Consolidation of Inorganic Precipitated Silica Gel

Colloidal gels are possible intermediates in the generation of highly porous particle systems. In the production process the gels are fragmented after their formation. These gel fragments compact to particles whose application-technological properties are determined by their size and porosity. In th...

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Main Authors: Matthias Kind, Hussein Sahabi
Format: Article
Language:English
Published: MDPI AG 2011-08-01
Series:Polymers
Subjects:
Online Access:http://www.mdpi.com/2073-4360/3/3/1423/
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spelling doaj-84af6fc9096f488496ec069509ebb8032020-11-24T22:15:27ZengMDPI AGPolymers2073-43602011-08-01331423143210.3390/polym3031423Consolidation of Inorganic Precipitated Silica GelMatthias KindHussein SahabiColloidal gels are possible intermediates in the generation of highly porous particle systems. In the production process the gels are fragmented after their formation. These gel fragments compact to particles whose application-technological properties are determined by their size and porosity. In the case of precipitated silica gels, this consolidation process depends on temperature and pH, among other parameters. It is shown that these dependencies can be characterized by oedometer measurements. Originally, the oedometer test (one-dimensional compression test) stemmed from soil mechanics. It has proven to be an interesting novel examination method for gels. Quantitative data of the time-dependent shrinkage of gel samples can be obtained. The consolidation of the gels shows a characteristic dependence on the above parameters.http://www.mdpi.com/2073-4360/3/3/1423/consolidationoedometerreorganizationshrinkagesilica gelsyneresis
collection DOAJ
language English
format Article
sources DOAJ
author Matthias Kind
Hussein Sahabi
spellingShingle Matthias Kind
Hussein Sahabi
Consolidation of Inorganic Precipitated Silica Gel
Polymers
consolidation
oedometer
reorganization
shrinkage
silica gel
syneresis
author_facet Matthias Kind
Hussein Sahabi
author_sort Matthias Kind
title Consolidation of Inorganic Precipitated Silica Gel
title_short Consolidation of Inorganic Precipitated Silica Gel
title_full Consolidation of Inorganic Precipitated Silica Gel
title_fullStr Consolidation of Inorganic Precipitated Silica Gel
title_full_unstemmed Consolidation of Inorganic Precipitated Silica Gel
title_sort consolidation of inorganic precipitated silica gel
publisher MDPI AG
series Polymers
issn 2073-4360
publishDate 2011-08-01
description Colloidal gels are possible intermediates in the generation of highly porous particle systems. In the production process the gels are fragmented after their formation. These gel fragments compact to particles whose application-technological properties are determined by their size and porosity. In the case of precipitated silica gels, this consolidation process depends on temperature and pH, among other parameters. It is shown that these dependencies can be characterized by oedometer measurements. Originally, the oedometer test (one-dimensional compression test) stemmed from soil mechanics. It has proven to be an interesting novel examination method for gels. Quantitative data of the time-dependent shrinkage of gel samples can be obtained. The consolidation of the gels shows a characteristic dependence on the above parameters.
topic consolidation
oedometer
reorganization
shrinkage
silica gel
syneresis
url http://www.mdpi.com/2073-4360/3/3/1423/
work_keys_str_mv AT matthiaskind consolidationofinorganicprecipitatedsilicagel
AT husseinsahabi consolidationofinorganicprecipitatedsilicagel
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