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Ch 20: The Micro/Macro Connection
Chapter 20, Problem 20

A 75 g ice cube at 0℃ is placed on a very large table at 20℃. You can assume that the temperature of the table does not change. As the ice cube melts and then comes to thermal equilibrium, what are the entropy changes of (a) the water, (b) the table, and (c) the universe?

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1
Calculate the heat transfer required to melt the ice cube. Use the latent heat of fusion for ice, which is approximately 334 J/g. Multiply this by the mass of the ice cube to find the total heat absorbed by the ice during melting.
Determine the change in entropy for the water as it melts. The change in entropy (\(\Delta S\)) due to heat transfer at a constant temperature can be calculated using the formula \(\Delta S = \frac{Q}{T}\), where \(Q\) is the heat absorbed and \(T\) is the absolute temperature in Kelvin.
Calculate the heat transfer from the table to the ice. Since the table remains at a constant temperature, the heat given off by the table is equal in magnitude but opposite in sign to the heat absorbed by the ice.
Determine the change in entropy for the table using the same entropy formula \(\Delta S = \frac{Q}{T}\). Remember to use the negative value of \(Q\) since the table is losing heat.
Calculate the total change in entropy for the universe, which is the sum of the entropy changes for the water and the table. This will give you an understanding of the second law of thermodynamics in action, as the total entropy of an isolated system never decreases.

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Key Concepts

Here are the essential concepts you must grasp in order to answer the question correctly.

Entropy

Entropy is a measure of the disorder or randomness in a system. In thermodynamics, it quantifies the amount of energy in a physical system that is not available to do work. When heat is transferred, such as when the ice cube melts, the entropy of the system changes, reflecting the distribution of energy among the particles. Understanding how entropy changes in different parts of a system is crucial for analyzing thermal processes.
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Thermal Equilibrium

Thermal equilibrium occurs when two objects in thermal contact no longer exchange heat, meaning they are at the same temperature. In this scenario, the ice cube and the table will reach thermal equilibrium when the ice has completely melted and the resulting water has warmed to the table's temperature. This concept is essential for understanding how energy transfers between the ice and the table affect their respective entropy changes.
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Heat Transfer

Heat transfer is the process by which thermal energy moves from one object or substance to another due to a temperature difference. In this case, heat flows from the warmer table to the colder ice cube, causing the ice to melt. The amount of heat transferred can be calculated using specific heat capacities and latent heat, which are important for determining the changes in entropy for both the water and the table during the melting process.
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