| Abstract: | The nature and extent of the reactions of synthetic Fe-free saponite have been investigated under experimental hydrothermal conditions as a first step towards understanding saponite reactivity under relatively simple conditions. Saponite crystallizes from amorphous gel of ideal saponite composition within 7 days at 300o-550oC under P = 1 kbar. Reactions subsequent to this initial crystallization depend on reaction T and interlayer cations. Saponite is found to react hydrothermally, over a period of 200 days, at T down to 400oC, at least 150oC lower than previously reported, but showed no signs of reaction below 400oC. At 450oC, a mixture of talc/saponite and saponite/phlogopite clays forms from K-saponite via intracrystalline layer transformations, while above 450oC the initial K-saponite dissolves, with talc and phlogopite forming as discrete phases. After 200 days reactions at 400-450oC were not complete, so that given sufficient time to reach equilibrium, a lower hydrothermal stability limit for saponite is possible. Further study of the Fe-bearing saponite system will be required before experimental results can be applied to natural systems.-D.F.B. |
| Genre: | Article |
| ProdID: | 70012024 |
| Citation Author: | Whitney, G. |
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| Citation End Page: | 8 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Clays & Clay Minerals |
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| Citation Number Of Pages: | 8 |
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| Citation Search Results Text: | Hydrothermal reactivity of saponite.; 1983; Article; Journal; Clays & Clay Minerals; Whitney, G. |
| Citation Start Page: | 1 |
| Citation Volume: | 31 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Hydrothermal reactivity of saponite.; 1983; Article; Journal; Clays & Clay Minerals; Whitney, G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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