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 Sfixed, each /Sis taken with Vfixed, and Nis always held fixed. From the thermodynamic identity (forU) 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,andG ). 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.

Short Answer

Expert verified

Maxwell relations are:

TVS=-PSVTPS=VSPTPS=PTVSPT=-VTP

Step by step solution

01

To find

Four Maxwell relations.

02

Keeping N as constant derive the given equation.

We have the thermodynamics identity:

dU=TdS-PdV+μdN

at constant volume and number of molecules (at which dN=0anddV=0)

we have:

T=USV............(1)

and at constant entropy and number of molecules (at which dN=0anddS=0)

we have:

P=-UVS............(2)

In the given we have: role="math" localid="1648414830374" VUS=SUV.......(3)

Now substitute equation (1) and (2) in (3)

TVS=-PSV

03

continuing derivation

We have following the enthalpy identity as:

dH=TdS+VdP+μdN

at constant pressure and number of molecules (at which dN=0anddP=0) we have:

role="math" localid="1648416938771" T=HSP.........(3)

again differentiate equation (3) w.r.t. P

TPS=HPS

Then at constant entropy and number of molecules (at which dN=0anddS=0) we have:

role="math" localid="1648416952292" V=HPS.........(4)

again differentiate equation (4) w.r.t. V

VSP=HPS

combine these two equations together to get the following result:

TPS=VSP

04

continuing derivation 

We have following the Helmholtz free energy is given by:

dF=-SdT-PdV+μdN

at constant pressure and number of molecules (at which dN=0anddP=0) we have:

role="math" localid="1648418905850" S=-FTP......(5)

again differentiate equation (5) w.r.t. V

SVT=-FVT

and at constant entropy and number of molecules (at which dN=0anddS=0) we have:

role="math" localid="1648418958034" P=-FVS......(6)

again differentiate equation (6) w.r.t. T

PTV=-FVT

combine these two equations together to get the following result:

TPS=PTV

05

continuing derivation 

We have following the Gibbs free energy is given by:

dG=-SdT+VdP+μdN

at constant pressure and number of molecules (at which dN=0anddP=0) we have:

role="math" localid="1648419302437" S=-GTP.......(7)

again differentiate the equation (7) w.r.t. P

SPT=-GPT

and at constant temperature and number of molecules (at which dN=0anddT=0) we have:

role="math" localid="1648419374743" V=GPS.......(8)

again differentiate equation (8) w.r.t. T

VTP=GPT

combine these two equations together to get the following result:

SPT=-VTP

06

Final answer

Maxwell relations are:

TVS=-PSVTPS=VSPTPS=PTVSPT=-VTP

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Most popular questions from this chapter

Calcium carbonate, CaCO3, has two common crystalline forms, calcite and aragonite. Thermodynamic data for these phases can be found at the back of this book.

(a) Which is stable at earth's surface, calcite or aragonite?

(b) Calculate the pressure (still at room temperature) at which the other phase

should become stable.

Assume that the air you exhale is at 35°C, with a relative humidity of 90%. This air immediately mixes with environmental air at 5°C and unknown relative humidity; during the mixing, a variety of intermediate temperatures and water vapour percentages temporarily occur. If you are able to "see your breath" due to the formation of cloud droplets during this mixing, what can you conclude about the relative humidity of your environment? (Refer to the vapour pressure graph drawn in Problem 5.42.)

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.

Let the system be one mole of argon gas at room temperature and atmospheric pressure. Compute the total energy (kinetic only, neglecting atomic rest energies), entropy, enthalpy, Helmholtz free energy, and Gibbs free energy. Express all answers in SI units.

Compare expression 5.68 for the Gibbs free energy of a dilute solution to expression 5.61 for the Gibbs free energy of an ideal mixture. Under what circumstances should these two expressions agree? Show that they do agree under these circumstances, and identify the function f(T, P) in this case.

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