| Abstract: | 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. -from Authors |
| Genre: | Article |
| ProdID: | 70017688 |
| Citation Author: | Eberl, D. D.; Velde, B.; McCormick, T. |
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| Citation End Page: | 60 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Clay Minerals |
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| Citation Number Of Pages: | 12 |
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| Citation Search Results Text: | Synthesis of illite-smectite from smectite at earth surface temperatures and high pH; 1993; Article; Journal; Clay Minerals; Eberl, D. D.; Velde, B.; McCormick, T. |
| Citation Start Page: | 49 |
| Citation Volume: | 28 |
| Citation Year: | 1993 |
| Type: | citation/reference |
| Text: | Synthesis of illite-smectite from smectite at earth surface temperatures and high pH; 1993; Article; Journal; Clay Minerals; Eberl, D. D.; Velde, B.; McCormick, T. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DOCUMENT): | ftp://brrcrftp.cr.usgs.gov/pub/ddeberl/EberlPapers/ClayPetrology/IlliteSynLowT.pdf |
| Date Other: | Fri, 1 Jan 1993 00:00 -0600 |
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