Interpretive Reports

Quantifying Anthropogenic Contributions to Century-Scale Groundwater Salinity Changes, San Joaquin Valley, California, USA

Hansen, J.A., Jurgens, B., and Fram, M.S., 2018, Science of the Total Environment, v. 642, p. 125-136

Related Study Unit(s): Central Eastside San Joaquin Basin Groundwater Resources Used for Public Supply, Eastern Sacramento Valley and Foothills Groundwater Resources Used for Domestic Supply, Kern County Sub-Basin Groundwater Resources Used for Public Supply, Madera-Chowchilla and Kings Sub-basins Groundwater Resources Used for Domestic Supply, Madera-Chowchilla Basin Groundwater Resources Used for Public Supply, Modesto, Turlock, and Merced Subbasins of the San Joaquin Valley Groundwater Resources Used for Domestic Supply, Northern San Joaquin Valley Groundwater Resources Used for Public Supply, Southeast San Joaquin Valley Groundwater Resources Used for Public Supply, Tule-Tulare-Kaweah and Associated Highlands Groundwater Resources Used for Domestic Supply, Western San Joaquin Valley Groundwater Resources Used for Public Supply

ABSTRACT

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Total dissolved solids (TDS) concentrations in groundwater tapped for beneficial uses (drinking water, irrigation, freshwater industrial) have increased on average by about 100 mg/L over the last 100 years in the San Joaquin Valley, California (SJV). During this period land use in the SJV changed from natural vegetation and dryland agriculture to dominantly irrigated agriculture with growing urban areas. Century-scale salinity trends were evaluated by comparing TDS concentrations and major ion compositions of groundwater from wells sampled in 1910 (Historic) to data from wells sampled in 1993-2015 (Modern). TDS concentrations in subregions of the SJV, the southern (SSJV), western (WSJV), northeastern (NESJV), and southeastern (SESJV) were calculated using a cell-declustering method. TDS concentrations increased in all regions, with the greatest increases found in the SSJV and SESJV. Evaluation of the Modern data from the NESJV and SESJV found higher TDS concentrations in recently recharged (post-1950) groundwater from shallow (< 50 m) wells surrounded predominantly by agricultural land uses, while premodern (pre-1950) groundwater from deeper wells, and recently recharged groundwater from wells surrounded by mainly urban, natural, and mixed land uses had lower TDS concentrations, approaching the TDS concentrations in the Historic groundwater. For the NESJV and SESJV, inverse geochemical modeling with PHREEQC indicated that weathering of primary silicate minerals accounted for the majority of the increase in TDS concentrations, contributing more than nitrate from fertilizers and sulfate from soil amendments combined. Bicarbonate showed the greatest increase among major ions, resulting from enhanced silicate weathering due to recharge of irrigation water enriched in CO2 during the growing season. The results of this study demonstrate that large anthropogenic changes to the hydrologic regime, like massive development of irrigated agriculture in semi-arid areas like the SJV, can cause large changes in groundwater quality on a regional scale.