DEVELOPMENT OF AMMONIUM-SAPONITES FROM GELS WITH VARIABLE AMMONIUM CONCENTRATION AND WATER-CONTENT AT LOW-TEMPERATURES

被引:46
作者
KLOPROGGE, JT
BREUKELAAR, J
JANSEN, JBH
GEUS, JW
机构
[1] UNIV UTRECHT,INST EARTH SCI,DEPT GEOCHEM,3508 TA UTRECHT,NETHERLANDS
[2] SHELL INT RES MAATSCHAPPIJ BV,KONINKLIJKE SHELL LAB AMSTERDAM,1003 AA AMSTERDAM,NETHERLANDS
[3] UNIV UTRECHT,DEPT INORGAN CHEM,3508 TB UTRECHT,NETHERLANDS
关键词
CATION EXCHANGE CAPACITY; INFRARED SPECTROSCOPY; SAPONITE; SYNTHESIS; THERMAL ANALYSIS; TRANSMISSION ELECTRON MICROSCOPY; X-RAY POWDER DIFFRACTION;
D O I
10.1346/CCMN.1993.0410111
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
Ammonium-saponite is hydrothermally grown at temperatures below 300-degrees-C from a gel with an overall composition corresponding to (NH4)0.6Mg3Si3.4Al0.6O10(OH)2. The synthetic saponite and coexisting fluid have been characterized by means of X-rav powder diffraction, X-ray fluorescence. Induced Coupled Plasma-Atomic Emission Spectroscopy, thermogravimetric analysis, transmission electron microscopy, CEC determination using an ammonia selective electrode, and pH measurement. In the crystallization model developed, crystallization started with the growth of individual tetrahedral layers with an aluminum substitution not controlled by the Al(IV)/Al(VI) ratio in the gel and hydrothermal fluid, on which the octahedral Mg layers can grow. During the synthesis, individual sheets stacked to form thicker flakes while lateral growth also took place. The remaining Al(VI) partly replaced ammonium as the interlayer cation.
引用
收藏
页码:103 / 110
页数:8
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