WebThe Soil Agricultural Groundwater Banking Index was developed by the University of California, Davis to indicate areas where farms could best participate in active recharge efforts. Depending on how the GSA regulates a basin, participating in recharge programs may be incentivized with groundwater credits for future use of groundwater supplies. WebThis map is part of the Soil Agricultural Groundwater Banking Index, which identifies farmlands with the most potential to capture groundwater and help 1/4. recharge the aquifer.
Map identifies farmland with greatest potential for …
Web2. Welcome to the UC Davis Soil Resource Laboratory. Our research covers many aspects of soil science including: Soil genesis and morphology. Rangeland soils. Hydropedology. … WebGoals / Objectives Stage groundwater recharge pilot studies at selected sites within California's Central Valley in order to systematically examine the physical, water quality, institutional, infrastructural, economic and legal parameters at play in agricultural groundwater banking (ag-GB) programs. The goal here is to test the feasibility and … theory of game-based learning
Map IDs farmland with greatest potential for …
Webters. O’Geen et al. (2015) developed a soil suitability index that iden-tifies potential locations for groundwater banking (large-scale storage of water in aquifers for later use) on agricultural lands. It is known as the Soil Agricultural Groundwater Banking Index (SAGBI) and is based on WebApr 12, 2024 · In many regions and for billions of people in Asia, groundwater is an irreplaceable resource for livelihoods and agriculture. Adverse impacts of climate change on groundwater resources are expected, including changes in recharge rates, saline intrusion in coastal aquifers, and decreased long term groundwater storage. WebOct 22, 2015 · The Soil Agricultural Groundwater Banking Index provides site-specific information on millions of acres of California farmland based on previous research led by Toby O’Geen, a UC Cooperative Extension … theory of gel formation