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

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

one could not convert any of its heat energy <strong>in</strong>to work’; ‘. . . if we could obta<strong>in</strong> work by extract<strong>in</strong>g<br />

the heat out of the ocean’. Such remarks can only be read as speak<strong>in</strong>g of heat as the energy<br />

<strong>in</strong>side th<strong>in</strong>gs. Feynman is perfectly aware of the difference between heat and <strong>in</strong>ternal energy,<br />

and frequently draws all the necessary dist<strong>in</strong>ctions. But it is, I th<strong>in</strong>k, a property of many<br />

approaches to statistical mechanics, which emphasize particular microscopic models, that they<br />

tend to make it natural to blur the dist<strong>in</strong>ction: to talk at one moment of heat as flow<strong>in</strong>g under a<br />

temperature difference and at another of heat as <strong>in</strong>ternal energy, usually ‘random’ <strong>in</strong> some<br />

sense. Indeed, <strong>in</strong> the exponential atmosphere argument, one is left with some impression that the<br />

molecules climb the gravitational hill at the expense of the ‘random’ <strong>in</strong>ternal energy or heat <strong>in</strong><br />

the gas.<br />

What is the Feynman’s temperature scale?<br />

Feynman offers the excuse to raise another matter.<br />

In the expression exp(- EIkT), what is T? In his approach to the Boltzmann factor, it appears<br />

that T is the temperature on the ideal gas scale, because the argument derives from the gas laws<br />

and k<strong>in</strong>etic theory. More fundamentally, of course, it is not that at all, but is a temperature<br />

def<strong>in</strong>ed statistically ; def<strong>in</strong>ed by a relation of the form<br />

T = E/kA lnn<br />

<strong>in</strong> which k functions, not as R/N, but as an arbitrary scale constant l<strong>in</strong>k<strong>in</strong>g an energy E and a<br />

change <strong>in</strong> the logarithm of a number of microstates to the Kelv<strong>in</strong> scale on which the triple po<strong>in</strong>t<br />

of water has a chosen value.<br />

Of course the ideal gas temperature is the same th<strong>in</strong>g, but it is the same because of what ideal<br />

gases are, not because of what temperature is. Similarly k = R/N because of the nature of ideal<br />

gases; the relation says noth<strong>in</strong>g about k.<br />

THE PSSC’ APPROACH<br />

<strong>The</strong> PSSC Physics: Advanced Topics Supplement (1 968) and College Physics (1968) propose a<br />

quite different, equally radical and equally simple approach, now ma<strong>in</strong>ly focused on the second<br />

law from a statistical po<strong>in</strong>t of view.<br />

<strong>The</strong> overall strategy<br />

<strong>The</strong> PSSC strategy is startl<strong>in</strong>gly simple. Perhaps the easiest case of all to argue statistically is that<br />

of the spread<strong>in</strong>g out of N <strong>in</strong>dependent particles <strong>in</strong>to double the previous volume. Argu<strong>in</strong>g that<br />

each has a probability of 50 per cent of be<strong>in</strong>g by chance <strong>in</strong> the orig<strong>in</strong>al half, the probability that<br />

all the particles wil so do is YP or 2-N. <strong>The</strong> logarithm -N In 2 of this quantity appears <strong>in</strong> the<br />

expression NkT In 2 for the work done <strong>in</strong> chang<strong>in</strong>g the volume (isothermally). In this case, the<br />

work done is equal to the heat exchanged with a heat s<strong>in</strong>k, so<br />

AQ = NkT In 2<br />

1. Physical Science Study Committee.<br />

161

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