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ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

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Page 1: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 2: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 3: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 4: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 5: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

ADSORPTION ISOTHERMS

discontinuous jumps: layering

transitions

some layering transitions

coexistence pressure

monolayer condensation

bilayer condensation

Page 6: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

= 0.450.60

Page 7: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

two-phase region

liquid-vapour transition of monolayer

two-phase region

two-phase region

two-phase region

two-phase region

Page 8: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

at two-phase coexistence

Page 9: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 10: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 11: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

LVSLSV

LVSLSV

Page 12: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 13: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 14: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Y(s)Y(s) = Q(s)

Page 15: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

if there exists such that there is a wetting transition, this is of 2nd order

Y(s)

s

Page 16: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

COMPLETE WETTING

T=TW

COMPLETE WETTING

T>TW

PARTIAL WETTING

T<TW

PARTIAL WETTING

T<TW

Page 17: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

area under curve )()(2

)( 0022

VsVsVs

s

V

s

V

dYd

Page 18: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 19: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 20: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 21: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

contribution from hard interaction

contribution from attractive interaction

(with correlations = step function)

Page 22: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 23: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 24: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 25: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 26: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation
Page 27: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

aba<s

a(TW )

abs<

Page 28: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Adsorption isotherms: Langmuir's model

Kr adsorbed on exfoliated graphite at T=77.3K

Vapour sector

Ns adatoms

s binding energy

N adsorption sites (N > Ns)

Distinguishable, non-interacting particles

The partition function is:

i

N

ss

EN

si eNNN

NeZ

)!(!

!

Using Stirling's approx., the free energy is:

)1log()1(loglog kTNNZkTF ssN

NN s / coverage

Page 29: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Chemical potential of the film:

1

log,,

kTdN

dF

N

Fs

TNTNf

ss

At low coverage

Film and bulk vapour are in equilibrium:

3

log1

logp

kTkTkTs

1

3*

se

kT

pp

ss eep ...1* linear for low (Henry's law)

This allows for an estimation of adsorption energies s by measuring the p-slope

Page 30: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Langmuir considers no mobility

Fowler and Guggenheim neglect xy localisation, consider full mobility (localisation only in z) and again no adatom interaction

N

i

is m

pNH

1

2

2

A = surface area

N

N

sAe

NZ

2!

1

The free energy is:

Again, calculating f and equating to of the (ideal) bulk gas:

Fowler and Guggenheim's model

2

logN

AekTNF s

snep 2*

ANn / (two-dimensional density)

Linear regime: has to do with absence of interactions

Es

Page 31: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Binder and Landau

Monte Carlo simulation of lattice-gas model with parameters for adsorption of H on Pd(100)

Limiting isotherm for

Corrections from 2D virial coefficients

T

Page 32: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Multilayer condensation in the liquid regimeellipsometric adsorption measurements of pentane on graphiteKruchten et al. (2005)

two-phase regions

2D critical points

Page 33: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Full phase diagram of a monolayerPeriodic quasi-2D solid

Commensurate or incommensurate?

Page 34: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Ar/graphite (Migone et al. (1984)

incommensurate solid

Page 35: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

commensurate monolayer incommensurate monolayer

two length scales:• lattice parameter of graphite• adatom diameter

three energy scales:• adsorption energy• adatom interaction• kT (entropy)

(also called floating phase)º3033

Kr/graphite

Page 36: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Kr/graphite

Specht et al. (1984)

Page 37: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Two-dimensional crystals

Absence of long-range order in 2D (Peierls, '30)

There is no true long-range order in 2D at T>0 due to excitation of long wave-length phonons with kT

sksk

kTn

,,

population of phonons with frequency

sk ,

),( sk

mode with force constant2

,, skskmf

kTkT

nxfsk

sksksksksk

,

,,,

2

,,2

1

22

,

,

2

skm

kTx

sk

The total mean displacement is

2

1

22 )(

g

dm

kTx

1a

1L

Page 38: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Using the Debye approximation for the density of states:

D

Dg

2,

3,)(

2

The mean square displacement when L goes to infinity is

Therefore, the periodic crystal structure vanishes in the thermodynamic limit

However, the divergence in <x2> is weak: in order to have , L has to be astronomical!

Da

LDLag

dm

kTx

2log

3,const)(11

22

2

1

22 ax

This is for the harmonic solid; there are more general proofs though

Page 39: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

XY model and Kosterlitz-Thouless (KT)

jiji JssJ cos

Freely-rotating 2D spins

The ground state is a perfectly ordered arrangement of spins

But: there is no ordered state (long-range order) for T>0

Consider a spin-wave excitation:

The energy is:

DLL

DLL

DLL

3in )/2(

2in )/2(

1in )/2(

3

2

grows without limit: ordered state robust w.r.t. T

goes to a constant: spin wave stable and no ordered state

limiting case (in fact NO)

Page 40: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Even though there is no long-range order, there may exist quasi-long-range order

No true long-range order: exponentially decaying correlations

• True long-range order: correlation function goes to a constant

• Quasi-long-range order(QLRO): algebraically decaying correlations

QLRO corresponds to a critical phase

Not all 2D models have QLRO:

• 2D Ising model has true long-range order (order parameter n=1)

• XY model superfluid films, thin superconductors, 2D crystals (order parameter n=2) only have QLRO

Spin excitations in the XY model can be discussed in terms of vortices (elementary excitations), which destroy long-range order

Page 41: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

vortex

topological charge = +1

antivortex

topological charge = -1

Page 42: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

We calculate the free energy of a vortex

The contribution from a ring a spins situated a distance r from the vortex centre is

r

Jr

J 22

2,1

2

2

rr

The total energy is

a

LJ

r

JdrE

L

a

v log lattice

parameterThe free energy is

a

LkTJ

a

LkT

a

LJTSEF vvv log2loglog

2

the vortex centre can be located at (L/a)2 different sites

Page 43: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

When Fv = 0 vortex will proliferate: ...571.12

J

kTc

Vortices interact as

a

rvKv ij

ji logVortices of same vorticity attract each other

Vortices of different vorticity repel each other

But one has to also consider bound vortex pairs

-1 +1

They do not disrupt order at long distances

Easy to excite

Screen vortex interactions

Page 44: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

KT theory: renormalisation-group treatment of screening effects

Confirmed experimentally for 2D supefluids and superconductor films. Also for XY model (by computer simulation)

Predictions:

• For T>Tc there is a disordered phase, with free vortices and free bound vortex pairs

• For T<Tc there is QLRO (bound vortex pairs)

• For T=Tc there is a continuous phase transition

K renormalises to a universal limiting value and then drops to zero

/ijrji ess cTTfor

)(Tji rss cTTfor

4

1

Page 45: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

The KT theory can be generalised for solids: KTHNY theory

There is a substrate. Also, there are two types of order:

• Positional order: correlations between atomic positions

Characterised e.g. by

• Bond-orientational order: correlations between directions of relative vectors between neighbouring atoms w.r.t. fixed crystallographic axis:

Two-dimensional melting

'rrg

)'()(66 ' rrierrg

Page 46: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

The analogue of a vortex is a a disclination

A disclination disrupts long-range positional order, but not the bond-orientational order

In a crystal disclinations are bound in pairs, which are dislocations,and which restore (quasi-) long-range positional order

Page 47: ADSORPTION ISOTHERMS discontinuous jumps: layering transitions some layering transitions coexistence pressure monolayer condensation bilayer condensation

Burgers vector

Dislocations

incr

easi

ng T