Section 6.2 · Further exercises · 2 of 13
Exercise 6.2.2: Why ice defrosts slowly
About the further exercises of Section 6.2
Thirteen further exercises in the spirit of the problems, the worked examples and the home exercises, graded from easy to harder within each group. Exercises 6.2.1–6.2.3 are about lossy media and the loss tangent, Exercises 6.2.4–6.2.5 about good conductors and the skin effect, Exercises 6.2.6–6.2.8 about plasmas and the group velocity, and Exercises 6.2.9–6.2.13 come from the exercise lecture and mix all three. They use only the equations listed at the head of this subsection, together with and , .
Why ice defrosts slowly
#At ice (about ) has , liquid water (Worked example 6.2.1, ). (a) Find the loss tangent and the effective conductivity of ice and classify it. (b) Find , and, with the low-loss formula, and the power penetration depth of ice. (c) What fraction of the power entering a thick block is absorbed in one pass, for ice and for water (reflections neglected)? (d) Find of ice.
Polarisation loss acts as the conductivity . Ice is so nearly lossless that the low-loss formula is exact for all practical purposes, and the absorbed fraction in one pass is .
and : a very good low-loss dielectric.
With : ice , water .
, practically real.
Water absorbs times more strongly than ice. A frozen block therefore heats very slowly until a spot melts, after which that spot absorbs almost everything and runs away: the cooked edges of badly defrosted food. Defrost programmes use a low average power in pulses, so that heat can conduct from the melted spots into the ice.
cf. Worked example 6.2.1