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Inorganic Microporous Membranes for Gas Separation in Fossil Fuel ...

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2 Theoretical background<br />

wall <strong>in</strong>teraction is often referred as transition flow and is presented <strong>in</strong> equation (11). The<br />

first term <strong>in</strong> equation (11) orig<strong>in</strong>ates from the viscous flow and the second from the<br />

Knudsen diffusion equation. Both contributions can be identified from experimental data<br />

(12).<br />

N = −<br />

2 ( Ar P + Br)<br />

ε dP<br />

τ dz<br />

⎛ 1 ⎞ 2 8<br />

A = ⎜ ⎟ B =<br />

(12)<br />

⎝ 8ηRT<br />

⎠ 3 πMRT<br />

The α-Al2O3 support with γ-Al2O3 <strong>in</strong>termediate layer show gas transport predom<strong>in</strong>antly<br />

by Knudsen diffusion as reported by Benes et al. 91<br />

Micropore diffusion<br />

Several research groups 45,91,122,124 have studied the gas transport <strong>in</strong> microporous media<br />

such as the well-def<strong>in</strong>ed pore size MFI zeolite type membranes and amorphous sol-gel<br />

derived silica membranes. The transport mechanisms <strong>in</strong> microporous membranes are a<br />

function of the pore size, (condensable) properties of the transported species, activity of<br />

the pore wall, applied temperature, texture and microstructure of the microporous layer<br />

such as the connectivity of the pores, the porosity, the concentration and the connectivity<br />

of the defects, and the thickness of the layers.<br />

The s<strong>in</strong>gle gas flux <strong>in</strong> microporous membranes is based on diffusion where the gas<br />

molecule pore wall <strong>in</strong>teraction is more frequent than the gas molecules <strong>in</strong>teraction. The<br />

diffusion flux (N <strong>in</strong> mol/m 2 s) is determ<strong>in</strong>ed by the concentration of the gas and the<br />

mobility of the gas to hop from one void (hereafter referred as the pore) to the<br />

neighbour<strong>in</strong>g pore. This theory of irreversible thermodynamics, where the flux of s<strong>in</strong>gle<br />

gas ‘i' is proportional to the gradient <strong>in</strong> its chemical potential <strong>for</strong> microporous<br />

membranes, is thoroughly outl<strong>in</strong>ed by Benes. 122 The mass transport <strong>in</strong> microporous<br />

membranes follows the Henry regime at high temperatures with relatively low pressure<br />

and results <strong>in</strong> the follow<strong>in</strong>g equation (13):<br />

~<br />

D<br />

N = ∆<br />

L<br />

( T ) K(<br />

T )<br />

P<br />

∆P represents the pressure difference over the membrane. L is the thickness of the<br />

membrane layer. D ( T )<br />

~<br />

35<br />

(11)<br />

(13)<br />

is the concentration <strong>in</strong>dependent s<strong>in</strong>gle component chemical<br />

diffusion coefficient and is related to the mobility of the gas component. K(T) is the<br />

Henry coefficient. The diffusion flux is a thermally activated process described by an

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