Entropy change in an isolated system

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In an isolated system where a solid at initial temperature To contacts a hotter reservoir at temperature T1, the entropy change of the universe is positive. This is because the positive entropy change of the solid, which gains heat, exceeds the negative entropy change of the reservoir, which loses heat at a higher temperature. The calculations for entropy changes are dS = dQ/To for the solid and dS = -dQ/T1 for the reservoir. The total change in entropy can be expressed as the sum of the individual changes, leading to a net increase in entropy. Thus, the process demonstrates the second law of thermodynamics, confirming that the total entropy of the universe increases.
indie452
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hi I am having a few conception problems with entropy

problem:
a solid with constant heat capacity and initial temp To, is brought in contact with hotter reservoir temp T1 and allowed to come into equilibrium. This is all isolated.

a) is the change in the entropy of the universe negative zero or positive thanks to the systems process. explain why
b) calculate entropy change to solid
c) calculate entropy change to reservoir

a) i would have thought that the entropy change of the universe is zero because entropy change is dQ/T and the change in Q for both systems is the same (for the solid its +ve and reservoir -ve)

b) dS = dQ/To
c) dS = -dQ/T1

is this right?
 
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indie452 said:
hi I am having a few conception problems with entropy

problem:
a solid with constant heat capacity and initial temp To, is brought in contact with hotter reservoir temp T1 and allowed to come into equilibrium. This is all isolated.

a) is the change in the entropy of the universe negative zero or positive thanks to the systems process. explain why
b) calculate entropy change to solid
c) calculate entropy change to reservoir

a) i would have thought that the entropy change of the universe is zero because entropy change is dQ/T and the change in Q for both systems is the same (for the solid its +ve and reservoir -ve)
The heat flow out of the reservoir is at the higher reservoir temperature.

The total heat flow out of the reservoir (negative) has to be equal in magnitude to the (positive) heat flow into the solid. But since the temperature of the solid is always less than that of the reservoir, the change in entropy of the reservoir (dS = dQ/T), which is negative, will have a smaller magnitude than the positive change in entropy of the solid. So the total change in entropy will be greater than 0.

b) dS = dQ/To
c) dS = -dQ/T1

is this right?
That is the initial differential change in entropy. The total change is:

\Delta S = \Delta S_{res} + \Delta S_{sol}

where:

(1) \Delta S_{res} = \int_{T_{ir}}^{T_{fr}} m_{res}C_{res}\frac{dT}{T} = m_{res}C_{res}\ln{\frac{T_{fr}}{T_{ir}}

and

(2) \Delta S_{sol} = \int_{T_{is}}^{T_{fs}} m_{sol}C_{sol}\frac{dT}{T} = m_{sol}C_{sol}\ln{\frac{T_{fs}}{T_{is}}AM
 
The book claims the answer is that all the magnitudes are the same because "the gravitational force on the penguin is the same". I'm having trouble understanding this. I thought the buoyant force was equal to the weight of the fluid displaced. Weight depends on mass which depends on density. Therefore, due to the differing densities the buoyant force will be different in each case? Is this incorrect?

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