Iron sulfide formation in young and rapidly-deposited permeable sands at the land-sea transition zone
Organic-poor, permeable quartz sands are often present at land-sea transition zones in coastal regions. Yet, the biogeochemical cycles of carbon, sulfur, and iron are not well studied here. The aim of this work was, therefore, to improve our understanding regarding the chemical processes in these pr...
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Published in | The Science of the total environment Vol. 649; pp. 264 - 283 |
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Main Authors | , , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
Netherlands
Elsevier B.V
01.02.2019
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Subjects | |
Online Access | Get full text |
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