Graphite is more compressible than diamond.

(a) Taking compressibilities into account, would you expect the transition from graphite to diamond to occur at higher or lower pressure than that predicted in the text?

(b) The isothermal compressibility of graphite is about 3 x 10-6 bar-1, while that of diamond is more than ten times less and hence negligible in comparison. (Isothermal compressibility is the fractional reduction in volume per unit increase in pressure, as defined in Problem 1.46.) Use this information to make a revised estimate of the pressure at which diamond becomes more stable than graphite (at room temperature).

Short Answer

Expert verified

(a) The graphite-to-diamond transition will occur at a little higher pressure.

(b) Hence, the pressure will be 16.33kbar.

Step by step solution

01

Given information

When the compressibility factor is ignored, the volume of the substance can be used to derive the pressure dependence of Gibbs free energy at constant temperature and is expressed as


GPT=V

Where,

G is the Gibbs energy

P is the pressure

V is the volume of the substance

The Gibbs free energy for one mole of diamond is greater than the Gibbs free energy of one mole of graphite by 2900 J.

02

Explanation 

(a) When the compressibility factor is taken into account, the pressure dependence of the Gibbs free energy (G) can be stated as follows:

GPT=Vo1-κTP

Where,

kT is the isothermal compressibility factor

Vo is the change in the volume of the substance

It can be seen from the preceding relationship that as pressure rises, volume decreases and G rises more slowly.

As a result, the graphite-to-diamond transition will occur at a little higher pressure.

03

Calculations

The pressure at which the diamond is more stable than graphite may be estimated by ignoring the compressibility of both material:

Gg=VgPGd=VdP+2.9kJ

Where,

g, d are for graphite and diamond respectively

G is the free energy

V is the volume

P is the pressure

The intersection of two lines will give the value for pressure

VgP=VdP+2.9kJP=2.9kJVg-Vd

Substituting the value of Vg-Vd=0.189kJ/kbarand solve for P

P=2.9kJ0.189kJ/kbar=15.3kbar

04

Calculations

When the compressibility factor is taken into account, the pressure dependence of Gibbs free energy at constant temperature is

GPT=Vo1-κTP

For a finite value of Gibbs free energy change at constant temperature,

ΔG=0PVo1-κT·PΔP=0PVo-Vo·κT·PΔP

On integrating further

ΔG=P·Vo-Vo·κT·P22

Substituting Gas God-Gogand localid="1646814662046" Vo=Vg-Vdin the equation

God-Gog=PVg-Vd-12Vg-VdκTP2PVg-Vd=God-Gog+12Vg-VdκTP2

Vdcan be neglected as compressibility of diamond is negligible as compared to graphite.

localid="1646814925186" PVg-Vd=God-Gog+12VgκTP2P=1Vg-VdGod-Gog+12VgκTP2

Substituting the value of God-Gog=2.9kJ

P=1Vg-Vd2.9kJ+12VgκTP2

Substituting the values in the above equation

localid="1646815170817" P=1(0.189kJ/kbar)2.9kJ+12(0.531kJ/kbar)3×10-3kbar-1(15.3kbar)2P=1(0.189kJ/kbar)[2.9kJ+0.186kJ]P=3.086kJ(0.189kJ/kbar)P=16.33kbar

Hence, the pressure will be 16.77kbar.

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Most popular questions from this chapter

Repeat the preceding problem with T/TC=0.8

Suppose that a hydrogen fuel cell, as described in the text, is to be operated at 75°Cand atmospheric pressure. We wish to estimate the maximum electrical work done by the cell, using only the room temperature data at the back of this book. It is convenient to first establish a zero-point for each of the three substances, H2,O2,andH2O. Let us take Gfor both H2andO2to be zero at 25°C, so that G for a mole of H2Ois -237KJat 25°C.

(a) Using these conventions, estimate the Gibbs free energy of a mole of H2at 75°C. Repeat for O2andH2O.

(b) Using the results of part (a), calculate the maximum electrical work done by the cell at 75°C, for one mole of hydrogen fuel. Compare to the ideal performance of the cell at25°C.

Problem 5.58. In this problem you will model the mixing energy of a mixture in a relatively simple way, in order to relate the existence of a solubility gap to molecular behaviour. Consider a mixture of A and B molecules that is ideal in every way but one: The potential energy due to the interaction of neighbouring molecules depends upon whether the molecules are like or unlike. Let n be the average number of nearest neighbours of any given molecule (perhaps 6 or 8 or 10). Let n be the average potential energy associated with the interaction between neighbouring molecules that are the same (4-A or B-B), and let uAB be the potential energy associated with the interaction of a neighbouring unlike pair (4-B). There are no interactions beyond the range of the nearest neighbours; the values of μoandμABare independent of the amounts of A and B; and the entropy of mixing is the same as for an ideal solution.

(a) Show that when the system is unmixed, the total potential energy due to neighbor-neighbor interactions is 12Nnu0. (Hint: Be sure to count each neighbouring pair only once.)

(b) Find a formula for the total potential energy when the system is mixed, in terms of x, the fraction of B.

(c) Subtract the results of parts (a) and (b) to obtain the change in energy upon mixing. Simplify the result as much as possible; you should obtain an expression proportional to x(1-x). Sketch this function vs. x, for both possible signs of uAB-u0.

(d) Show that the slope of the mixing energy function is finite at both end- points, unlike the slope of the mixing entropy function.

(e) For the case uAB>u0, plot a graph of the Gibbs free energy of this system

vs. x at several temperatures. Discuss the implications.

(f) Find an expression for the maximum temperature at which this system has

a solubility gap.

(g) Make a very rough estimate of uAB-u0for a liquid mixture that has a

solubility gap below 100°C.

(h) Use a computer to plot the phase diagram (T vs. x) for this system.

In working high-pressure geochemistry problems it is usually more

convenient to express volumes in units of kJ/kbar. Work out the conversion factor

between this unit and m3

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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