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Description
Understanding how water infiltrates and recharges subsurface aquifers is important in
protecting groundwater resources. The water infiltration process, however, is very complex,
especially in karst areas where many surface karst features, such as sinkholes and sinking
streams, provide different pathways connecting surface water to groundwater. In this
project, we propose to use a novel electrical resistivity method to monitor water movement
in different types of surface karst features. Using a newly modified AGI SuperSting
resistivity meter, we will conduct in-situ 3D time-lapse electrical resistivity surveys to
accurately measure temporal changes of electrical resistivity beneath karst features. These
temporal changes in resistivity will allow us to analyze the infiltration rates of water into
the subsurface as well as detect fast and slow flows within these features in responding to
hydrologic events of varying magnitude and duration. We will conduct this study in the
Royal Spring groundwater basin which provides sources of drinking water for Georgetown.
The collected data will also be incorporated into a numerical modeling study to understand
hydrologic and morphologic processes in the groundwater basin.
Status | Finished |
---|---|
Effective start/end date | 6/18/19 → 12/31/21 |
Funding
- US Geological Survey
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Projects
- 1 Finished
-
104B State Water Resources Research Institute Program 2016 - 2021
Ormsbee, L., Atwood, D., D'Angelo, E., Erhardt, A., Evans, S., Ford, W., Fox, J., Parris, T., Unrine, J., Zhu, J., Pennell, K., Agouridis, C., Brion, G., Cagle, L., Edwards, D., Fryar, A., Lee, B., Matocha, C., Munshaw, G., Price, S., Salmeron Cortasa, M., Wang, Y., Wei, Y., Wendroth, O. & Yost, S.
3/1/16 → 12/31/21
Project: Research project