X-RAY STUDIES OF REHYDRATION BEHAVIORS FOR MONTMORILLONITE
スポンサーリンク
概要
- 論文の詳細を見る
The rehydration properties for Ca-, Mg-, Na- and K-saturated montmorillonites after heating at various temperatures were examined and positions of interlayer cations for unheated, dehydrated and rehydrated specimens were investigated by means of one-dimensional Fourier analysis. Mg-saturated specimen dehydrated irreversibly after heating at 400℃, while rehydration was recognized after heating at 600℃ for Ca- and Na-saturated specimens and at 700℃ for K-saturated specimen. After heating at 600℃ for the Na-saturated specimen, the interlayer cations (Na^+) migrated into shallow part of the hexagonal holes, and the heated specimen restored its original hydrated configuration of interlayer region after water saturation. In the case of after heating at 800℃, the interlayer cations (Na^+) migrated into deep part of the holes, and drehydration did not occur even after water saturation. These results are due to the fixation of interlayer cations (Na^+) to the hexagonal holes of SiO_4 network after heating at 800℃, and it becomes difficult to extract these fixed cations from the holes. Therefore, the migrated positions of interlayer cations play an important role in its rehydration properties.
- 日本粘土学会の論文
著者
-
TOMITA KATSUTOSHI
Institute of Earth Sciences, Faculty of Science, Kagoshima University
-
Kawano Motoharu
Institute Of Earth Sciences Faculty Of Science Kagoshima University
-
Tomita Katsutoshi
Institute Of Earth Sciences Faculty Of Science Kagoshima University
関連論文
- QUANTITATIVE ESTIMATION AND DISTRIBUTION OF DETRITAL CLAY MINERALS IN THE SURFACE SEDIMENTS OF SOUTH YATSUSHIRO KAI, JAPAN
- CLAY MINERALS IN THE BOTTOM SEDIMENTS FROM KAGOSHIMA BAY, SOUTH KYUSHU, JAPAN
- X-RAY STUDIES OF REHYDRATION BEHAVIORS FOR MONTMORILLONITE
- CRYSTAL STRUCTURE OF DEHYDROXYLATED 2M_1 SERICITE AND ITS RELATIONSHIP WITH MIXED-LAYER MICA/SMECTITE
- AMMONIUM-BEARING DIOCTAHEDRAL 2M_1 MICA FROM AIRA DISTRICT, KAGOSHIMA PREFECTURE
- Clay mineralogical study on the upper 800m of 1,400m sediment core samples from Lake Biwa.