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231223s2008 xx |||||o 00| ||eng c |
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|a 10.1021/la802112h
|2 doi
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|a pubmed25n0612.xml
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|a (DE-627)NLM183721225
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|a (NLM)18925764
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|a DE-627
|b ger
|c DE-627
|e rakwb
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|a eng
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| 100 |
1 |
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|a Zhao, Hongying
|e verfasserin
|4 aut
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| 245 |
1 |
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|a Probing surface charge potentials of clay basal planes and edges by direct force measurements
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|c 2008
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|a Text
|b txt
|2 rdacontent
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|a ƒaComputermedien
|b c
|2 rdamedia
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|a ƒa Online-Ressource
|b cr
|2 rdacarrier
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|a Date Completed 09.01.2009
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|a Date Revised 01.12.2018
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|a published: Print-Electronic
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|a Citation Status MEDLINE
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|a The dispersion and gelation of clay suspensions have major impact on a number of industries, such as ceramic and composite materials processing, paper making, cement production, and consumer product formulation. To fundamentally understand controlling mechanisms of clay dispersion and gelation, it is necessary to study anisotropic surface charge properties and colloidal interactions of clay particles. In this study, a colloidal probe technique was employed to study the interaction forces between a silica probe and clay basal plane/edge surfaces. A muscovite mica was used as a representative of 2:1 phyllosilicate clay minerals. The muscovite basal plane was prepared by cleavage, while the edge surface was obtained by a microtome cutting technique. Direct force measurements demonstrated the anisotropic surface charge properties of the basal plane and edge surface. For the basal plane, the long-range forces were monotonically repulsive within pH 6-10 and the measured forces were pH-independent, thereby confirming that clay basal planes have permanent surface charge from isomorphic substitution of lattice elements. The measured interaction forces were fitted well with the classical DLVO theory. The surface potentials of muscovite basal plane derived from the measured force profiles were in good agreement with those reported in the literature. In the case of edge surfaces, the measured forces were monotonically repulsive at pH 10, decreasing with pH, and changed to be attractive at pH 5.6, strongly suggesting that the charge on the clay edge surfaces is pH-dependent. The measured force profiles could not be reasonably fitted with the classical DLVO theory, even with very small surface potential values, unless the surface roughness was considered. The surface element integration (SEI) method was used to calculate the DLVO forces to account for the surface roughness. The surface potentials of the muscovite edges were derived by fitting the measured force profiles with the surface element integrated DLVO model. The point of zero charge of the muscovite edge surface was estimated to be pH 7-8
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|a Journal Article
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|a Research Support, Non-U.S. Gov't
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| 650 |
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7 |
|a Aluminum Silicates
|2 NLM
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| 650 |
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7 |
|a Colloids
|2 NLM
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| 650 |
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7 |
|a Hydroxyl Radical
|2 NLM
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| 650 |
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7 |
|a 3352-57-6
|2 NLM
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| 650 |
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|a Silicon Dioxide
|2 NLM
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| 650 |
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7 |
|a 7631-86-9
|2 NLM
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| 650 |
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7 |
|a Clay
|2 NLM
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| 650 |
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7 |
|a T1FAD4SS2M
|2 NLM
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| 650 |
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7 |
|a mica
|2 NLM
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| 650 |
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|a V8A1AW0880
|2 NLM
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| 700 |
1 |
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|a Bhattacharjee, Subir
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Chow, Ross
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Wallace, Dean
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Masliyah, Jacob H
|e verfasserin
|4 aut
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| 700 |
1 |
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|a Xu, Zhenghe
|e verfasserin
|4 aut
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| 773 |
0 |
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|i Enthalten in
|t Langmuir : the ACS journal of surfaces and colloids
|d 1985
|g 24(2008), 22 vom: 18. Nov., Seite 12899-910
|w (DE-627)NLM098181009
|x 1520-5827
|7 nnas
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| 773 |
1 |
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|g volume:24
|g year:2008
|g number:22
|g day:18
|g month:11
|g pages:12899-910
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| 856 |
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|u http://dx.doi.org/10.1021/la802112h
|3 Volltext
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|d 24
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|h 12899-910
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