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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Bibliographic Details
Main Author: Saelens, Elsa
Other Authors: Lyons, Berry
Format: Thesis
Language:English
Published: The Ohio State University 2017
Subjects:
Online Access:http://hdl.handle.net/1811/86983