Synthesis of illite-smectite from smectite at Earth surface temperatures and high pH
It is well known that illite-smectite can form from smectite at elevated temperatures in natural and experimental systems. However, the conversion of smectite to illite-smectite is also found in some natural systems that have never been heated. The present experiments show that illite layers can form from smectite by chemical reaction at 35° and 60°C at high solution pH. The rate of this reaction is accelerated by wetting and drying.
Citation Information
Publication Year | 1993 |
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Title | Synthesis of illite-smectite from smectite at Earth surface temperatures and high pH |
DOI | 10.1180/claymin.1993.028.1.06 |
Authors | D.D. Eberl, Bruce Velde, T. C. McCormick |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Clay Minerals |
Index ID | 70017688 |
Record Source | USGS Publications Warehouse |