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Lesson 42 · Changing state
Energy in, temperature flat
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Energy in, temperature flat

Drop a thermometer in melting ice and watch: heat pours in, and the reading parks at 0 °C until the last crystal is gone. On a heating curve that is the plateau — and it is where Q=mc ΔTQ = mc\,\Delta T goes powerless, because ΔT=0\Delta T = 0 there. The energy is still being spent; it is buying a change of phase, prying the molecules apart instead of speeding them up.

The plateau has its own machine: Q=mLQ = mL (read aloud: Q equals m L): the heat QQ in joules, the mass mm crossing in kilograms, and LL, the latent heat — the crossing fee per kilogram, in J/kg, with no ΔT\Delta T anywhere in it. Water charges two different fares, and the subscript says which crossing: LfL_f is fusion, the melting-and-freezing fee, Lf=334 kJ/kgL_f = 334\ \mathrm{kJ/kg}; LvL_v is vaporization, the boiling-and-condensing fee, Lv=2260 kJ/kgL_v = 2260\ \mathrm{kJ/kg} — nearly seven times steeper. Match the L to the crossing, and never let mc ΔTmc\,\Delta T anywhere near a plateau.

QLmm

Q=mLQ = m L

  • QQ= Heat absorbed or released (energy)
  • mm= Mass changing phase (mass)
  • LL= Specific latent heat (specific latent heat)
Latent Heat solver →