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

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3 Experimental<br />

3.4 Characterisation <strong>for</strong> microporous materials and membranes<br />

3.4.1 <strong>Microporous</strong> material characterisation<br />

Particle size analysis of the sols was per<strong>for</strong>med by us<strong>in</strong>g dynamic light scatter<strong>in</strong>g (DLS)<br />

equipment (Horiba Nanoparticle Size Analyzer LB-550) and small angle X-ray<br />

scatter<strong>in</strong>g. Prior to analysis, the sols were filtered with a Schleicher & Schuell 800 nm<br />

membrane sieve.<br />

Small angle X-ray scatter<strong>in</strong>g<br />

SAXS studies 126 were per<strong>for</strong>med us<strong>in</strong>g a NANOSTAR camera (Bruker AXS), fitted with<br />

a rotat<strong>in</strong>g anode source, run at 40 kV and 40 mA and filtered to yield only CuKα with<br />

wavelength λ=1.540 Å. The collimation path consisted of 3 p<strong>in</strong>holes and the primary<br />

beam stop at about 1.05 m from the sample position was chosen at 2 mm <strong>in</strong> diameter to<br />

allow the smallest scatter<strong>in</strong>g vector q~0.006 Å -1 to be obta<strong>in</strong>ed. Scatter<strong>in</strong>g patterns <strong>in</strong><br />

2-dimensionals were collected on a Hi-Star Xenon-filled 1000·1000 wired grid area<br />

detector. Typical acquisition times <strong>for</strong> the dilute solutions, which were kept <strong>for</strong> 10 hours,<br />

<strong>for</strong> statistical reasons, <strong>in</strong> sealed quartz capillaries of 1.5 mm diameter <strong>in</strong> the evacuated<br />

sample chamber. Transmissions of the solutions were <strong>in</strong> the order of 40-50% from<br />

absorbance measurements us<strong>in</strong>g a glassy carbon standard which was <strong>in</strong>serted <strong>in</strong> the<br />

optical path between the sample and the detector. The spot size of the beam on the<br />

sample was 500 µm. All data was corrected <strong>for</strong> background scatter<strong>in</strong>g of the quartz after<br />

a radially averag<strong>in</strong>g process of the raw data to yield a usable scatter<strong>in</strong>g vector range<br />

0.008

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