Groundwater dynamics after California drought
As part of California’s 2014 Sustainable Groundwater Management Act, Sacramento area groundwater basins were designated as a high priority for management under groundwater sustainability plans. Determining sustainable groundwater use is not possible without first quantifying groundwater extraction and recharge. This project will characterize groundwater recharge using groundwater age, recharge location, and recharge temperature. Results from the project will be compared to a similar study performed in pre-drought conditions to investigate changes in aquifer recharge, and to develop a groundwater flow model for the area. This information will be valuable for local water stakeholders working to create a groundwater sustainability plan.
Assistant Professor, Geology Department
California State University, Sacramento
Sacramento area groundwater basins have been designated high priority under the 2014 Sustainable Groundwater Management Act. This means that the basins are required to develop groundwater sustainability plans. Determining levels of sustainable groundwater use is not possible without first quantifying recharge to ensure that groundwater removed does not significantly exceed the amount added. This project aims to characterize the aquifers within east Sacramento following California’s historic five-year drought.
It is anticipated that the Lower American River is the primary recharge source for the aquifers. River flows have been exceptionally low due to the drought and groundwater pumping was accelerated to supplement the limited surface water availability. It is therefore hypothesized that groundwater recharge did not keep up with extraction, drawing flow from other areas of the aquifer and depleting the groundwater supply.
The project will involve sampling water from sixteen monitoring wells and from surface water bodies in potential areas of recharge. Tritium and dissolved noble gases will be analyzed to determine the recharge source location and seasonal timing, and describe the flow path of groundwater. Results will be used to develop a groundwater model in order to understand past flow and predict future aquifer behavior. Results will also be compared to similar analyses performed in pre-drought conditions, enabling investigation of changes in aquifer dynamics during California’s ongoing drought.
Results from this research could provide valuable insight into recharge mechanisms and groundwater dynamics for east Sacramento aquifers. Quantifying recharge mechanisms and rates will be critical for calculating sustainable groundwater yield as local groundwater sustainability agencies develop their groundwater sustainability plans.