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1.1

The crisis of classical physics

By 1900 physics looked finished. Three unremarkable experimental facts tore up the foundations.

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After this section you should be able to

  • State what classical physics covered around 1900 and what it believed it had settled
  • Say exactly where each of the three dead ends gets stuck: the ultraviolet catastrophe, low-temperature specific heat, atomic stability
  • Explain why none of the three can be fixed by patching classical theory

Start with something slightly counter-intuitive: physicists in 1900 did not feel anything was missing.

The textbooks divided the world up like this:

  • Mechanics handles how things move. Newton’s three laws plus gravitation get you from cannonballs to Neptune.
  • Electromagnetism handles electricity, magnetism and light. Maxwell’s four equations unified them and predicted electromagnetic waves into the bargain — which Hertz duly produced in 1887.
  • Thermodynamics and statistical mechanics handle heat, energy and entropy. Boltzmann reduced macroscopic temperature to molecules banging about.

Between them they covered essentially every experiment that could then be done. Students were occasionally advised against reading physics on the grounds that all that remained was measuring the constants to another decimal place.

This chapter is about how the second cloud turned into a downpour. To make the road ahead easier, let us first lay out the three most damaging contradictions — not solving them, just being precise about where they get stuck.

Dead end one: heat something up and the formula returns infinity

Anything with a temperature glows. Iron at 600 °C is dull red, at 1200 °C orange-white; the Sun’s surface at 5800 K is white. Physicists idealised this as a black body: a cavity that only absorbs and never reflects, observed through a small hole.

The question is plain: how is the radiated energy distributed across frequencies?

The measured curve is of course nothing like this. It rises, peaks at some frequency, then falls, and the total energy is finite.

Note the character of this failure: the theory is not slightly off, it returns infinity. That kind of error cannot be repaired with a correction factor.

Dead end two: cool it down and the heat capacity “vanishes”

The second dead end uses the same equipartition theorem in a different setting.

Each atom in a solid vibrates about its lattice site, which we can treat as three springs. Each oscillator has kinetic and potential energy, equipartition hands it kBTk_BT, and a mole of solid therefore has

CV=3NAkB=3R25 J/(molK)(1.1.3)C_V=3N_Ak_B=3R\approx 25\ \text{J}/(\text{mol}\cdot\text{K})\tag{1.1.3}

This is the Dulong–Petit law, and at room temperature it is startlingly accurate for most metals.

How can equipartition fail? Its derivation uses only the most basic assumptions of statistical mechanics. Either statistical mechanics is wrong, or the premise that “every degree of freedom can take up energy continuously” is wrong.

Dead end three: a classical atom lasts under a ten-billionth of a second

In 1911 Rutherford fired alpha particles at gold foil and found that the positive charge and nearly all the mass sit in a tiny nucleus, with the electrons outside. So what are the electrons doing?

A stationary electron would simply be pulled straight into the nucleus by the Coulomb force. So it must orbit — like a planet round the Sun.

The classical model cannot account for spectra either. A continuously shrinking orbit means a continuously changing frequency, so atoms should emit a continuous spectrum. What is actually measured is a set of sharp lines, positioned precisely enough to serve as an element’s fingerprint.

What comes next

Of the three dead ends, the first was prised open first. At the end of 1900, in order to make a formula match the measured curve, Planck made an assumption he himself was unhappy with.

The next section looks at what he actually did, and why he spent more than a decade refusing to believe it.

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