In Problems 3.30 and 3.31 you calculated the entropies of diamond and graphite at 500 K. Use these values to predict the slope of the graphite- diamond phase boundary at 500 K, and compare to Figure 5.17. Why is the slope almost constant at still higher temperatures? Why is the slope zero at T = 0?

Short Answer

Expert verified

At T=0 K the slope will be zero.

Step by step solution

01

Given information

We have the information of entropies, so

Entropy of diamond at500KisSa=7·59J/KEntropy of diamond at500KisSg=12·33J/KMolar Volumes of diamond isVd=3·42cm3=3.42×10-6m3Molar Volumes of graphite isVg=6·30cm3=5·30×10-6m3

Now, the change in entropies and molar volume will be:

Change in entropiesΔS=Sg-Sd=12·33J/K-7·59J/K=4.74J/K

role="math" localid="1646931515944" ChangeinMolarvolumesΔV=Vg-Vd=5·30×10-6m3-3·42×10-6m3=1.88×10-6m3

02

Calculation

The slope of phase boundary will be:

dPdT=ΔSΔV=4.74J/K1·88×10-6m3=2·5213×106N/m2KdPdT=2·52×106PaK

The graphite-diamond phase boundary slope at 500 K is this.

03

Calculations

ΔS0at high temperatures because, according to the Dulong-Petits law, both heat capacities approach 3R at high temperatures.

ΔS0

AsT0, both entropies approaches zero, soΔS0

dPdT=ΔSΔV=0

At T=0 K the slope will be zero.

Unlock Step-by-Step Solutions & Ace Your Exams!

  • Full Textbook Solutions

    Get detailed explanations and key concepts

  • Unlimited Al creation

    Al flashcards, explanations, exams and more...

  • Ads-free access

    To over 500 millions flashcards

  • Money-back guarantee

    We refund you if you fail your exam.

Over 30 million students worldwide already upgrade their learning with Vaia!

One App. One Place for Learning.

All the tools & learning materials you need for study success - in one app.

Get started for free

Most popular questions from this chapter

The formula for Cp-Cv derived in the previous problem can also be derived starting with the definitions of these quantities in terms of U and H. Do so. Most of the derivation is very similar, but at one point you need to use the relation P=-(F/V)T.

Go through the arithmetic to verify that diamond becomes more stable than graphite at approximately 15 kbar.

The density of ice is 917 kg/m*.

(a) Use the Clausius-Clapeyron relation to explain why the slope of the phase boundary between water and ice is negative.

(b) How much pressure would you have to put on an ice cube to make it melt at -1°C?

(c) ApprOximately how deep under a glacier would you have to be before the weight of the ice above gives the pressure you found in part (b)? (Note that the pressure can be greater at some locations, as where the glacier flows over a protruding rock.)

(d) Make a rough estimate of the pressure under the blade of an ice skate, and calculate the melting temperature of ice at this pressure. Some authors have claimed that skaters glide with very little friction because the increased pressure under the blade melts the ice to create a thin layer of water. What do you think of this explanation?

The compression factor of a fluid is defined as the ratio PV/NkT; the deviation of this quantity from 1 is a measure of how much the fluid differs from an ideal gas. Calculate the compression factor of a Van der Waals fluid at the critical point, and note that the value is independent of a and b. (Experimental values of compression factors at the critical point are generally lower than the Van der Waals prediction, for instance, 0.227 for H22O, 0.274 for CO22, and 0.305 for He.)

Consider a completely miscible two-component system whose overall composition is x, at a temperature where liquid and gas phases coexist. The composition of the gas phase at this temperature is xaand the composition of the liquid phase is xb. Prove the lever rule, which says that the proportion of liquid to gas is x-xa/xb-x. Interpret this rule graphically on a phase diagram.

See all solutions

Recommended explanations on Physics Textbooks

View all explanations

What do you think about this solution?

We value your feedback to improve our textbook solutions.

Study anywhere. Anytime. Across all devices.

Sign-up for free