NS009
Mountain-Sourced Recharge Into Groundwater Systems: Insights Gained From Geophysics and Hydrogeochemistry
Mountain-Sourced Recharge Into Groundwater Systems: Insights Gained From Geophysics and Hydrogeochemistry
Session ID#: 73950
Session Description:
Groundwater recharge in mountain regions supports local alpine and subalpine hydrological processes and acts to replenish water in adjacent valley aquifers. Subsurface mountain hydrologic systems are not only limited to the thin mantle of soil, but also include weathering bedrock and glacial deposits that host movement of groundwater through faults, fractures, and in certain cases, through the rock matrix. Visualizing these flow paths and tracking volumes of snowmelt and/or rainfall partitioned to shallow storage, deep storage, or downgradient recharge is important for closing water budgets, water resources planning and management, and groundwater modeling. This session focuses on advancements in tracking mountain-sourced recharge in groundwater systems using either geophysical imaging, hydrogeochemical measurements - or a combination of methods â at scales ranging from hillslopes, to catchments, to mountain block recharge. We encourage submissions focused on both method development as well as new process understandings using remote sensing, in-situ observations, and modeling.
Co-Organized:
- H - Hydrology
Index Terms:
0740 Snowmelt [CRYOSPHERE]
0994 Instruments and techniques [EXPLORATION GEOPHYSICS]
1829 Groundwater hydrology [HYDROLOGY]
1835 Hydrogeophysics [HYDROLOGY]
Primary Convener: Andy Parsekian, University of Wyoming, Laramie, WY, United States
Conveners: Hoori Ajami, University of California Riverside, Riverside, CA, United States, Rosemary J Knight, Stanford Univ, Stanford, CA, United States and Laurie Huning, University of California, Irvine, Civil and Environmental Engineering, Irvine, CA, United States
Primary Liaison: Andy Parsekian, University of Wyoming, Laramie, WY, United States
See more of: Near Surface Geophysics
