Role of Microbes in the Smectite-to-Illite Reaction
Science
By: J. Kim, H. Dong, J. Seabaugh, Steven W. Newell, and D. D. Eberl
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Abstract
Temperature, pressure, and time have been thought to control the smectiteto-illite (S-I) reaction, an important diagenetic process used for petroleum exploration. We demonstrated that microorganisms can promote the S-I reaction by dissolving smectite through reduction of structural FE(III) at room temperature and 1 atmosphere within 14 days. This reaction typically requires conditions of 300?? to 350??C, 100 megapascals, and 4 to 5 months in the absence of microbial activity. These results challenge the conventional concept of the S-I reaction and of reaction kinetic models.
Suggested Citation
Kim, J., Dong, H., Seabaugh, J., Newell, S.W., Eberl, D.D., 2004, Role of Microbes in the Smectite-to-Illite Reaction: Science, v. 303, no. 5659, p. 830-832, https://doi.org/10.1126/science.1093245.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Role of Microbes in the Smectite-to-Illite Reaction |
| Series title | Science |
| DOI | 10.1126/science.1093245 |
| Volume | 303 |
| Issue | 5659 |
| Year Published | 2004 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 830 |
| Last page | 832 |