Flow-path changes in permafrost soils affect Fe-organic carbon interactions: evidence from silicon isotopes
Silicon isotope fractionation upon amorphous silica precipitation is sensitive to freeze-thaw cycles in arctic soils that are composed of carbon-rich permafrost (i.e. soil layer that remains frozen for at least two consecutive years) covered by an active layer (i.e. soil layer that thaws in summer i...
Main Authors: | , , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2024
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/287448 |