THE PHYSICAL DIMENSIONS OF FUNDAMENTAL CLAY PARTICLES

被引:145
作者
NADEAU, PH
机构
关键词
D O I
10.1180/claymin.1985.020.4.06
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 ;
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页码:499 / 514
页数:16
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共 41 条
[1]   EFFECT OF EARLY NUCLEATION CONDITIONS ON SYNTHETIC MUSCOVITE POLYTYPISM AS SEEN BY HIGH-RESOLUTION TRANSMISSION ELECTRON-MICROSCOPY [J].
AMOURIC, M ;
BARONNET, A .
PHYSICS AND CHEMISTRY OF MINERALS, 1983, 9 (3-4) :146-159
[2]   GROWTH MECHANISM, POLYTYPISM AND POLYMORPHISM OF SYNTHETIC HYDROXYLATED MUSCOVITE [J].
BARONNET, A ;
AMOURIC, M ;
CHABOT, B .
JOURNAL OF CRYSTAL GROWTH, 1976, 32 (01) :37-59
[3]   CESIUM - A MEANS OF DETERMINING THE STRUCTURE OF SMECTITES [J].
BESSON, G ;
GLAESER, R ;
TCHOUBAR, C .
CLAY MINERALS, 1983, 18 (01) :11-19
[4]   WATER SORPTION ON CA-SATURATED CLAYS .1. MULTILAYER SORPTION AND MICROPOROSITY IN SOME ILLITES [J].
BRANSON, K ;
NEWMAN, ACD .
CLAY MINERALS, 1983, 18 (03) :277-287
[5]  
Brindley GW, 1980, CRYSTAL STRUCTURES C, P125, DOI DOI 10.1180/MONO-5
[6]  
Brown G., 1978, The Chemistry of Soil Constituents (Greenland, D.J.
[7]  
Hayes, M.H.B., Editors)., P29
[8]  
CONLEY RF, 1966, CLAYS CLAY MINERALS, V14, P317
[9]   STRUCTURE AND SWELLING OF FIBROUS AND GRANULAR SAPONITIC CLAY FROM ORROCK QUARRY, FIFE, SCOTLAND [J].
COWKING, A ;
WILSON, MJ ;
TAIT, JM ;
ROBERTSON, RHS .
CLAY MINERALS, 1983, 18 (01) :49-64
[10]  
Cross, 1979, GEOCHEMISTRY COLLOID