In this problem you will derive approximate formulas for the shapes of the phase boundary curves in diagrams such as Figures 5.31 and 5.32, assuming that both phases behave as ideal mixtures. For definiteness, suppose that the phases are liquid and gas.

(a) Show that in an ideal mixture of A and B, the chemical potential of species A can be written μA=μA°+kTln(1-x)where A is the chemical potential of pure A (at the same temperature and pressure) and x=NB/NA+NB. Derive a similar formula for the chemical potential of species B. Note that both formulas can be written for either the liquid phase or the gas phase.

(b) At any given temperature T, let x1 and xgbe the compositions of the liquid and gas phases that are in equilibrium with each other. By setting the appropriate chemical potentials equal to each other, show that x1and xg obey the equations =1-xl1-xg=eΔGA°/RTandxlxg=eΔGB°/RT and where ΔG°represents the change in G for the pure substance undergoing the phase change at temperature T.

(c) Over a limited range of temperatures, we can often assume that the main temperature dependence of ΔG°=ΔH°-TΔS°comes from the explicit T; both ΔH°andΔS°are approximately constant. With this simplification, rewrite the results of part (b) entirely in terms of ΔHA°,ΔHB° TA, and TB (eliminating ΔGandΔS). Solve for x1and xgas functions of T.

(d) Plot your results for the nitrogen-oxygen system. The latent heats of the pure substances areΔHN2°=5570J/molandΔHO2°=6820J/mol. Compare to the experimental diagram, Figure 5.31.

(e) Show that you can account for the shape of Figure 5.32 with suitably chosenΔH° values. What are those values?

Short Answer

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Step by step solution

01

Given information

Diagrams such as Figures 5.31 and 5.32, assuming that both phases behave as ideal mixtures. For definiteness, suppose that the phases are liquid and gas.

02

 Step 2: Explanation

The Gibbs free energy is given by:

G=U-TS+PV

For a single component ideal gas system at constant temperature, the change in Gibbs free energy with pressure is:

G-G°=p°pVdP

where,

p°is the pressure of the pure Substance

G°is the Gibbs free energy of the pure substance.

Substituting from the ideal gas law, we get

V=nRT/P

G-G°=nRTp°pdPP

Integrating it,

role="math" localid="1647032806277" G-G°=nRT[ln(P)]p°pG-G°=nRTlnpp°G=G°+nRTlnpp°(1)

In terms of chemical potential, the Gibbs free energy is given by:

G=Nμ

Substitute this into (1)

Nμ=Nμ°+NkTlnpp°μ=μ°+kTlnpp°

Let's say we have substance A, and its chemical potential is as follows:

μA=μA°+kTlnpp°

When another substance B is added to A, the chemical potential of A in the mixture is calculated as follows:

μA=μA°+kTlnpAp°

Let the fraction of the substance B be r thus the fraction of substance A is 1- a, the pressure can be written as:

pA=(1-x)p°

Now, we get

μA=μA°+kTln(1-x)(2)

For B we get

μB=μB°+kTln(x)(3)

03

Explanation

Let x1 and xg be the equilibrium compositions of the liquid and gas phases, respectively, and equating the chemical potentials yields:

μg=μl

Using (2), we have

μg°+kTln1-xg=μl°+kTln1-xlμg°-μl°kT=ln1-xl-ln1-xg

For 1 mole, we have NAk=R

NAμg°-μl°RT=ln1-xl1-xgNAΔμA°RT=ln1-xl1-xg

But ΔGA°=NAΔμA°

ΔGA°RT=ln1-xl1-xg

Exponentiation both sides

eΔGA°/RT=1-xl1-xg(4)

Now using (3) we get

μg°+kTlnxg=μl°+kTlnxlμg°-μl°kT=lnxl-lnxg

For 1 mole we have NBk=R

NBμg°-μl°RT=lnxlxgNBΔμA°RT=lnxlxg

But ΔGB°=NBΔμB°

ΔGB°RT=lnxlxg

exponentiation both sides to get:

eΔGB°/RT=xlxg(5)

04

 Step 4: Explanation

For a short range temperatures we can use ΔG°=ΔH°-TΔS°

So from (4) and (5), we get

eΔHA°-TΔSA°/RT=1-xl1-xgeΔHB°-TΔSB°/RT=xlxg

To eliminate it, we must solve these equations for and x1and xg, substituting from the second equation into the first:

1-xgeΔHA°-TΔSA°/RT=1-xgeΔHB°-TΔSB°/RTxgeΔHA°-TΔSA°/RT-eΔHB°-TΔSB°/RT=1-eΔHA°-TΔSA°/RTxg=1-eΔHA°-TΔSA°/RTeΔHA°-TΔSA°/RT-eΔHB°-TΔSB°/RT

Substitute in second equation

xl=1-eΔHA°-TΔSA°/RTeΔHB°-TΔSB°/RTeΔHA°-TΔSA°/RT-eΔHB°-TΔSB°/RT

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Most popular questions from this chapter

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.

A mixture of one part nitrogen and three parts hydrogen is heated, in the presence of a suitable catalyst, to a temperature of 500° C. What fraction of the nitrogen (atom for atom) is converted to ammonia, if the final total pressure is 400 atm? Pretend for simplicity that the gases behave ideally despite the very high pressure. The equilibrium constant at 500° C is 6.9 x 10-5. (Hint: You'l have to solve a quadratic equation.)

Repeat the preceding problem with T/TC=0.8

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:

NaAlSi3O8NaAlSi2O6+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 S and V.

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

κT=κS+TVβ2CP.

(Here κS=-(1/V)(V/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.

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