Water residence time controls iron-organic carbon interactions in waters draining a sub-Arctic fen
Does iron (Fe) act to stabilise (e.g., via attachment to ferrihydrite) or degrade (e.g., via photo-degradation) organic carbon (OC) in Arctic Rivers? Characterising the interaction between Fe and OC in headwaters, prior to transport along the continuum, is key to answering this question. Here we ask...
Main Authors: | , , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2022
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/268695 |