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Use the definition of temperature to prove the zeroth law of thermodynamics, which says that if system A is in thermal equilibrium with system B, and system B is in thermal equilibrium with system C, then system A is in thermal equilibrium with system C. (If this exercise seems totally pointless to you, you're in good company: Everyone considered this "law" to be completely obvious until 1931, when Ralph Fowler pointed out that it was an unstated assumption of classical thermodynamics.)

Short Answer

Expert verified

When the slopes of all three systems A, B, and C are equal, the systems are considered to be in thermal equilibrium, or at the same temperature.

Step by step solution

01

Concept Introduction

Temperature is a measure of hotness or coldness represented on one of several arbitrary scales that describes the natural flow of heat energy.

02

Explanation

If two items are in thermal equilibrium, their temperatures are said to be the same. The entropy and energy of a system can be used to express temperature. The gauge of randomness is entropy. The Zeroth law states that if a system A and a system B are in thermal equilibrium with another system C individually, then systems A and B will be in thermal equilibrium as well.

Mathematically, temperature can be stated as:

1T=SU

By rearranging the terms,

T=US

The entropy vs energy graph will have equal slopes if the system is in thermal equilibrium. Because any two systems in thermal equilibrium have the same SUvalues, system B and C must have the same slope as system A, resulting in their slopes being identical. The zeroth law, which asserts that a system A can be set in thermal equilibrium with any other systems that are all in thermal equilibrium with each other, is the foundation of thermodynamics.

03

Final answer

As a result, if the slopes of all three systems A, B, and C are similar, the systems are said to be in thermal equilibrium, or at the same temperature.

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Most popular questions from this chapter

Sketch (or use a computer to plot) a graph of the entropy of a two-state paramagnet as a function of temperature. Describe how this graph would change if you varied the magnetic field strength.

Verify every entry in the third line of Table 3.2 (starting with N=98.

Use Table 3.1 to compute the temperatures of solid A and solid B when qA=1. Then compute both temperatures when qA=60. Express your answers in terms of ε/k, and then in kelvins assuming that ε=0.1eV.

Consider a monatomic ideal gas that lives at a height z above sea level, so each molecule has potential energy mgzin addition to its kinetic energy.

(a) Show that the chemical potential is the same as if the gas were at sea level, plus an additional term mgz:

μ(z)=-kTlnVN2πmkTh23/2+mgz.

(You can derive this result from either the definition μ=-T(S/N)U,Vor the formula μ=(U/N)S,V.

(b) Suppose you have two chunks of helium gas, one at sea level and one at height z, each having the same temperature and volume. Assuming that they are in diffusive equilibrium, show that the number of molecules in the higher chunk is

N(z)=N(0)e-mgz/kT

in agreement with the result of Problem 1.16.

When the sun is high in the sky, it delivers approximately 1000 watts of power to each square meter of earth's surface. The temperature of the surface of the sun is about 6000K, while that of the earth is about 300K.

(a) Estimate the entropy created in one year by the flow of solar heat onto a square meter of the earth.

(b) Suppose you plant grass on this square meter of earth. Some people might argue that the growth of the grass (or of any other living thing) violates the second law of thermodynamics, because disorderly nutrients are converted into an orderly life form. How would you respond?

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