An investigation of soil moisture associated with ephemeral streams, Wright Valley, Antarctica
Ephemeral streams in Wright Valley, Antarctica, are fed by glacial melt and flow for between four and ten weeks annually. Hyporheic zones develop concomitantly with ephemeral stream channels. These zones are areas of saturated or moistened soil, depending on their proximity to the stream. The hyporh...
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Other Authors: | , |
Format: | Thesis |
Language: | English |
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The University of Waikato
2019
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Online Access: | https://hdl.handle.net/10289/12866 |