Kirsten Faulkner is a Hydrologist specializing in groundwater age at the California Water Science Center.
Kirsten Faulkner began her career with the USGS California Water Science Center in 2018 after completing her M.S. in Geology from California State University, Long Beach. Her research is primarily focused on groundwater age and environmental tracers. She uses groundwater age models to understand water quality across 3-dimensional space and time. This information can be used to evaluate availability and susceptibility of drinking water resources. Prior to her work with the USGS, Kirsten worked in investment and finance.
Professional Experience
Hydrologist, U.S. Geological Survey, California Water Science Center
Education and Certifications
M.S., Geology, California State University, Long Beach
B.S., Geology, California State University, Long Beach
Science and Products
Modeling the dynamic penetration depth of post-1950s water in unconfined aquifers using environmental tracers: Central Valley, California
Over a third of groundwater in USA public-supply aquifers is Anthropocene-age and susceptible to surface contamination
Critical aquifer overdraft accelerates degradation of groundwater quality in California’s Central Valley during drought
Effects of montane watershed development on vulnerability of domestic groundwater supply during drought
Data for assessing the penetration depth post-1950s water in the Central Valley aquifer system, California (July 2022)
Groundwater data and age information from samples collected in Minnesota
Dissolved Noble Gas Concentrations and Modeled Recharge Temperatures for Groundwater from Northern Sierra Nevada Foothills Shallow Aquifer Assessment Study Units, 2015-2017: Results from the California GAMA Priority Basin Project
Data for Groundwater Age in the Western Principal Aquifers, 2004-2018
Science and Products
- Publications
Modeling the dynamic penetration depth of post-1950s water in unconfined aquifers using environmental tracers: Central Valley, California
The penetration depth of post-1950s recharge (D-1950) in aquifers is a marker that is frequently used to identify groundwater that is susceptible to anthropogenic contamination. Here, we compute D-1950 values at wells, interpolate them in space, and project them across time to map the moving front of modern recharge in four dimensions in the Central Valley aquifer system, California, USA. TracersAuthorsKirsten Faulkner, Bryant Jurgens, Stefan Voss, Danielle Dupuy, Zeno LevyOver a third of groundwater in USA public-supply aquifers is Anthropocene-age and susceptible to surface contamination
The distribution of groundwater age is useful for evaluating the susceptibility and sustainability of groundwater resources. Here, we compute the aquifer-scale cumulative distribution function to characterize the age distribution for 21 Principal Aquifers that account for ~80% of public-supply pumping in the United States. The aquifer-scale cumulative distribution function for each Principal AquifAuthorsBryant Jurgens, Kirsten Faulkner, Peter B. McMahon, Andrew Hunt, Gerolamo C. Casile, Megan B. Young, Kenneth BelitzCritical aquifer overdraft accelerates degradation of groundwater quality in California’s Central Valley during drought
Drought-induced pumpage has precipitated dramatic groundwater-level declines in California’s Central Valley over the past 30 years, but the impacts of aquifer overdraft on water quality are poorly understood. This study coupled over 160,000 measurements of nitrate from ∼6,000 public-supply wells with a 30-year reconstruction of groundwater levels throughout the Central Valley to evaluate dynamic rAuthorsZeno Levy, Bryant Jurgens, Karen R. Burow, Stefan Voss, Kirsten Faulkner, Jose Alfredo Arroyo-Lopez, Miranda S. FramEffects of montane watershed development on vulnerability of domestic groundwater supply during drought
Climate change is expected to reduce recharge to montane aquifers in the western United States, but it is unclear how this will impact groundwater resources in watersheds where intensive surface-water development has disrupted the natural hydrologic regime. To better understand sources of recharge and associated vulnerabilities of groundwater supply in this setting, we made a detailed geochemicalAuthorsZeno Levy, Miranda S. Fram, Kirsten Faulkner, Charles N. Alpers, Evelyn M Soltero, Kimberly A. Taylor - Data
Data for assessing the penetration depth post-1950s water in the Central Valley aquifer system, California (July 2022)
This dataset provides groundwater ages estimates that were used in an assessment of the penetration depth of modern groundwater in the Central Valley aquifer system (CVAL). Groundwater ages were estimated by calibration of environmental tracers (tritium, tritiogenic helium-3, chlorofluorocarbons, sulfur hexafluoride, carbon-14 and radiogenic helium-4) to lumped parameter models (LPMs) for samplesGroundwater data and age information from samples collected in Minnesota
Groundwater age distributions and susceptibility to natural and anthropogenic contaminants were assessed for selected wells, streambed piezometers, and springs in southeastern Minnesota. The data provide information to understand how long it will take to observe groundwater quality improvements from best management practices implemented at land surface to reduce losses of nitrate (and other chemicDissolved Noble Gas Concentrations and Modeled Recharge Temperatures for Groundwater from Northern Sierra Nevada Foothills Shallow Aquifer Assessment Study Units, 2015-2017: Results from the California GAMA Priority Basin Project
This data release documents 155 sets of dissolved noble gas analyses (neon, argon, krypton, xenon) and 153 modeled recharge temperatures for groundwater sampled from domestic water supply wells and springs throughout the northern Sierra Nevada foothills as part of the California State Water Resources Control Board's Groundwater Ambient Monitoring and Assessment (GAMA) Program in 2015-2017. Data frData for Groundwater Age in the Western Principal Aquifers, 2004-2018
Groundwater age distribution and susceptibility to natural and anthropogenic contaminants were assessed for selected principal aquifers of the Western United States: the Central Valley aquifer system (CVAL), the Basin and Range basin-fill aquifers (BNRF), the Rio Grande aquifer system (RIOG), the High Plains aquifer (HPAQ), the Columbia Plateau basaltic-rock aquifers (CLPT), and the Colorado Plate