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The influence of mercury contact angle, surface tension, and retraction mechanism on the interpretation of mercury porosimetry data

Rigby, Sean P. and Edler, Karen J. LU orcid (2002) In Journal of Colloid and Interface Science 250(1). p.175-190
Abstract

The use of a semi-empirical alternative to the standard Washburn equation for the interpretation of raw mercury porosimetry data has been advocated. The alternative expression takes account of variations in both mercury contact angle and surface tension with pore size, for both advancing and retreating mercury meniscii. The semi-empirical equation presented was ultimately derived from electron microscopy data, obtained for controlled pore glasses by previous workers. It has been found that this equation is also suitable for the interpretation of raw data for sol-gel silica spheres. Interpretation of mercury porosimetry data using the alternative to the standard Washburn equation was found to give rise to pore sizes similar to those... (More)

The use of a semi-empirical alternative to the standard Washburn equation for the interpretation of raw mercury porosimetry data has been advocated. The alternative expression takes account of variations in both mercury contact angle and surface tension with pore size, for both advancing and retreating mercury meniscii. The semi-empirical equation presented was ultimately derived from electron microscopy data, obtained for controlled pore glasses by previous workers. It has been found that this equation is also suitable for the interpretation of raw data for sol-gel silica spheres. Interpretation of mercury porosimetry data using the alternative to the standard Washburn equation was found to give rise to pore sizes similar to those obtained from corresponding SAXS data. The interpretation of porosimetry data, for both whole and finely powdered silica spheres, using the alternative expression has demonstrated that the hysteresis and mercury entrapment observed for whole samples does not occur for fragmented samples. Therefore, for these materials, the structural hysteresis and overall level of mercury entrapment is caused by the macroscopic (>∼30 μm), and not the microscopic (<∼30 μm), properties of the porous medium. This finding suggested that mercury porosimetry may be used to obtain a statistical characterization of sample macroscopic structure similar to that obtained using MRI. In addition, from a comparison of the pore size distribution from porosimetry with that obtained using complementary nitrogen sorption data, it was found that, even in the absence of hysteresis and mercury entrapment, pore shielding effects were still present. This observation suggested that the mercury extrusion process does not occur by a piston-type retraction mechanism and, therefore, the usual method for the application of percolation concepts to mercury retraction is flawed.

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publishing date
type
Contribution to journal
publication status
published
keywords
Contact angle, Electron microscopy, Mercury porosimetry, Porous media, Retraction mechanism, SAXS, Surface tension
in
Journal of Colloid and Interface Science
volume
250
issue
1
pages
16 pages
publisher
Elsevier
external identifiers
  • scopus:0036351230
ISSN
0021-9797
DOI
10.1006/jcis.2002.8286
language
English
LU publication?
no
id
f2448485-7d50-4959-a6a9-f36237401dcc
date added to LUP
2023-05-04 18:45:41
date last changed
2023-06-13 12:40:28
@article{f2448485-7d50-4959-a6a9-f36237401dcc,
  abstract     = {{<p>The use of a semi-empirical alternative to the standard Washburn equation for the interpretation of raw mercury porosimetry data has been advocated. The alternative expression takes account of variations in both mercury contact angle and surface tension with pore size, for both advancing and retreating mercury meniscii. The semi-empirical equation presented was ultimately derived from electron microscopy data, obtained for controlled pore glasses by previous workers. It has been found that this equation is also suitable for the interpretation of raw data for sol-gel silica spheres. Interpretation of mercury porosimetry data using the alternative to the standard Washburn equation was found to give rise to pore sizes similar to those obtained from corresponding SAXS data. The interpretation of porosimetry data, for both whole and finely powdered silica spheres, using the alternative expression has demonstrated that the hysteresis and mercury entrapment observed for whole samples does not occur for fragmented samples. Therefore, for these materials, the structural hysteresis and overall level of mercury entrapment is caused by the macroscopic (&gt;∼30 μm), and not the microscopic (&lt;∼30 μm), properties of the porous medium. This finding suggested that mercury porosimetry may be used to obtain a statistical characterization of sample macroscopic structure similar to that obtained using MRI. In addition, from a comparison of the pore size distribution from porosimetry with that obtained using complementary nitrogen sorption data, it was found that, even in the absence of hysteresis and mercury entrapment, pore shielding effects were still present. This observation suggested that the mercury extrusion process does not occur by a piston-type retraction mechanism and, therefore, the usual method for the application of percolation concepts to mercury retraction is flawed.</p>}},
  author       = {{Rigby, Sean P. and Edler, Karen J.}},
  issn         = {{0021-9797}},
  keywords     = {{Contact angle; Electron microscopy; Mercury porosimetry; Porous media; Retraction mechanism; SAXS; Surface tension}},
  language     = {{eng}},
  number       = {{1}},
  pages        = {{175--190}},
  publisher    = {{Elsevier}},
  series       = {{Journal of Colloid and Interface Science}},
  title        = {{The influence of mercury contact angle, surface tension, and retraction mechanism on the interpretation of mercury porosimetry data}},
  url          = {{http://dx.doi.org/10.1006/jcis.2002.8286}},
  doi          = {{10.1006/jcis.2002.8286}},
  volume       = {{250}},
  year         = {{2002}},
}