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- 富田 克利
- 鹿児島大学理学部地学教室
書誌事項
- タイトル別名
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- Synthesis of a regularly interstratified mineral of mica/montmorillonite and its formation mechanism
- ウンモ モンモリロナイト キソクガタ コンゴウソウ コウブツ ノ ゴウセイ ト
この論文をさがす
抄録
There are many hypotheses on the formation mechanism of mixed-layer minerals. In this paper, a formation mechanism of rectorite-type mixed-layer mineral from mica was investigated on the basis of experimental results. Dehydroxylated sericites were transformed into a mica/montmorillonite mixed-layer mineral by various leaching methods with acid solutions, molten LiNO3, sodium tetraphenylboron, sodium cobaltinitrite, and solutions containing salts. By the above procedures, 2M type scricites were easily changed into a regularly interstratified mineral of mica/montmorillonite. A random mixed-layer mineral of mica/montmorillonite was formed from 1M sericite. In order to change the 2M sericitesinto a regularly interstratified mineral, they should be heated up to the temperatur range of dehydroxylation. The formation of a rectorite-type mixedlayer mineral from 2M sericite may be explained on the orientations of the (OH) bonds after release of the potassium ions.
収録刊行物
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- 鉱物学雜誌
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鉱物学雜誌 14 (Special1), 104-128, 1979
一般社団法人 日本鉱物科学会
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詳細情報 詳細情報について
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- CRID
- 1390001206526558336
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- NII論文ID
- 130003623472
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- NII書誌ID
- AN00084868
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- ISSN
- 18837018
- 04541146
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- NDL書誌ID
- 2044905
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可