Reversibility of heat transfer

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Reversible heat exchange requires an infinitesimal temperature difference between the system and heat source at every step, allowing for gradual temperature increases from T1 to T2. However, each heat transfer results in a net increase in entropy, as the entropy decrease of the hotter reservoir is less than the increase in the cooler body. This leads to the conclusion that true reversibility is unattainable in nature, as it would necessitate an infinite amount of time. Despite this, the concept of reversibility remains valuable for approximating actual processes. Understanding these principles is essential for thermodynamic analysis and applications.
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In the case of reversible heat exchange which the cooler body rises in temperature from T1 to T2, it requires that the temperature difference between the system and the heat source must be infinitesimal in every step. Usually the model is like that: Give a heat reservoir of temperature slightly higher than T1, make a small amount of heat transfer, than the temperature of cold body rise a little bit. Then use another hotter reservoir and transfer another infinitesimal amount of heat, repeat the steps until the body is T2.

The problem is: In every step the entropy decrease of hotter reservoir is smaller than the entropy increase of the cooler body. There is a net increase in entropy of the system. Although the increase is close to zero, we have done infinite number of step in order to increase the temperature to T2. How can we ensure the overall increase in entropy is zero so that it is a reversible process?
 
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It is reversible only in the limit of dT = (T2-T1) → 0 .
There is no truly reversible process in nature, since such a process would take an infinite time.
Actual processes can at most be very close to reversible.
It is nevertheless a useful concept and it can even be useful as an approximation to actual processes.
 
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