PARTICLE-PARTICLE AND PARTICLE-WATER INTERACTIONS IN AQUEOUS CLAY SUSPENSIONS. PART I. APPLICATION OF A MODIFIED ROBINSON EQUATION TO VISCOSITY DATA
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概要
- 論文の詳細を見る
The Robinson equation was modified and applied to the viscosity data of clay suspensions to which the Einstein equation was not applicable. The modified Robinson equation is : η_<rel>-1=k'S'V/(1-S'V) where η_<rel> is the relative viscosity, V the volume concentration of clay particles (cm^3/cm^3). S'a parameter for the ratio of the effective volume of clay particles to their actual volume and k'another parameter related to particle-particle interaction. The S'value increased from about 10 for spherical halloysite suspensions to allophane, kaolinite, montmorillonite and up to 1900 for fibrous imogolite suspensions. The k'value increased from about 1 for deflocculated suspensions to 20 for flocculated suspensions.
- 日本粘土学会の論文
著者
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Egashira Kazuhiko
Faculty of Agriculture, Kyushu University
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Egashira Kazuhiko
Faculty Of Agriculture
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WADA Koji
Faculty of Agriculture, Kyushu University
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NITAWAKI Yoshikazu
Faculty of Agriculture
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Wada Koji
Faculty Of Agriculture
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