Groundwater storage and depletion trends in the Loess areas of China

Groundwater is the essential source of drinking and irrigation water supplies in most parts of the world. The Loess area is one among the largest manufacturers of agricultural merchandise in China and is to a great extent dependent on groundwater for public water supply and irrigation. The effect of expanded open supplies and irrigation on groundwater levels has not been very much investigated, both spatially and temporally. Thus, this study has used remote sensing data from NASA’s Gravity Recovery and the Global Land Data Assimilation Systems to assess the aggregate change in groundwater storage across the Loess area over a period of 13 years, from 2002 to 2014. The results demonstrate that the total groundwater depletion occurred at the rate of 529.73 km3 yr−1, and the mean groundwater consumption rate was −3.89 cm yr−1 between the winter and monsoon seasons during the period of 2002–2014. The most extreme consumption rate occurred during 2004 (−7.60 cm yr−1), while the minimum occurred during 2003 (1.13 cm yr−1). Groundwater consumption at such high rates will prompt unsustainable groundwater levels, bringing about financial anxiety, vulnerability to environmental change and excruciating burdens to sustenance and water security. Careful assessment of spatiotemporal groundwater storage in the Loess area will help China’s water resource managers and policymakers administrate groundwater resources in the future to improve water and food security.

[1]  Gan Zhang,et al.  Polypedogenic case of loess overlying red clay as a response to the Last Glacial–Interglacial cycle in mid-subtropical Southeast China , 2015 .

[2]  S. Seneviratne,et al.  Basin scale estimates of evapotranspiration using GRACE and other observations , 2004 .

[3]  Juana Paul Moiwo,et al.  Comparison of GRACE with in situ hydrological measurement data shows storage depletion in Hai River basin, Northern China , 2009 .

[4]  Seasonal water storage change of the Yangtze River basin detected by GRACE , 2006 .

[5]  W. Dietrich,et al.  Sediment load and floodplain deposition rates: Comparison of the Fly and Strickland rivers, Papua New Guinea , 2008 .

[6]  J. Famiglietti,et al.  Satellite-based estimates of groundwater depletion in India , 2009, Nature.

[7]  M. Watkins,et al.  The gravity recovery and climate experiment: Mission overview and early results , 2004 .

[8]  James L. Davis,et al.  Land water storage within the Congo Basin inferred from GRACE satellite gravity data , 2006 .

[9]  P. Lherminier,et al.  Recent changes in the Greenland–Scotland overflow‐derived water transport inferred from hydrographic observations in the southern Irminger Sea , 2009 .

[10]  X. Chang,et al.  The ice sheet height changes and mass variations in Antarctica by using ICESat and GRACE data , 2011 .

[11]  Peiyue Li,et al.  Assessment of groundwater vulnerability in the Yinchuan Plain, Northwest China using OREADIC , 2012, Environmental Monitoring and Assessment.

[12]  I. Velicogna Increasing rates of ice mass loss from the Greenland and Antarctic ice sheets revealed by GRACE , 2009 .

[13]  Jin-zhong Yang,et al.  Analysis of rainfall-recharge relationships , 1996 .

[14]  Wenzhao Liu,et al.  Impacts of land use change and climate variability on hydrology in an agricultural catchment on the Loess Plateau of China , 2009 .

[15]  Xiufeng He,et al.  Estimating Total Discharge in the Yangtze River Basin Using Satellite-Based Observations , 2013, Remote. Sens..

[16]  Byron D. Tapley,et al.  Interannual variability of Greenland ice losses from satellite gravimetry , 2011 .

[17]  Thomas C. Winter,et al.  Ground water and surface water a single resource: U , 1998 .

[18]  W. Feng,et al.  Evaluation of groundwater depletion in North China using the Gravity Recovery and Climate Experiment (GRACE) data and ground‐based measurements , 2013 .

[19]  N. Takegawa,et al.  Rapid aerosol particle growth and increase of cloud condensation nucleus activity by secondary aerosol formation and condensation: A case study for regional air pollution in northeastern China , 2009 .

[20]  Byron D. Tapley,et al.  Contribution of ice sheet and mountain glacier melt to recent sea level rise , 2013 .

[21]  Matthew Rodell,et al.  The potential for satellite-based monitoring of groundwater storage changes using GRACE: the High Plains aquifer, Central US , 2002 .

[22]  Qingren Wang,et al.  Phosphorus fractionation and distribution in sediments from wetlands and canals of a water conservation area in the Florida Everglades , 2011 .

[23]  J. Famiglietti,et al.  Estimating groundwater storage changes in the Mississippi River basin (USA) using GRACE , 2007 .

[24]  J. Wahr,et al.  Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada , 2012 .

[25]  F. Landerer,et al.  Accuracy of scaled GRACE terrestrial water storage estimates , 2012 .

[26]  W. Tad Pfeffer,et al.  Recent contributions of glaciers and ice caps to sea level rise , 2012, Nature.

[27]  J. Kimball,et al.  A new global river network database for macroscale hydrologic modeling , 2012 .

[28]  O. Andersen,et al.  Global inter‐annual gravity changes from GRACE: Early results , 2005 .

[29]  F. R. Troech,et al.  Soil and Water Conservation , 1976 .

[30]  M. Rodell,et al.  Water in the Balance , 2013, Science.

[31]  Jurgen Neuberg,et al.  Unprecedented pressure increase in deep magma reservoir triggered by lava‐dome collapse , 2006 .

[32]  S. Swenson,et al.  Post‐processing removal of correlated errors in GRACE data , 2006 .

[33]  Christopher Potter,et al.  Simulating the impacts of disturbances on forest carbon cycling in North America: processes, data, models, and challenges , 2011 .

[34]  Wenji Zhao,et al.  Subregional‐scale groundwater depletion detected by GRACE for both shallow and deep aquifers in North China Plain , 2015 .

[35]  D. Chambers,et al.  Estimating Geocenter Variations from a Combination of GRACE and Ocean Model Output , 2008 .

[36]  B. D. Tapley,et al.  Recent La Plata basin drought conditions observed by satellite gravimetry , 2010 .

[37]  D. Frank,et al.  Reconstructed warm season temperatures for Nome, Seward Peninsula, Alaska , 2004 .

[38]  R. Nerem,et al.  Recent Greenland Ice Mass Loss by Drainage System from Satellite Gravity Observations , 2006, Science.

[39]  Matthew Rodell,et al.  Groundwater depletion in the Middle East from GRACE with implications for transboundary water management in the Tigris-Euphrates-Western Iran region , 2013, Water resources research.

[40]  John S. Kimball,et al.  Global Biomass Variation and Its Geodynamic Effects: 1982–98 , 2005 .

[41]  Jens Wickert,et al.  The Falling Lake Victoria Water Level: GRACE, TRIMM and CHAMP Satellite Analysis of the Lake Basin , 2008 .

[42]  Q. Tang,et al.  Anthropogenic impacts on mass change in North China , 2013 .

[43]  Frédéric Frappart,et al.  Changes in terrestrial water storage versus rainfall and discharges in the Amazon basin , 2013 .

[44]  Houze Xu,et al.  Trend of China land water storage redistribution at medi- and large-spatial scales in recent five years by satellite gravity observations , 2009 .

[45]  B. Tapley,et al.  2005 drought event in the Amazon River basin as measured by GRACE and estimated by climate models , 2009 .

[46]  Charles S. Zender,et al.  Gravity Recovery and Climate Experiment (GRACE) detection of water storage changes in the Three Gorges Reservoir of China and comparison with in situ measurements , 2011 .

[47]  Kenneth L. Clark,et al.  Ecosystem carbon dioxide fluxes after disturbance in forests of North America , 2010 .

[48]  Alexander Y. Sun,et al.  Predicting groundwater level changes using GRACE data , 2013 .