Problem 5.35. The Clausius-Clapeyron relation 5.47 is a differential equation that can, in principle, be solved to find the shape of the entire phase-boundary curve. To solve it, however, you have to know how both L and V depend on temperature and pressure. Often, over a reasonably small section of the curve, you can take L to be constant. Moreover, if one of the phases is a gas, you can usually neglect the volume of the condensed phase and just take V to be the volume of the gas, expressed in terms of temperature and pressure using the ideal gas law. Making all these assumptions, solve the differential equation explicitly to obtain the following formula for the phase boundary curve:

P= (constant) x e-L/RT

This result is called the vapour pressure equation. Caution: Be sure to use this formula only when all the assumptions just listed are valid.

Short Answer

Expert verified

HenceP=constant×e-LRT

Step by step solution

01

Given information

Using the ideal gas law,

PVg=RTVg=RTP

Using Clausius Clapeyron Equation

dPdT=LT·ΔVdPdT=LT·Vg=LT×RTP=P·LRT2dPP=LR·dTT2

02

Calculation

Integrating both sides

dPP=LR·dTT2lnP=-LR·1T+constant

Exponentiating both sides

P=e-LRT+const
role="math" localid="1646902017006" P=constant×e-LRT

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Most popular questions from this chapter

Because osmotic pressures can be quite large, you may wonder whether the approximation made in equation5.74is valid in practice: Is μ0really a linear function of Pto the required accuracy? Answer this question by discussing whether the derivative of this function changes significantly, over the relevant pressure range, in realistic examples.

μ0T,P2μ0T,P1+P2-P1μ0P......equation(5.74)

How can diamond ever be more stable than graphite, when it has

less entropy? Explain how at high pressures the conversion of graphite to diamond

can increase the total entropy of the carbon plus its environment.

Functions encountered in physics are generally well enough behaved that their mixed partial derivatives do not depend on which derivative is taken first. Therefore, for instance,
VUS=SUV

where each /Vis taken with S fixed, each/S is taken with V fixed, and N is always held fixed. From the thermodynamic identity (for U ) you can evaluate the partial derivatives in parentheses to obtain

TVS=-PSV

a nontrivial identity called a Maxwell relation. Go through the derivation of this relation step by step. Then derive an analogous Maxwell relation from each of the other three thermodynamic identities discussed in the text (for H, F, and G ). Hold N fixed in all the partial derivatives; other Maxwell relations can be derived by considering partial derivatives with respect to N, but after you've done four of them the novelty begins to wear off. For applications of these Maxwell relations, see the next four problems.


Repeat the preceding problem with T/TC=0.8

When carbon dioxide "dissolves" in water, essentially all of it reacts to form carbonic acid, H2CO3:

CO2(g)+H2O(l)H2CO3(aq)

The carbonic acid can then dissociate into H* and bicarbonate ions,

H2CO3(aq)H+(aq)+HCO3-(aq)

(The table at the back of this book gives thermodynamic data for both of these reactions.) Consider a body of otherwise pure water (or perhaps a raindrop) that is in equilibrium with the atmosphere near sea level, where the partial pressure of carbon dioxide is 3.4 x 10-4 bar (or 340 parts per million). Calculate the molality of carbonic acid and of bicarbonate ions in the water, and determine the pH of the solution. Note that even "natural" precipitation is somewhat acidic.

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