Thermodynamics: T-S slope at constant volume

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SUMMARY

The discussion focuses on deriving the slope of an isochoric process in a temperature-entropy (T-S) diagram, establishing that the slope is T/Cv, where T represents temperature and Cv is the heat capacity at constant volume. The participants clarify that for isochoric processes, the equation dQ = Cv * dT holds true, as no work is done (dV=0) and energy changes occur solely through heat transfer. The relationship is confirmed by equating dQ = T * dS and manipulating the equations to show that dT/dS equals T/Cv, effectively demonstrating the derivation of the slope.

PREREQUISITES
  • Understanding of thermodynamic concepts, particularly isochoric processes.
  • Familiarity with the T-S diagram and its significance in thermodynamics.
  • Knowledge of heat capacity, specifically Cv (heat capacity at constant volume).
  • Basic calculus skills for manipulating differential equations.
NEXT STEPS
  • Study the derivation of the first law of thermodynamics in relation to isochoric processes.
  • Learn about the implications of the T-S diagram in various thermodynamic cycles.
  • Explore the relationship between heat capacity and temperature changes in different thermodynamic processes.
  • Investigate the differential energy equation and its applications in thermodynamic analysis.
USEFUL FOR

This discussion is beneficial for students and professionals in thermodynamics, particularly those studying heat transfer, energy systems, and anyone seeking to deepen their understanding of isochoric processes and T-S diagrams.

2DGamer
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1. Prove that the slope of an isochoric process in a T-S diagram is T/Cv where T is the temperature and Cv is the heat capacity at constant volume



2. dQ = T * dS (I understand this)
dQ = Cv * dT for isochoric processes (I don't understand this)




3. Since the two equations share dQ I set them equal to each other:
Cv * dT = T * dS
Then I just rewrote the equation as:
T/Cv = dT/dS
And dT/dS describes the slope of the line which is T/Cv
My main problem is that I don't understand why dQ = Cv*dT. The book just gave it to us, but I'm thinking that I need to be able to derive it or the problem is just too easy.

 
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2DGamer said:
dQ = Cv * dT for isochoric processes (I don't understand this)

For isochoric (constant-volume, dV=0) processes, no work is done (work being P\,dV), so any energy change dU in the system must be in the form of heat transfer q. Additionally, we can use the differential energy equation

dU(=q)=T\,dS-P\,dV=T\,dS=T\left(\frac{\partial S}{\partial T}\right)_V\,dT=C_V\,dT

which uses the definition of C_V. Does this make sense?
 

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