2013
DOI: 10.1016/b978-0-08-098258-8.00028-6
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Clay Science

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Cited by 137 publications
(1 citation statement)
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“…The Vrm layer is composed of one Mg-O 4 (OH) 2 octahedral sheet sandwiched between two opposing silicon-oxygen tetrahedral sheets. The layer charge mainly arises from the substitution of Al 3+ for Si 4+ in tetrahedral sheet [14,22], which makes the higher layer charge density (0.6-0.9 eq./formula unit) than Mt (0.2-0.6 eq./formula unit) [14,23]. This unique structure characteristics signi cantly in uences several physicochemical properties of clay minerals, such as higher cation exchange capacity, better thermal stability and thermal expansion [19,24].…”
Section: Introductionmentioning
confidence: 99%
“…The Vrm layer is composed of one Mg-O 4 (OH) 2 octahedral sheet sandwiched between two opposing silicon-oxygen tetrahedral sheets. The layer charge mainly arises from the substitution of Al 3+ for Si 4+ in tetrahedral sheet [14,22], which makes the higher layer charge density (0.6-0.9 eq./formula unit) than Mt (0.2-0.6 eq./formula unit) [14,23]. This unique structure characteristics signi cantly in uences several physicochemical properties of clay minerals, such as higher cation exchange capacity, better thermal stability and thermal expansion [19,24].…”
Section: Introductionmentioning
confidence: 99%