Sulfur isotope distribution in solfatares, Yellowstone National Park
Science
By: R. Schoen and R. O. Rye
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Abstract
Sulfur isotope data on hydrogen sulfide, native sulfur, and sulfates from acid hot-spring areas at Yellowstone National Park suggest that hydrogen sulfide oxidizes to sulfur analogically, whereas sulfur undergoes biological oxidation to sulfuric acid. An exception occurs at Mammoth Hot Springs where hydrogen sulfide apparently undergoes biochemical oxidation to sulfur.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Sulfur isotope distribution in solfatares, Yellowstone National Park |
| Series title | Science |
| Volume | 170 |
| Issue | 3962 |
| Year Published | 1970 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 1082 |
| Last page | 1084 |
| Google Analytic Metrics | Metrics page |