SURFACE-PROPERTIES AND CLAY MINERALOGY OF HYDRATED HALLOYSITIC SOIL CLAYS .1. EXISTENCE OF INTERLAYER K+ SPECIFIC SITES

被引：25

作者：

DELVAUX, B

HERBILLON, AJ

DUFEY, JE

VIELVOYE, L

机构：

[1] UNIV NANCY 1,CNRS,UP6831,CTR PEDOL BIOL,BP 5,F-54501 VANDOEUVR NANCY,FRANCE

[2] CATHOLIC UNIV LOUVAIN,MUSEE ROYAL AFRIQUE CENT,UNITE SCI SOL,B-1348 LOUVAIN LA NEUVE,BELGIUM

[3] CATHOLIC UNIV LOUVAIN,MUSEE ROYAL AFRIQUE CENT,SECT PHYS CHIM MINERAL,B-1348 LOUVAIN LA NEUVE,BELGIUM

来源：

CLAY MINERALS | 1990年 / 25卷 / 02期

关键词：

D O I：

10.1180/claymin.1990.025.2.01

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：

Six deferrated clay (<2 μm) samples from the major B horizons of pedons derived from basaltic pyroclasts (Western Cameroon) were selected. These soil clays represent the types of secondary constituents characteristic of different weathering stages in soils derived from such volcanic materials under humid tropical conditions. All the surface properties observed point to the presence of smectite units intimately associated with halloysite in these clays. The results further suggest that the layer charge of these smectite units differs in different samples. -from Authors

引用

页码：129 / 139

页数：11

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[Anonymous], 1968, CLAY MINER

[2]

BLAKEMORE LC, 1983, ICOMAND5 NZ SOIL BUR

[3]

CARTER D. L., 1965, SOIL SCI, V100, P356, DOI 10.1097/00010694-196511000-00011

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