SURFACE-PROPERTIES AND CLAY MINERALOGY OF HYDRATED HALLOYSITIC SOIL CLAYS .2. EVIDENCE FOR THE PRESENCE OF HALLOYSITE SMECTITE (H/SM) MIXED-LAYER CLAYS

被引：48

作者：

DELVAUX, B

HERBILLON, AJ

VIELVOYE, L

MESTDAGH, MM

机构：

[1] UNIV NANCY 1,CNRS,UP6831,CTR PEDOL BIOL,F-54501 VANDOEUVRE NANCY,FRANCE

[2] 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.1990.025.2.02

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 clays from volcanic ash soils at different stages of weathering differ in their relative halloysite content to kaolinite and several surface properties. The information obtained explains why these clays have high CEC and distinct affinities for K+. This study will help to clarify the controversy concerning the CEC and related surface properties attributed to hydrated halloysite. -from Authors

引用

页码：141 / 160

页数：20

共 70 条

[1]

ANGEL BR, 1974, CLAY MINER, V10, P247, DOI 10.1180/claymin.1974.010.4.03

[2]

[Anonymous], 1965, CLAY CLAY MINER, DOI DOI 10.1346/CCMN.1964.0130121

[3] SPHEROIDAL HALLOYSITE IN A GUATEMALAN SOIL [J].