Entropy change of melting ice cube initially at -5°C

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SUMMARY

The entropy change of a 10g ice cube initially at -5°C when it completely melts is calculated to be 12.62 J/K. The calculation involves two stages: first, the entropy change as the ice warms from -5°C to 0°C, yielding 0.388 J/K, and second, the entropy change during the phase transition from ice to water, which contributes 12.23 J/K. The total entropy change is the sum of these two values, confirming that entropy, being a state function, can be added directly.

PREREQUISITES
  • Understanding of thermodynamic concepts, specifically entropy and state functions.
  • Familiarity with the specific heat capacity of ice (cice = 2.1 kJ/kg·K).
  • Knowledge of latent heat of fusion for ice (Lice-water = 3.34 x 105 J/kg).
  • Proficiency in calculus, particularly integration and natural logarithms.
NEXT STEPS
  • Study the principles of thermodynamics, focusing on entropy and state functions.
  • Learn about phase transitions and the associated thermodynamic equations.
  • Explore the application of the Clausius inequality in calculating entropy changes.
  • Investigate the relationship between temperature and entropy in various states of matter.
USEFUL FOR

Students in physics or chemistry, particularly those studying thermodynamics, as well as educators and professionals involved in energy transfer and phase change processes.

Flucky
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Homework Statement


Calculate the entropy change of an ice cube of mass 10g, at an initial temperature of -5°C, when it completely melts.

cice = 2.1 kJkg-1K-1
Lice-water = 3.34x105 Jkg-1


Homework Equations


dQ = mcdT
dS = \frac{dQ}{T}
ΔS = \frac{Q}{T}
Q = mL


The Attempt at a Solution


First I set the problem out in two stages:
a) the entropy change from the ice going from -5°C to 0°C (in order to melt)
b) the entropy change from the ice going to water

For a)
dQ = mcdT ---------(1)
dS = \frac{dQ}{T} ---------(2)

Putting (1) into (2):

dS = \frac{mcdT}{T}
ΔS = mc∫\frac{1}{T}dT
ΔS = mcln(Tf/Ti)

∴ΔS1 = (0.01)(2100)ln(\frac{273}{268}) = 0.388 JK-1


For b)
Q = mL = (0.01)(3.34x105) = 3340J

ΔS2 = \frac{Q}{T} = \frac{3340}{273} = 12.23 JK-1


∴ total ΔS = ΔS1 + ΔS2 = 0.388 + 12.23 = 12.62 JK-1

Am I right in simply adding the to changes of entropy together? Does ΔS work like that?

Cheers.
 
Physics news on Phys.org
Looks good, and the answer is yes, the entropies add. Entropy is a state function, like gravitational potential. If you went from 0 to 1m above ground you would have g x 1m change in potential. If you went from 1m to 2m there would be a further g x 1m change in potential. Giving total change in potential = g x 2m.
 
Great, thanks
 

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