Irreversibility of a Process: Finding ΔQ and ΔS of a Mass Dropped into the Sea

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Homework Help Overview

The discussion revolves around the irreversibility of a process involving a mass with heat capacity dropped into the sea, exploring the changes in heat (ΔQ) and entropy (ΔS) associated with this scenario.

Discussion Character

  • Exploratory, Assumption checking, Conceptual clarification

Approaches and Questions Raised

  • Participants discuss the relationship between heat transfer and work, questioning the nature of work in this context. They explore the entropy changes for both the mass and the sea, with some participants attempting to derive expressions for these changes.

Discussion Status

There is an ongoing exploration of the entropy changes for both the mass and the sea, with participants providing expressions and questioning assumptions about the system. Some guidance has been offered regarding the calculations of ΔQ and ΔS, but no consensus has been reached on the implications of these values.

Contextual Notes

Participants note the lack of information regarding the mass of the sea and its impact on the calculations. There is also a discussion about the implications of infinite mass and negligible temperature changes in the context of the problem.

Gregg
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Homework Statement



A mass m with heat capacity c at temperature T_1 is dropped into the sea at T_2.


What is the irreversibility of the process?

Homework Equations



I = T_0 (\Delta S + \Delta S_E )

I = W_{\text{rev}} - W

The Attempt at a Solution



Heat in is Q=mc\Delta T the temperature of the sea remains constant by the first law W=Q. What is the distinction between the work for a reversible process and the work?
 
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No work is involved. ΔW =0, ΔU = -Q for the mass and +Q for the sea.

U of the sea does change, albeit mightily little.

Write an expression for the entropy change of the mass and of the sea.

What constitutes the irreversibility calls for a verbal answer, plus reference to the line above.
 
Well since the mass of the sea is not given I assume that the change in internal energy is negligable. Made an error with work! Of course there is no work.

So the key is to find the entropy change of the sea and of the block.

\Delta s_{\text{sea}} = \frac{mc(T_2-T_1)}{T_2}

\Delta s_{\text{block}} = ?

is it log?
 
No, U of the sea goes up. It's an infinite mass all right, so an infinitely small rise in temperature, but ΔU and Q go up together & are finite. Where do you think the loss of Q from the mass goes? Of course, ΔT of the sea is essentially zero. Have to be careful with infinities and zeros.
 
Gregg said:
\Delta s_{\text{block}} = ?

is it log?
Yes. You have dS = dQ/T and dQ=mc dT. Put those together and integrate.
 
I = T_0(mc(\frac{T_0-T_1}{T_0})+mc \log(\frac{T_0}{T_1}))

T_1 > T_0. So, is \Delta S_{\text{sea}} < 0 ?

I know that mc \log (\frac{T_0}{T_1}) < 0
 
No, the sea absorbs heat, so its entropy increases.
 
Anyway, you got ΔQ and ΔS for the mass correct now. Although, simplify by writing ΔQ of mass = mc(T2 - T1).

So what do you think ΔQ of the sea is? And then ΔS of the sea?
 

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