Section 6: Phase Changes Flashcards

(32 cards)

1
Q

an equation of state f(P,V,T)=0 yields

A

a 3D surface of equilibrium states

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2
Q

projections onto 2D graphs

A

PV graph - isotherm
PT graph - isochores
VT graph - isobars

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3
Q

moving between two states on the 2D plots still

A

involves changes in the 3rd parameter

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4
Q

phase changes produce

A

abrupt gradient changes on the PVT-surface

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5
Q

1st order phase changes

A

melting and boiling point

accompanied by a change in specific volume

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6
Q

PVT-surfaces have regions of

A

single-phase and regions of phase coexistence bounded by saturation lines

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7
Q

the saturation lines for liquid and vapour meet at

A

the critical point

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8
Q

for T>Tc

A

no condensation into a liquid is possible with increasing pressure

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9
Q

for T<Tc

A

an increase in pressure can cause a change of state

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10
Q

for T>Tc, gases and liquids are

A

indistinct

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11
Q

natural choice of thermodynamic potential to analyse phase equilibria

A

gibbs free energy

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12
Q

for two phases Gtot=

A

M1g1+M2g2

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13
Q

at equilibrium dGtot=

A

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

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14
Q

at equilibrium, the specific gibbs free energies are

A

equal

can be extended for more than two phases

eg at triple point gsolid=gliquid=gvapour

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15
Q

adding the restriction of the phase equilibrium leaves

A

one degree of freedom along the a line on the PT plot

gradient of this phase boundary is (dP/dT)v

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16
Q

for specific quantities the differential form of the Gibbs free energy is given by

A

dg=dP/ρ -sdT

17
Q

the change in entropy at the phase transition can be related to

A

a latent heat

since delta Q = T delta S = mL

this leads to the Clausius-Clapeyron equation for first order phase changes

18
Q

clausius-clapeyron equation is also useful as a

A

directly measurable proof of the 2nd law

19
Q

cc eqn - the volumes V1 and V2 are the volumes

A

occupied by the same amount of matter in the two phases

20
Q

cc eqn - depending on the units of L, m could be in

A

kilogram, moles or number of molecules

21
Q

mL is measured in

22
Q

for first order changes there is a volume change associated with

A

the latent heat, L

most materials expand upon melting (except from eg water)

23
Q

1st order - for an isobaric path from A to B across the melting line we have

A

(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

24
Q

at equilibrium the specific gibbs functions for solid and liquid are equal so we expect

A

the separate curves for liquid and solid to intersect at the phase boundary

25
the equilibrium phase has the lowest value for
the gibbs function the gradient of g therefore has to be discontinuous
26
gradient of g being discontinuous menas that the entropy
must be discontinuous across the phase boundary
27
all first order phase changes have a
discontinuous 1st derivative of the gibbs function g
28
the kinks in the gibbs functions at the transition is associated with the
latent heat for the phase transition
29
across second-order phase transitions, first order derivatives are
continuous S=-(dG/dT)p and V=(dG/dP)T so deltaS=deltaV=0 and no latent heat and no volume change
30
second order derivatives for second order phase transitions
discontinuous eg discontinuities in the bulk moduli, compressibilities and heat capacities
31
third order phase transitions also occur eg
in ferromagnetics or superfluids
32