Legendre transformation again, now to exclude both S and V :

Gibbs Free Energy and Chemical Potential The chemical potential If we add one particle to a system, holding T and P fixed, the Gibbs free energy of the system will increase by . By adding more particles, we do not change the value of  since we do not change the density:    (N). Note that U, H, and F, whose differentials also have the term  dN, depend on N non- linearly, because in the processes with the independent variables (S,V,N), (S,P,N), and (V,T,N),  =  (N) might vary with N.  - this gives us a new interpretation of the chemical potential: at least for the systems with only one type of particles, the chemical potential is just the Gibbs free energy per particle.

Example: Pr.5.9. Sketch a qualitatively accurate graph of G vs. T for a pure substance as it changes from solid to liquid to gas at fixed pressure. - the slope of the graph G(T ) at fixed P should be –S. Thus, the slope is always negative, and becomes steeper as T and S increases. When a substance undergoes a phase transformation, its entropy increases abruptly, so the slope of G(T ) is discontinuous at the transition. T G solid liquid gas T S solid liquid gas - these equations allow computing Gibbs free energies at “non-standard” T (if G is tabulated at a “standard” T)

The Minimum Free Energy Principle (P,T = const) Under these conditions (fixed P, V, and N), the maximum entropy principle of an isolated system is transformed into a minimum Gibbs free energy principle for a system in the thermal contact + mechanical equilibrium with the reservoir. UsUs UsUs S R+s GsGs reservoir +system system G/T is the net entropy cost that the reservoir pays for allowing the system to have volume V and energy U, which is why minimizing it maximizes the total entropy of the whole combined system. Thus, if a system, whose parameters T,P, and N are fixed, is in thermal contact with a heat reservoir, the stable equilibrium is characterized by the condition: stable equilibrium

Processes at P = const and T = const Let’s consider the processes at P = const and T = const in general, including the processes with “other” work : Then The “other” work performed on a system at T = const and P = const in a reversible process is equal to the change in the Gibbs free energy of the system. Gibbs Free Energy  the Spontaneity of Chemical Reactions In other words, the Gibbs free energy gives all the reversible work except the PV work. If the mechanical work is the only kind of work performed by a system, the Gibbs free energy is conserved: dG = 0.

Maxwell relation More in Problem 5.12

Summary PotentialVariables U (S,V,N)S, V, N H (S,P,N)S, P, N F (T,V,N)V, T, N G (T,P,N)P, T, N