Section 6: Phase Changes Flashcards
(32 cards)
an equation of state f(P,V,T)=0 yields
a 3D surface of equilibrium states
projections onto 2D graphs
PV graph - isotherm
PT graph - isochores
VT graph - isobars
moving between two states on the 2D plots still
involves changes in the 3rd parameter
phase changes produce
abrupt gradient changes on the PVT-surface
1st order phase changes
melting and boiling point
accompanied by a change in specific volume
PVT-surfaces have regions of
single-phase and regions of phase coexistence bounded by saturation lines
the saturation lines for liquid and vapour meet at
the critical point
for T>Tc
no condensation into a liquid is possible with increasing pressure
for T<Tc
an increase in pressure can cause a change of state
for T>Tc, gases and liquids are
indistinct
natural choice of thermodynamic potential to analyse phase equilibria
gibbs free energy
for two phases Gtot=
M1g1+M2g2
at equilibrium dGtot=
g1dM1+g2dM2=0 as dgi=0
both dG and di=0
mass conservation for a closed system gives dMtot=dm1+dm2=0
yields g1=g2
at equilibrium, the specific gibbs free energies are
equal
can be extended for more than two phases
eg at triple point gsolid=gliquid=gvapour
adding the restriction of the phase equilibrium leaves
one degree of freedom along the a line on the PT plot
gradient of this phase boundary is (dP/dT)v
for specific quantities the differential form of the Gibbs free energy is given by
dg=dP/ρ -sdT
the change in entropy at the phase transition can be related to
a latent heat
since delta Q = T delta S = mL
this leads to the Clausius-Clapeyron equation for first order phase changes
clausius-clapeyron equation is also useful as a
directly measurable proof of the 2nd law
cc eqn - the volumes V1 and V2 are the volumes
occupied by the same amount of matter in the two phases
cc eqn - depending on the units of L, m could be in
kilogram, moles or number of molecules
mL is measured in
joules
for first order changes there is a volume change associated with
the latent heat, L
most materials expand upon melting (except from eg water)
1st order - for an isobaric path from A to B across the melting line we have
(dg/dT)p=-s
d2g/dT2)p=-(ds/dT)p=-cp/T
but along this path s>0 and cp>0 so plot of g(T) has negative slope and curvature
at equilibrium the specific gibbs functions for solid and liquid are equal so we expect
the separate curves for liquid and solid to intersect at the phase boundary