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Lesson 3 · Warming and melting
Slopes and plateaus
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Slopes and plateaus

Heat a beaker of ice steadily and plot temperature against time. The graph is not a ramp — it is a staircase of slopes and plateaus, and each kind of segment has its own machine. On a slope the temperature climbs and Q=mc ΔTQ = mc\,\Delta T answers. On a plateau the thermometer sits still while energy pours in, and the machine is Q=mLQ = mL — Q equals m L, where QQ is the heat in joules, mm is the mass changing phase in grams, and LL is the specific latent heat in joules per gram: the price of changing one gram's phase, with no temperature change bought at all.

Water carries two of them: melting costs Lf=334 J/gL_f = 334\ \mathrm{J/g} (the subscript f is for fusion, the chemist's word for melting) and boiling costs Lv=2260 J/gL_v = 2260\ \mathrm{J/g} (v for vaporization). Nearly seven times as much — which is why a pot takes minutes to reach boiling and then a quarter of an hour to boil dry. The named exam wound: reaching for mc ΔTmc\,\Delta T on a plateau. There ΔT=0\Delta T = 0, so the machine cheerfully reports that melting an iceberg is free. Look at which segment the question lives on BEFORE you pick up a formula.

mcpQΔT

Q=mcΔTQ = m c \Delta T

  • QQ= Heat energy (energy)
  • mm= Mass (mass)
  • cpc_p= Specific heat capacity (specific heat capacity)
  • ΔT\Delta T= Temperature change (temperature difference)
Sensible Heat (Q = mcΔT) solver →
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 →