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

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4 Results and discussion<br />

Raman Intensity<br />

752<br />

647<br />

579<br />

800 600 400<br />

Wavenumber/cm -1<br />

104<br />

419<br />

432<br />

450<br />

380<br />

600ºC<br />

500ºC<br />

Figure 71 Raman spectra of the Ti0.5Zr0.5O2 membranes calc<strong>in</strong>ed at 500ºC (green) and at 600ºC (blue)<br />

us<strong>in</strong>g the excitation of 514.5 nm, 20.6 mW.<br />

4.3.3.3 Am<strong>in</strong>e approach - Organic content <strong>in</strong> membrane layers<br />

The effective pore size <strong>in</strong> the layers can be determ<strong>in</strong>ed by an amorphous film around the<br />

nanocrystals or <strong>in</strong> comb<strong>in</strong>ation with the presence of organic residues orig<strong>in</strong>at<strong>in</strong>g from the<br />

am<strong>in</strong>es. The latter hypothesis was put <strong>for</strong>ward by Duke et al. 94 <strong>for</strong> carbon rema<strong>in</strong><strong>in</strong>gs<br />

and by Xomeritakis et al. 140 <strong>for</strong> am<strong>in</strong>e groups <strong>in</strong> microporous silica membranes.<br />

The carbon content at the outer surface of the membrane layers as determ<strong>in</strong>ed by XPS<br />

decreases with calc<strong>in</strong>ation temperature and is slightly higher than the carbon content of<br />

the bulk material as determ<strong>in</strong>ed by ICP (Figure 72). However, sputter<strong>in</strong>g the surface with<br />

argon <strong>for</strong> 2 m<strong>in</strong>utes reduces the carbon content to comparable values. This suggests that<br />

the observed high carbon concentrations orig<strong>in</strong>ate significantly from atmospheric<br />

contam<strong>in</strong>ation. Strik<strong>in</strong>g is the agreement between the carbon content trend <strong>in</strong> the powders<br />

and the layer with <strong>in</strong>creas<strong>in</strong>g ZrO2 <strong>in</strong> the sample. Both bulk material and membrane layer<br />

show an <strong>in</strong>crease <strong>in</strong> carbon content with an <strong>in</strong>creas<strong>in</strong>g ZrO2 content. This can be<br />

expla<strong>in</strong>ed by the slightly higher reactivity of the titanium precursor compared to that of<br />

the zirconium precursor result<strong>in</strong>g <strong>in</strong> stronger organic-<strong>in</strong>organic bonds.

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