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Calculate the Helmholtz free energy of a van der Waals fluid, up to an undetermined function of temperature as in equation5.56. Using reduced variables, carefully plot the Helmholtz free energy (in units of NkTc) as a function of volume for T/Tc=0.8Identify the two points on the graph corresponding to the liquid and gas at the vapor pressure. (If you haven't worked the preceding problem, just read the appropriate values off Figure5.23.) Then prove that the Helmholtz free energy of a combination of these two states (part liquid, part gas) can be represented by a straight line connecting these two points on the graph. Explain why the combination is more stable, at a given volume, than the homogeneous state represented by the original curve, and describe how you could have determined the two transition volumes directly from the graph of F.

Short Answer

Expert verified

The Helmholtz free energy is:

F=xFl+(1-x)Fg=Fg-xFg-Fl

Step by step solution

01

Given information

We have been givenF=G-PVfor any type of system, we can use gibbs free energy.

02

Simplify

Terms used in this:

Pin terms of V:

F=-NkTln(V-Nb)+(NkT)(Nb)V-Nb-2aN2V-PV+c(T)

when we put the expression in terms of dimensionless variable

=-tln(3v-1)-98v+f(t)

To plot this function we use

Plot[-.8*log[3v-1]-9/(8v),{v,.4,6}]

Then the total volume of the system is:

F=xFl+(1-x)Fg=Fg-xFg-Fl

On elimination x from equation ,we get:

F=Fg-Vg-VVg-VlFg-Fl.

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Most popular questions from this chapter

When solid quartz "dissolves" in water, it combines with water molecules in the reaction

SiO2(s)+2H2O(l)โŸทH4SiO4(aq)

(a) Use this data in the back of this book to compute the amount of silica dissolved in water in equilibrium with solid quartz, at 25ยฐ C

(b) Use the van't Hoff equation (Problem 5.85) to compute the amount of silica dissolved in water in equilibrium with solid quartz at 100ยฐC.

The methods of this section can also be applied to reactions in which one set of solids converts to another. A geologically important example is the transformation of albite into jadeite + quartz:

NaAlSi3O8โŸทNaAlSi2O6+SiO2

Use the data at the back of this book to determine the temperatures and pressures under which a combination of jadeite and quartz is more stable than albite. Sketch the phase diagram of this system. For simplicity, neglect the temperature and pressure dependence of both โˆ†S and โˆ†V.

A formula analogous to that for CP-CVrelates the isothermal and isentropic compressibilities of a material:

ฮบT=ฮบS+TVฮฒ2CP.

(Here ฮบS=-(1/V)(โˆ‚V/โˆ‚P)Sis the reciprocal of the adiabatic bulk modulus considered in Problem 1.39.) Derive this formula. Also check that it is true for an ideal gas.

Below 0.3 K the slope of the ยฐHe solid-liquid phase boundary is negative (see Figure 5.13).

(a) Which phase, solid or liquid, is more dense? Which phase has more entropy (per mole)? Explain your reasoning carefully.

(b) Use the third law of thermodynamics to argue that the slope of the phase boundary must go to zero at T = 0. (Note that the *He solid-liquid phase boundary is essentially horizontal below 1 K.)

(c) Suppose that you compress liquid *He adiabatically until it becomes a solid. If the temperature just before the phase change is 0.1 K, will the temperature after the phase change be higher or lower? Explain your reasoning carefully.

Problem 5.64. Figure 5.32 shows the phase diagram of plagioclase feldspar, which can be considered a mixture of albite NaAlSi3O8and anorthiteCaAl2Si2O8

a) Suppose you discover a rock in which each plagioclase crystal varies in composition from center to edge, with the centers of the largest crystals composed of 70% anorthite and the outermost parts of all crystals made of essentially pure albite. Explain in some detail how this variation might arise. What was the composition of the liquid magma from which the rock formed?

(b) Suppose you discover another rock body in which the crystals near the top are albite-rich while the crystals near the bottom are anorthite-rich. Explain how this variation might arise.

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