Domestic well vulnerability to drought duration and unsustainable groundwater management in California's Central Valley

被引:66
作者
Pauloo, R. A. [1 ]
Escriva-Bou, A. [2 ]
Dahlke, H. [1 ]
Fencl, A. [3 ]
Guillon, H. [1 ]
Fogg, G. E. [1 ]
机构
[1] Univ Calif Davis, Hydrol Sci, One Shields Ave, Davis, CA 95616 USA
[2] Publ Policy Inst Calif, Water Policy Ctr, 500 Washington St,Suite 600, San Francisco, CA 94111 USA
[3] Univ Calif Davis, Dept Environm Sci & Policy, One Shields Ave, Davis, CA 95616 USA
基金
美国国家科学基金会;
关键词
groundwater; drought; domestic well; well failure; water management; dry well; AQUIFER RECHARGE; DRINKING-WATER; RISK;
D O I
10.1088/1748-9326/ab6f10
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Millions of Californians access drinking water via domestic wells, which are vulnerable to drought and unsustainable groundwater management. Groundwater overdraft and the possibility of longer drought duration under climate change threatens domestic well reliability, yet we lack tools to assess the impact of such events. Here, we leverage 943 469 well completion reports and 20 years of groundwater elevation data to develop a spatially-explicit domestic well failure model covering California's Central Valley. Our model successfully reproduces the spatial distribution of observed domestic well failures during the severe 2012-2016 drought (n = 2027). Next, the impact of longer drought duration (5-8 years) on domestic well failure is evaluated, indicating that if the 2012-2016 drought would have continued into a 6 to 8 year long drought, a total of 4037-5460 to 6538-8056 wells would fail. The same drought duration scenarios with an intervening wet winter in 2017 lead to an average of 498 and 738 fewer well failures. Additionally, we map vulnerable wells at high failure risk and find that they align with clusters of predicted well failures. Lastly, we evaluate how the timing and implementation of different projected groundwater management regimes impact groundwater levels and thus domestic well failure. When historic overdraft persists until 2040, domestic well failures range from 5966 to 10 466 (depending on the historic period considered). When sustainability is achieved progressively between 2020 and 2040, well failures range from 3677 to 6943, and from 1516 to 2513 when groundwater is not allowed to decline after 2020.
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页数:14
相关论文
共 62 条
  • [11] Managed winter flooding of alfalfa recharges groundwater with minimal crop damage
    Dahlke, Helen E.
    Brown, Andrew G.
    Orloff, Steve
    Putnam, Daniel
    O'Geen, Toby
    [J]. CALIFORNIA AGRICULTURE, 2018, 72 (01) : 65 - 75
  • [12] Anthropogenic warming has increased drought risk in California
    Diffenbaugh, Noah S.
    Swain, Daniel L.
    Touma, Danielle
    [J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2015, 112 (13) : 3931 - 3936
  • [13] Impact of water withdrawals from groundwater and surface water on continental water storage variations
    Doell, P.
    Hoffmann-Dobrev, H.
    Portmann, F. T.
    Siebert, S.
    Eicker, A.
    Rodell, M.
    Strassberg, G.
    Scanlon, B. R.
    [J]. JOURNAL OF GEODYNAMICS, 2012, 59-60 : 143 - 156
  • [14] Chromium isotopes and the fate of hexavalent chromium in the environment
    Ellis, AS
    Johnson, TM
    Bullen, TD
    [J]. SCIENCE, 2002, 295 (5562) : 2060 - 2062
  • [15] The global groundwater crisis
    Famiglietti, J. S.
    [J]. NATURE CLIMATE CHANGE, 2014, 4 (11) : 945 - 948
  • [16] Faunt C., 2009, US Geological Survey professional paper 1766, P225, DOI [10.3133/pp1766, DOI 10.3133/PP1766]
  • [17] Feinstein L, 2017, TECHNICAL REPORT
  • [18] Fujii R, 1995, Water-Resources Investigations Report 95-4048, DOI [10.3133/wri954048, DOI 10.3133/WRI954048]
  • [19] Domestic well reliability: evaluating supply interruptions from groundwater overdraft, estimating costs and managing economic externalities
    Gailey, Robert M.
    Lund, Jay R.
    Medellin-Azuara, Josue
    [J]. HYDROGEOLOGY JOURNAL, 2019, 27 (04) : 1159 - 1182
  • [20] Gailey RM, 2017, HYDROGEOL J, V25, P2163, DOI 10.1007/s10040-017-1588-y