Core 2: Entropy Flashcards
How does G change at constant temperature but changing pressure? How does this apply to solids/liquids and gases?
dG=Vdp
For solids and liquids, volume is effectivally constant so ΔG=VΔp (integration from above)
For gases, V changes with pressure so it is substituted using pV=nRT. This integrates to ΔG=nRTln(pf/pi)
How are Cp,m and CV,m related? What are their values for monoatomic and polyatomic gases? What are these values based on?
Cp,m=CV,m+R
Monoatomic: Cp,m=R5/2 CV,m=R3/2
Polyatomic: Cp,m>R5/2 CV,m>R3/2
They are based on the degrees of freedom of the gas.
What is the entropy change from a fusion reaction?
ΔfusS=ΔfusH(Tf)/Tf
What is the equation for change in G when the pressure and temperature change?
dG=Vdp-SdT
What is Trouton’s rule?
ΔvapS is approximately the same for all liquids, around 85 J K-1 mol-1
What is the Clapeyron equation for phase diagrams?
m=dp/dT=ΔtrsS/ΔtrsV=ΔtrsH/TΔtrsV
State the equation for S using the number of microstates
S=kBln(W)
What is the entropy change when a gas is heated between two temperatures?
What if the is only a very small change between these temperatures? Why does this equation work?
What assumption as been made?
ΔS=nCp,mln(Tf/Ti)
dS=nCp,mdT/T, qrev is being estimated to CpΔT
Cp,m is not dependant on temperature, this can be improved by taking Cp,m=a+bT2 +c/T2
How is the entropy change of the surroundings related to the entropy change of the system?
ΔSsurr=-ΔSsystem
ΔSsurr=-qrev/T
How can the absolute entropy of a gas be adapted when the pressure is changed from 1 bar?
How can this be adapted for real gases?
Using the equation ΔG=nRTln(pf/pi), pi is p⦵
The change of entropy can then be added to G⦵m to find the new Gm value at p.
Gm(p)=G⦵m+nRTln(p/p⦵)
The p term is changed to f=øp for real gases.
How does entropy change for a gas expanding isothermally at:
- Constant pressure
- Constant volume
- ΔS=nRln(Vf/Vi)
- ΔS=nRln(pi/pf)
What is the Clausius-Clapeyron equation for the liquid-gas phase boundary?
What does this integrate to? How is it useful?
d(lnp)/dT=ΔvapH/RT2
lnp=(ΔvapH/RT)+c but this is useful for finding vapour pressure at different temperatures.
What is the van’t Hoff isochore?
How can its alternate forms be used?
lnK=(ΔrH⦵/RT)+ΔrS⦵/R
This can be used to calculate K at different temperatures. It can also be used to find ΔrH⦵ and ΔrS⦵ from a graph of lnK and 1/T
What is the equation for ΔU?
What can work be broken down into?
When is ΔU=0
ΔU=q+w
w=-pΔV
For an isothermal process
What is K for evapouration or sublimation of water?
K=pH2O(g)/p⦵