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1

The corresponding text from Physical chemistry of surfaces Part 1 (CH server)

1) p. 41-52 (till Table 3.4, inclusive) 2) p. 52 (from 3.7.2) till p. 59

3. Dubinin-Radushkevich (DR) model

2

Pore filling

Adsorption potential of the vapour

Characteristic adsorption energy of the surface, Gaussian distribution

M. Polanyi

   

    

2

0

exp A

W E

W

 

 

  

 

 

 

 

2

2 0

2 p0

RT W exp

W ln

E p

(2)

3

plot

ln2(p0/p)

lnW

 

 

  

 

 

 

 

2

2 0

2 p0

RT W exp

W ln

E p plot

4

Interpretation of the fitted parameters

1. Derivation of specific surface area from monolayer capacity

2

A m A s

S n N a m

   g

Avogadro’s number Area occupied by a single adsorbent Monolayer capacity

1) (Most often) N2, 77 K

2) Initial part of the isotherm (p/p0=0.05-0.35 ) 3) nm from the linear plot of minimum 5 measured

points

4) as=0.162 nm2

CONDITIONS!!!!

(3)

5

Surface area of selected solids

Activated carbon 600-1400 m2/g

Silica 300- 600 m2/g

Catalysts 50- 300 m2/g

Dust (particle diameter 0.1 mm) 0.1-0.5 m2/g

 1 

s m m

p p

Kn n n

RT Kln  G

Langmuir model

BET model

(E Ea L)

C e

RT DR model

E characteristic adsorption energy

  G H T S 

6

- Can be measured directly (calorimetry) - Indirect info from the isotherms

2. The adsorption energy

(4)

 

   

  2

ln

s

mads

n

p H

T RT

lnp vs. 1/T

ns

p/p0

T1

T2

3. Isosteric heat of adsorption

Hmads

HmadsQizostf( )ns

7

The story told by the adsorption isotherm

1st layer completed p/p0<0,1:

micropore desorption

adsorption

Total pore volum a meso- and d<200 nm

macropores get filled

8

(5)

G

des

< G

ads

Adsorption hysteresis:

0

0

ln ln

  

  

ads ads

des des

G RT p p G RT p

p

9

p K

r =r +t Adsorption/desorption in mesopores::

adsorption and desorption

10

layer vs. meniscus

(6)

meniscus layer

11

The change of volume and surface area in a

cylindrical pore with a radius r semi-sphere wits a radius r Adsorption:on the surface

of a cylinder: r(r-dr)

Desorption:

GEOMETRY

p K 12

r =r +t

Kelvin equation

Saturation pressure in a cylindrical capillary of radius rK:

cos=1

POSSIBLE REASONS OF THE HYSTERESIS:

1. The different mechanism of ads/des

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13

Pore size distribution can be deduced with the Kelvin equation

Limits of the Kelvin equation:

H1 cylinder

H2 network, ink-bottle H3-H4 slit-like

14

2. Influence of the pore structure/shape (interactions, diffusion, network effect)

(8)

Example: ageing of an Alumina supported Ir catalyst

Sample SBET, m2/g Vtot, cm3/g

fresh 210 0,556

used 109 0,508

15

The range of Kelvin is limited

min1

r nm rmax25nm

 

0

ln 2 LV mLcos

K

p V

p r RTγ θ

What shall we do with the macropores?

Mercury porosimetry

Capillary attraction < 90 repulsion  > 90

 P hg(  f g) Work of wetting:

W=SLA-SGA=-ALGcos

SG = SL + LG cos  Volumetric work: W=VP

16

(9)

2 o P r    c s

Hg 480

N

m

és   140 

7.5 m atmospheric pressure 3.5 nm

P=2000 bar

1.5 nm

P=5000 bar

Washburn-equation

P excess pressure Commercial instruments:

Cylindrical pores:

17

Mercury porosimetry

How to measure macroporosity?

2 o P r    c s

Hg 480

N

m és =140 °

Washburn-equation P excess pressure -ALGcos=VP

For cylindrical pores:

18

7.5 m atmospheric pressure 3.5 nm

P=2000 bar

1.5 nm

P=5000 bar Commercial instruments:

Drawback:- environmental

- contamination of the sample

- damage of the sample

(10)

Porogram

Intrusion Extrusion

B: 500 Å C: 75 Å D: 29 Å

Porous Al2O3powder 19

20

Various methods for the determination of pore size distribution

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