Free Energy and Phase & Chemical Equilibria Flashcards
How do you derive the equation where du can be used to determine spontaneity of a reaction? Why is this not the most helpful?
ds>=dq/T
dq<=TdS
du= dq + dw
du <= TdS -Pex dV (from inequality above)
if constant S and V
du<=0 to be spontaneous, or =0 at equilibrium
Hard to maintain a constant entropy in a lab
What is the equation for Helmholtz free energy? Derive how the condition for equilibrium can obtained
A= u- TS
dA=du - TdS - SdT
dA<= TdS -P ex dV - TdS -SdT
dA<= -Pex dV - SdT
for a process at constant V and T
dA<= 0, at equilibrium=0
What is the equation for Gibbs free energy? Show how it can be used for a reaction at equilibrium?
G= A + pV
dG= dA + pdV + Vdp
dG<= -Pex dV - sdT + pdV + Vdp
at mechanical equilibrium where p=p ex
dG<= Vdp - sdT
for a process at constant p and t, dG<0
and dG=0 at equilibrium
e.g phase transitions, chemical reactions…
How can the Gibbs free energy incorporate enthalpy?
G= A + pV
G= U - TS + pV
G= U + pV - TS
G= H - TS
How can a systems ability to do non pV work be used within the free energy equations? What is the maximum available work of a system?
dw= -P ex dV + dwe, other work
dG<= dwe or equal at equilibrium
The maximum work from a process at constant T and P is equal to the decrease gibbs free energy
What are the terms involved in the fundamental equations?
They show how the 4 energy state functions, U, H, A, G, vary with P, V, S, and T
Can all be derived from definitions of the the energy state functions, and using the first and second law and pv work
How can the fundamental equation for H be derived? and A?
H= U + pV
dH= du + pdV + Vdp
dH= TdS - pdV + pdV + Vdp
dH= TdS + Vdp
A= u -TS
dA= du - Tds - SdT
dA= TdS- pdV - TdS - SdT
dA= pdV - SdT
Why can we remove the inequality when deriving the fundamental equations but not for spontaneity arguements?
Replacing du rev with du
As valid for changes between equilibrium states
How can the maxwell relations be derived?
Start with any fundamental equation
e.g dH= TdS + Vdp
implies H= H(S, p )
dH= (∂H/∂S)p dS + (∂H/∂p)s dP
implies (∂H/∂S)p = T and (∂H/∂p)s = V
and as ∂²H / ∂s∂p = ∂²H / ∂p∂s
so taking the derivative with respect to p for t as already done for s
(∂T/∂P)s = (∂V/∂s)p
How do you derive the Gibbs-Helmholtz equation?
G= H -TS
-S= (G-H) / T
From the maxwell equations,
-S=(∂G/∂T)p
(∂G/∂T)p - G/T= -H/T from subbing in and rearranging
but if we take G/T and differentiate implicitly with respect to T, using the product rule
= 1/T (∂G/∂T)p - G/T²
=1/T ((∂G/∂T)p - G/T)
which is 1/T a factor of -H/T
so
∂/∂T (G/T) = - H / T²
How do you derive the van’t Hoft equation from the Gibbs Helmholtz?
ΔrG⦵ = -RTlnkp
ΔrG/T⦵=-Rlnkp
∂/∂T (ΔrG/T⦵) = - ΔH / T²
∂/∂T (Rlnkp) = ∂/∂T (ΔrG/T⦵)
∂/∂T (lnkp) = - ΔH / RT²
How do you derive an equation to show how G varies with pressure for ideal gases and solids?
dG= Vdp - SdT
using the maxwell relation, (∂G/∂p)T= V
moving the p over and integrate
G2-G1= ∫ v dp
of a perfect gas, using v= nrt/p
G2-G1= nRTln(p2/p1)
using p1=1 bar
G2- G⦵=nRTln(p2/p⦵)
G2= G⦵ + nRTln(p2/p⦵)
for solids
G2-G1=v ∫ dp, as V independent of p
G2= G⦵ + V⦵(p-p⦵)
How can the idea of isothermal compressibility used for an equation of how G of solids varies with pressure?
graph lnV against p
slope=-k = (∂lnV/∂p)T= -1/v (∂V/∂p)T
rearrange for V
then same G integral as before, replace V with -1/k (∂V/∂p)T
G2-G1= (v2-v1) / k
-k = (∂lnV/∂p)T, rearrange for v2 in terms of v and e
end up with
G2= G⦵ + V/k(1-e^-k(p2-p⦵)
and as k approaches 0,
G2= G⦵ + v⦵(p2-p⦵)
What are the conditions for phase equilibrium and how have these been derived?
Suppose an equilibrium between a and b, where dn moles of a is converted to b, constant p,t
dG= G(b) - G (a) dn
at equilibrium dG=0
so G(b) = G(a)
can be 2 or 3 states. but 3 states have isolated points in the p,t plane
What does the p/t graph for water look like?
Y=mx line from origin between s and g
almost backwards line from triple point between solid and liquid
almost quadratic from triple point up ish between liquid and gas