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New trends in physics teaching, v.4; The ... - unesdoc - Unesco

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Introductory statistical <strong>physics</strong><br />

dp = -nmg dh<br />

m be<strong>in</strong>g the mass of one molecule. <strong>The</strong> rest follows us<strong>in</strong>g k<strong>in</strong>etic theory.<br />

Feynman then presents this result, not as a special case but as an <strong>in</strong>stance of a general result<br />

n = constant exp(-E/kT)<br />

<strong>in</strong> which exp(-E/kT) is the Boltzmann factor with mgh generalized to any appropriate potential<br />

energy difference.<br />

Figure 1 shows how Feynman’s strategy works, After an <strong>in</strong>troduction on random walks to<br />

<strong>in</strong>troduce statistical distributions, the exponential atmosphere argument is used to go straight to<br />

applications of the Boltzmann factor, of which he gives several varied examples. But nowhere<br />

Exponential<br />

atmosphere<br />

Boltzmann<br />

factor<br />

ll<br />

Reversible and<br />

i rrevers i b le<br />

processes<br />

Chance<br />

State, distribution<br />

E<strong>in</strong>ste<strong>in</strong> solid; Boltzmann factor;<br />

Mix<strong>in</strong>g W,,,<br />

Q‘/Q =N/n<br />

c a I cu lat io n by<br />

permutation unit change<br />

quantum shuffl<strong>in</strong>g<br />

Isothermal<br />

expansion<br />

AlnQ=Nln2<br />

A S =NRTA 1nV<br />

Entropy: use of<br />

numerical values<br />

I<br />

Uses of Boltzmann:<br />

vapour pressure<br />

Uses of entropy:<br />

equilibrium<br />

meltlng, evaporation<br />

eng<strong>in</strong>es. cycles<br />

statistical<br />

Figure 1. Feynman’s <strong>in</strong>troductory method.<br />

159

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