Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.scitotenv.2018.05.333 |
Quantifying anthropogenic contributions to century-scale groundwater salinity changes, San Joaquin Valley, California, USA | |
Hansen, Jeffrey A.; Jurgens, Bryant C.; Fram, Miranda S. | |
通讯作者 | Hansen, Jeffrey A. |
来源期刊 | SCIENCE OF THE TOTAL ENVIRONMENT
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ISSN | 0048-9697 |
EISSN | 1879-1026 |
出版年 | 2018 |
卷号 | 642页码:125-136 |
英文摘要 | 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. Published by Elsevier B.V. |
英文关键词 | Total dissolved solids Tds Trends San Joaquin valley Bicarbonate Nitrate |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000439405600013 |
WOS关键词 | CONTERMINOUS UNITED-STATES ; PESTICIDE-RESIDUES ; SUPPLY WELLS ; NITRATE ; WATER ; AQUIFER ; QUALITY ; URANIUM ; TRENDS |
WOS类目 | Environmental Sciences |
WOS研究方向 | Environmental Sciences & Ecology |
来源机构 | United States Geological Survey |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/212983 |
作者单位 | US Geol Survey, Placer Hall,6000 J St, Sacramento, CA 95819 USA |
推荐引用方式 GB/T 7714 | Hansen, Jeffrey A.,Jurgens, Bryant C.,Fram, Miranda S.. Quantifying anthropogenic contributions to century-scale groundwater salinity changes, San Joaquin Valley, California, USA[J]. United States Geological Survey,2018,642:125-136. |
APA | Hansen, Jeffrey A.,Jurgens, Bryant C.,&Fram, Miranda S..(2018).Quantifying anthropogenic contributions to century-scale groundwater salinity changes, San Joaquin Valley, California, USA.SCIENCE OF THE TOTAL ENVIRONMENT,642,125-136. |
MLA | Hansen, Jeffrey A.,et al."Quantifying anthropogenic contributions to century-scale groundwater salinity changes, San Joaquin Valley, California, USA".SCIENCE OF THE TOTAL ENVIRONMENT 642(2018):125-136. |
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