Tracing the contribution from weathering to a glacial stream in Antarctica
In high latitude environments, silicon is supplied to river waters by both glacial and non-glacial chemical weathering. The signal of these two end-members is often obscured by biological uptake and/or groundwater input in the river catchment. McMurdo Dry Valleys, characterised by extensive permafro...
Main Authors: | , , , , , , , , |
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Other Authors: | |
Format: | Conference Object |
Language: | English |
Published: |
2019
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Subjects: | |
Online Access: | http://hdl.handle.net/2078.1/224240 |