H2O(s)⇌H2O(l)
At melting point of H2O at (273 K = T)
dG = VdP - SdT
At constant temperature
d(ΔG)=ΔV(dP)=(ρLM−ρSM)dP
ρL=DensityofLiq.H2O
ρS=Densityofice
d(ΔG)=M(ρL⋅ρSρS−ρL)dP
Integrating
ΔG=M(ρL⋅ρSρS−ρL)(P−1)
Pressure increased from 1 atm to P atm
ρS<ρL,P>1
ΔG is -ve, so melting in forward direction spontaneous.
Method 2 :
Ice⇌Water
On Increasing P : Molecule Come closer & density increasing; water is formed;
Ice → Water;
Since Sice<Swater
∵ProcessFromIcetowaterisspontaneous;
ΔG<0
In physical equilibrium, on increasing pressure, equilibrium shift toward more density side.