Change in Entropy — Question 4

Section 20-2 · Physics pages 3258–3259

Question 4 Heating through a phase transition requires three entropy contributions A .100 kg sample starts as ice at 253 K and ends as liquid water at 293 K, at fixed pressure. Use melting temperature 273 K, ci = 2100 J/(kg K), cw = 4200 J/(kg K), and latent heat Lf = 334000 J/kg. Treat all values as constant in the stated ranges. Q added T melting Axes and labels specify the model; the sketch is schematic. (a) Calculate the entropy changes for warming ice, melting, and warming water. (b) Find total heat and total entropy change. Explain why the latent-heat term is divided by a fixed temperature rather than integrated over a temperature interval.
Show solutionHide solution
Question 4 - Solution Heating through a phase transition requires three entropy contributions Q added T melting (a) Method and calculation ∆Si = mci ln(273/253) ≈15.9773 J/K. ∆Sm = mLf/273 ≈122.344 J/K, ∆Sw = mcw ln(293/273) ≈29.6943 J/K. (b) Interpretation and further calculation ∆Stotal ≈168.016 J/K. Q = mci(20) + mLf + mcw(20) = 4200 + 33400 + 8400 = 46000 J. An equilibrium phase change at fixed pressure proceeds at its coexistence temperature, so ∫δQrev/T = Qlatent/Tm. Physical check The large entropy of melting reflects latent heat transfer without a temperature rise.

Question 4

Heating through a phase transition requires three entropy contributions

A .100 kg sample starts as ice at 253 K and ends as liquid water at 293 K, at fixed pressure. Use melting temperature 273 K, ci=2100c_i=2100 J/(kg K), cw=4200c_w=4200 J/(kg K), and latent heat Lf=334000L_f=334000 J/kg. Treat all values as constant in the stated ranges.

Diagram shown in the original SVG worksheet.

  1. Calculate the entropy changes for warming ice, melting, and warming water.

  2. Find total heat and total entropy change. Explain why the latent-heat term is divided by a fixed temperature rather than integrated over a temperature interval.

Question 4 - Solution

Heating through a phase transition requires three entropy contributions

Diagram shown in the original SVG worksheet.

(a) Method and calculation

ΔSi=mciln⁡(273/253)≈15.9773J/K.\Delta S_i=mc_i\ln(273/253)\approx15.9773\,\mathrm{J/K}.ΔSm=mLf/273≈122.344J/K,ΔSw=mcwln⁡(293/273)≈29.6943J/K.\Delta S_m=mL_f/273\approx122.344\,\mathrm{J/K},\quad\Delta S_w=mc_w\ln(293/273)\approx29.6943\,\mathrm{J/K}.

(b) Interpretation and further calculation

ΔStotal≈168.016J/K.\Delta S_{\mathrm{total}}\approx168.016\,\mathrm{J/K}.Q=mci(20)+mLf+mcw(20)=4200+33400+8400=46000J.Q=mc_i(20)+mL_f+mc_w(20)=4200+33400+8400=46000\,\mathrm J.An equilibrium phase change at fixed pressure proceeds at its coexistence temperature, so ∫δQrev/T=Qlatent/Tm\int\delta Q_{\mathrm{rev}}/T=Q_{\mathrm{latent}}/T_m.

Physical check

The large entropy of melting reflects latent heat transfer without a temperature rise.