Expansion behaviour of commercial vermiculites at 1000 °C

被引:61
作者
Marcos, C. [1 ]
Rodriguez, I.
机构
[1] Univ Oviedo, Dept Geol, E-33005 Oviedo, Asturias, Spain
关键词
Commercial vermiculites; Heating; Mossbauer spectra; X-RAY-DIFFRACTION; IRON OXIDATION-STATE; OF-SOUTH-AFRICA; MOSSBAUER-SPECTROSCOPY; TETRAHEDRAL FE-3+; INTERLAYER WATER; MONTMORILLONITE LAYERS; INTERSTRATIFIED PHASES; EXCHANGEABLE CATIONS; TRIOCTAHEDRAL MICAS;
D O I
10.1016/j.clay.2010.02.012
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
Commercial vermiculites from different places were studied in order to know the cause of their different behaviour after abrupt heating at 1000 C. Mossbauer spectroscopy provided Fe(2+) and Fe(3+) contents and allowed identification of both tetrahedral and octahedral iron. The Fe(2+) content was higher in type-2 vermiculites (with K(+)- or >1 and/or Na(+) and/or Ca(2+) with or without Mg(2+) as the principal interlayer cations) than in type-1 vermiculites (with Mg(2+) or Mg(2+) and K(+) (<1) as the principal interlayer cations). The higher iron content seemed to facilitate the fixing of potassium ions. This was responsible of the larger expansion after abrupt heating at 1000 degrees C for 1 min. (C) 2010 Elsevier B.V. All rights reserved.
引用
收藏
页码:492 / 498
页数:7
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