Morphological Analysis of Physically Reconstructed Silica Monoliths with Submicrometer Macropores: Effect of Decreasing Domain Size on Structural Homogeneity.
Morphological Analysis of Physically Reconstructed Silica Monoliths with Submicrometer Macropores: Effect of Decreasing Domain Size on Structural Homogeneity.
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具有亚微米大孔的物理重建二氧化硅整体的形态分析:减小域尺寸对结构均匀性的影响
DOI:
10.1021/la5046018
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发表时间:
2015
期刊:
影响因子:
--
通讯作者:
U. Tallarek
中科院分区:
文献类型:
--
作者:
D. Stoeckel;C. Kübel;M. O. Loeh;B. M. Smarsly;U. Tallarek
Silica monoliths are increasingly used as fixed-bed supports in separation and catalysis because their bimodal pore space architecture combines excellent mass transport properties with a large surface area. To optimize their performance, a quantitative relationship between morphology and transport characteristics has to be established, and synthesis conditions that lead to a desired morphology optimized for a targeted application must be identified. However, the effects of specific synthesis parameters on the structural properties of silica monoliths are still poorly understood. An important question is how far the macropore and domain size can be reduced without compromising the structural homogeneity. We address this question with quantitative morphological data derived for a set of eight macroporous–mesoporous silica monoliths with an average macropore size (dmacro) of between 3.7 and 0.1 μm, prepared following an established route involving the sol–gel transition and phase separation. The macropore space of the silica monolith samples is reconstructed using focused ion beam scanning electron microscopy followed by a quantitative assessment of geometrical and topological properties based on chord length distributions (CLDs) and branch-node analysis of the pore network, respectively. We observe a significant increase in structural heterogeneity, indicated by a decrease in the parameterkderived from fitting ak-gamma function to the CLDs, whendmacroreaches the submicrometer range. The compromised structural homogeneity of silica monoliths with submicrometer macropores could possibly originate from early structural freezing during the competitive processes of sol–gel transition and phase separation. It is therefore questionable if the common approach of reducing the morphological features of silica monoliths into the submicrometer regime by changing the point of sol–gel transition can be successful. Alternative strategies and a better understanding of the involved competitive processes should be the focus of future research.
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DOI:
--
发表时间:
2002
期刊:
影响因子:
--
作者:
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通讯作者:
D. Lubda
DOI:
10.1021/la0613225
发表时间:
2006-11
期刊:
Langmuir : the ACS journal of surfaces and colloids
影响因子:
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通讯作者:
Yan Yao;K. Czymmek;R. Pazhianur;A. Lenhoff
影响因子:
3.1
作者:
S. Altmaier;K. Cabrera
通讯作者:
K. Cabrera
影响因子:
16.6
作者:
Karwacki, Lukasz;de Winter, D. A. Matthijs;Weckhuysen, Bert M.
通讯作者:
Weckhuysen, Bert M.
DOI:
10.1016/j.chroma.2013.08.087
发表时间:
2013
期刊:
Journal of chromatography. A
影响因子:
--
作者:
K. Hormann;U. Tallarek
通讯作者:
U. Tallarek