Kim, J. (2004) Role of Microbes in the Smectite-to-Illite Reaction. Science, 303 (5659). 830-832 doi:10.1126/science.1093245

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	Not Yet Imported: Applied and Environmental Microbiology - journal-article : 10.1128/AEM.68.12.6256-6262.2002 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 5725
	Not Yet Imported: International Journal of Systematic Bacteriology - journal-article : 10.1099/00207713-45-3-441 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 35038
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	For example natural smectite ranges from 0.4 mmol of Fe 3+ /g for Wyoming Na-montmorillonite (Swy-1) to 0.5 mmol of Fe 3+ /g for Upton montmorillonite ∼1 mmol of Fe 3+ /g for Gulf Coast smectites 3.5 mmol of Fe 3+ /g for the ferruginous smectite (Swa-1) and 4.3 mmol of Fe 3+ /g for the smectite used in this study.
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	Not Yet Imported: Applied and Environmental Microbiology - journal-article : 10.1128/AEM.68.8.3759-3770.2002 If you would like this item imported into the Digital Library, please contact us quoting Journal ID 5725
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	We thank M. D. Richardson D. R. Peacor and J. W. Stucki for extensive comments and discussion. This work was partially supported by the Naval Research Laboratory (contribution no. 7430-03-04). Acknowledgment is made to the donors of the Petroleum Research Fund administered by the American Chemical Society for support (or support in part) of this research to H. D.

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