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

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4 Results and discussion<br />

successful reproduced seeded DOH synthesis still <strong>in</strong>cludes significantly amount of SDA.<br />

This could have resulted <strong>in</strong> almost completely templated DOH. The chemical analysis<br />

confirm this expectation with a 5.5 wt% (0.22 mol%) carbon content. This amount,<br />

related to the theoretically determ<strong>in</strong>ed SiO2/ADA ratio of 34 <strong>in</strong> DOH, results <strong>in</strong> a ~75%<br />

cage occupancy. To summarise, it was not possible to synthesize DOH without the<br />

addition of (small amounts of) SDA by us<strong>in</strong>g secondary growth of seeds.<br />

Post treatments<br />

Several post treatments are compared <strong>in</strong> order to remove the organic template from the<br />

largest DOH [5 12 6 8 ] cages, namely 1) conventional calc<strong>in</strong>ations, 2) conventional<br />

calc<strong>in</strong>ations of DOH synthesised with traces of titanium to assist the burnout by catalytic<br />

oxidation, 3) reduc<strong>in</strong>g the crystal size to shorten the path length of the oxygen and<br />

combusted gasses by means of mechanical ball mill<strong>in</strong>g and 4) calc<strong>in</strong>ation <strong>in</strong> comb<strong>in</strong>ation<br />

with pressurised air.<br />

1) Conventional calc<strong>in</strong>ations<br />

The structure direct<strong>in</strong>g agent (SDA) occluded <strong>in</strong> DOH could not be removed completely<br />

by means of conventional calc<strong>in</strong>ation <strong>in</strong> air under ambient pressure and at temperatures<br />

between 700 and 900ºC. This is <strong>in</strong> l<strong>in</strong>e with other published results. 66,71-73 If all large<br />

cages are occupied by an ADA molecule the organic compounds amount to a total of<br />

6.9 wt.%. A complete SDA removal is observed at about 1400ºC, which is coupled with<br />

DOH structure breakdown (Figure 30). The XRD patterns of the ‘as-made’ and the<br />

calc<strong>in</strong>ed sample at 900ºC <strong>for</strong> 5 hours clearly show a broad diffraction around 22° 2Θ<br />

<strong>in</strong>dicat<strong>in</strong>g amorphous silica (Figure 31). This typical crystall<strong>in</strong>ity loss after calc<strong>in</strong>ation is<br />

coupled with an <strong>in</strong>crease <strong>in</strong> the <strong>in</strong>tensity <strong>for</strong> the low angle and is typical of empty<strong>in</strong>g<br />

zeolite cages. Several samples suffer significant crystall<strong>in</strong>ity loss after calc<strong>in</strong>ation.<br />

58

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