THE GEOCHEMISTRY OF MINOR CATIONS WITHIN ANTARCTICA STREAM WATER: DETERMINING THE ROLE OF THE HYPORHEIC ZONE
The McMurdo Dry Valleys, Antarctica, are a polar desert containing ephemeral streams driven by glacial meltwater that flow 4–12 weeks in the austral summer. These streams contain a shallow area of porous sediment known as the hyporheic zone where there is rock-water interaction and water can be temp...
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Format: | Thesis |
Language: | English |
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The Ohio State University
2017
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Online Access: | http://hdl.handle.net/1811/86983 |