INFLUENCE OF ORGANOCATION STRUCTURE ON ADSORPTION OF MONOPYRIDINIUM AND OF BIPYRIDINIUM CATIONS BY EXPANDING LATTICE CLAY-MINERALS .2. ADSORPTION BY NA+-VERMICULITE

被引：8

作者：

HAYES, MHB ^{[1
]}

PICK, ME ^{[1
]}

TOMS, BA ^{[1
]}

机构：

[1] CENT ELECT GENERATING BOARD,BERKELEY NUCL LABS,BERKELEY GL13 9PB,GLOUCESTERSHIRE,ENGLAND

来源：

JOURNAL OF COLLOID AND INTERFACE SCIENCE | 1978年 / 65卷 / 02期

关键词：

D O I：

10.1016/0021-9797(78)90157-1

中图分类号：

O64 [物理化学（理论化学）、化学物理学];

学科分类号：

070304 ; 081704 ;

摘要：

引用

页码：266 / 275

页数：10

共 9 条

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[4] INFLUENCE OF ORGANOCATION STRUCTURE ON ADSORPTION OF MONOPYRIDINIUM AND OF BIPYRIDINIUM CATIONS BY EXPANDING LATTICE CLAY-MINERALS .1. ADSORPTION BY NA+-MONTMORILLONITE [J].

HAYES, MHB ;

PICK, ME ;

TOMS, BA .

JOURNAL OF COLLOID AND INTERFACE SCIENCE, 1978, 65 (02) :254-265

[5]

HAYES MHB, 1972, P INT CLAY C MADRID, P675

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[8] ESTIMATION OF SURFACE CHARGE DENSITY OF MICA AND VERMICULITE BY COMPETITIVE ADSORPTION OF DIQUAT2+ VS PARAQUAT2+ [J].

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SOIL SCIENCE SOCIETY OF AMERICA PROCEEDINGS, 1970, 34 (03) :527-&

[9] EFFECT OF CATION EXCHANGE CAPACITY ON RETENTION OF DIQUAT2+ AND PARAQUAT2+ BY 3-LAYER TYPE CLAY MINERALS .I. ADSORPTION AND RELEASE [J].

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