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Q. 1.46

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An Introduction to Thermal Physics
Found in: Page 32
An Introduction to Thermal Physics

An Introduction to Thermal Physics

Book edition 1st
Author(s) Daniel V. Schroeder
Pages 356 pages
ISBN 9780201380279

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Short Answer

Measured heat capacities of solids and liquids are almost always at constant pressure, not constant volume. To see why, estimate the pressure needed to keep V fixed as T increases, as follows.

(a) First imagine slightly increasing the temperature of a material at constant pressure. Write the change in volume,dV1, in terms of d T and the thermal expansion coefficient β introduced in Problem 1.7.

(b) Now imagine slightly compressing the material, holding its temperature fixed. Write the change in volume for this process, d V2, in terms of d P and the isothermal compressibility κT, defined as

κT1VVPT

(c) Finally, imagine that you compress the material just enough in part (b) to offset the expansion in part (a). Then the ratio of dP to dT is equal to (P/T)V, since there is no net change in volume. Express this partial derivative in terms of β and κT. Then express it more abstractly in terms of the partial derivatives used to define β and κT. For the second expression you should obtain

PTV=(V/T)P(V/P)T

This result is actually a purely mathematical relation, true for any three quantities that are related in such a way that any two determine the third.

(d) Compute β,κT, and (P/T)V for an ideal gas, and check that the three expressions satisfy the identity you found in part (c).

(e) For water at 25C,β=2.57×104K1 and κT=4.52×1010Pa1. Suppose you increase the temperature of some water from 20C to 30C. How much pressure must you apply to prevent it from expanding? Repeat the calculation for mercury, for which (at 25C ) β=1.81×104K1 andκT=4.04×1011Pa1

Given the choice, would you rather measure the heat capacities of these substances at constant v or at constant p ?

(A) The change in volume in dV1and thermal coefficient is dV1=βVdT

(B) The change in volume of dV2 is dV2=κTVdP

(C) The second expression is PTV=(V/T)P(V/P)T

(D) An ideal gas of three expression is β=1T,κT=1P.PT=βκT

(E) The heat capacities of substances constant is ΔPwater =5.686×106Pa,ΔPmercury =4.48×107Pa

See the step by step solution

Step by Step Solution

Step :1  The thermal expansion coefficient (part a)

Substances' heat capacity can be determined at constant volume or constant pressure. It's relatively simple to assess a gas's heat capacity by enclosing it in a sealed container and keeping it at a constant volume. However, measuring heat capacity at constant pressure is much easier for solids and liquids. We can calculate how much pressure must be increased to prevent a solid or liquid from expanding when heated.

(a) The thermal expansion coefficient is:

β=ΔV/VΔT

Imagine that the substrate atmospheric temperature slightly at constant pressure, and the thermal expansion coefficient, which is a measure of the relative volume change with temperature at constant pressure, is:

β=ΔV/VΔT=1VVTpVTp=βV

However, becauseV is a function of T and P,V(T,P), the volume change due to the differential:

dV=VPTdP+VTPdT

Equation (2) becomes: dp=0at constant pressure.

dV=VTPdT

Substitute (2) for (1) to get the following volume change:

dV1=βVdT

Step :2  Constant temperature (part b)

(b) Assume we compress a solid (or a liquid) slightly at constant temperature d T= 0, resulting in equation (2):

dV=VPTdP

Given that the isothermal compressibility is the reciprocal of the bulk modulus:

κT=1VVPTVPT=κTV

Substituting equation (5) into equation (4), the volume change is:

dV2=κTVdP

Step :3 Change in volume after two action (part c)

(c) The net change in volume after the two actions in (a) and (b) is zero:

dV1+dV2=0dV1=dV2

Substitute

βVdT=κTVdP

PTV=βκT

From (1) and (5)

PTV=βκy=1VVTΓ1VVPT

PTV=PTTVPT

PTV=(V/T)P(V/P)T

Step :4  Ideal gas law (part d)

(d) From the ideal gas law, PV=NkT, and using equation (5) and (1) we have:

β=1VVTp=1VNkTPTp

β=NkPV=NkNkT=1T

κT=1VVPT=1VNkTPPT=NkTVP2

κT=NkTVP2=NkT(VP)P=NkT(NkT)P=1P

Divide

PT=βκT

Now from equation

PTV=βκT

NkTVTV=βκT

NkV=βκT

PT=βκT

We can conclude that the results from (d), equation , and (c) equation , are identical.

Step :5  For water (part e)

(e) For water, the given values are:

β=2.57×104K1κ=4.52×1010Pa1

So the pressure increase

PT=βκTP=βκTTΔP=βκTΔT

But the temperature difference is

ΔT=TfTi=3020=10K

So the pressure difference is

ΔP=βκTΔT=2.57×1044.52×1010×10=5.686×106Pa

ΔP=5.686×106Pa

For mercury the temperature range is

β=1.81×104K1κ=4.04×1011Pa1

So the pressure increase must be

ΔP=βκTΔT=1.81×1044.04×1011×10ΔP=4.48×107Pa

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