Sub-regional groundwater storage recovery in North China Plain after the South-to-North water diversion project

•GWS recovery was observed by 617 monitoring wells in NCP after MRP operation.•GRACE detected similar patterns of GWS depletion and recovery with wells.•Pumping decrease and precipitation increase jointly drove GWS recovery. The South-to-North water diversion Middle Route Project (MRP) is expected t...

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Published inJournal of hydrology (Amsterdam) Vol. 597; p. 126156
Main Authors Zhang, Chong, Duan, Qingyun, J.-F. Yeh, Pat, Pan, Yun, Gong, Huili, Moradkhani, Hamid, Gong, Wei, Lei, Xiaohui, Liao, Weihong, Xu, Lei, Huang, Zhiyong, Zheng, Longqun, Guo, Xueru
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.06.2021
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ISSN0022-1694
1879-2707
DOI10.1016/j.jhydrol.2021.126156

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Abstract •GWS recovery was observed by 617 monitoring wells in NCP after MRP operation.•GRACE detected similar patterns of GWS depletion and recovery with wells.•Pumping decrease and precipitation increase jointly drove GWS recovery. The South-to-North water diversion Middle Route Project (MRP) is expected to alleviate the long-term groundwater storage (GWS) depletion in North China Plain (NCP) after the beginning of its operation in December 2014. This study aims to investigate the effect of MRP on GWS by comparing GWS changes before (2003–2014) and after (2015–2018) the MRP operation. The analysis was conducted by using groundwater level data from 617 wells in NCP, and then evaluated against satellite-based water storage data from Gravity Recovery and Climate Experiment (GRACE) and its Follow-On missions. On average in NCP, a decreasing trend of −19.1 ± 5.1 mm/yr was seen in GWS based on well observations during 2003–2014, but a recovery trend of +1.8 ± 0.7 mm/yr was found during 2015–2018. The GWS recovery was most prominent in subregions where groundwater over-utilization had occurred in NCP. GRACE exhibited the capacity to detect the regional GWS depletion during 2003–2014, but difficult to distinguish the sub-regional GWS recovery during 2015–2018. The potential causes for GWS recovery were found to be complicated, not only caused by the reduction of groundwater pumping as accelerated by MRP-diverted water, but also the increasing precipitation recharge of aquifers and the enhanced management of groundwater system. The findings highlight that GWS in NCP has started a gradual transition from unsustainable depletion to sub-regional recovery as benefit from the MRP water diversion.
AbstractList •GWS recovery was observed by 617 monitoring wells in NCP after MRP operation.•GRACE detected similar patterns of GWS depletion and recovery with wells.•Pumping decrease and precipitation increase jointly drove GWS recovery. The South-to-North water diversion Middle Route Project (MRP) is expected to alleviate the long-term groundwater storage (GWS) depletion in North China Plain (NCP) after the beginning of its operation in December 2014. This study aims to investigate the effect of MRP on GWS by comparing GWS changes before (2003–2014) and after (2015–2018) the MRP operation. The analysis was conducted by using groundwater level data from 617 wells in NCP, and then evaluated against satellite-based water storage data from Gravity Recovery and Climate Experiment (GRACE) and its Follow-On missions. On average in NCP, a decreasing trend of −19.1 ± 5.1 mm/yr was seen in GWS based on well observations during 2003–2014, but a recovery trend of +1.8 ± 0.7 mm/yr was found during 2015–2018. The GWS recovery was most prominent in subregions where groundwater over-utilization had occurred in NCP. GRACE exhibited the capacity to detect the regional GWS depletion during 2003–2014, but difficult to distinguish the sub-regional GWS recovery during 2015–2018. The potential causes for GWS recovery were found to be complicated, not only caused by the reduction of groundwater pumping as accelerated by MRP-diverted water, but also the increasing precipitation recharge of aquifers and the enhanced management of groundwater system. The findings highlight that GWS in NCP has started a gradual transition from unsustainable depletion to sub-regional recovery as benefit from the MRP water diversion.
The South-to-North water diversion Middle Route Project (MRP) is expected to alleviate the long-term groundwater storage (GWS) depletion in North China Plain (NCP) after the beginning of its operation in December 2014. This study aims to investigate the effect of MRP on GWS by comparing GWS changes before (2003–2014) and after (2015–2018) the MRP operation. The analysis was conducted by using groundwater level data from 617 wells in NCP, and then evaluated against satellite-based water storage data from Gravity Recovery and Climate Experiment (GRACE) and its Follow-On missions. On average in NCP, a decreasing trend of −19.1 ± 5.1 mm/yr was seen in GWS based on well observations during 2003–2014, but a recovery trend of +1.8 ± 0.7 mm/yr was found during 2015–2018. The GWS recovery was most prominent in subregions where groundwater over-utilization had occurred in NCP. GRACE exhibited the capacity to detect the regional GWS depletion during 2003–2014, but difficult to distinguish the sub-regional GWS recovery during 2015–2018. The potential causes for GWS recovery were found to be complicated, not only caused by the reduction of groundwater pumping as accelerated by MRP-diverted water, but also the increasing precipitation recharge of aquifers and the enhanced management of groundwater system. The findings highlight that GWS in NCP has started a gradual transition from unsustainable depletion to sub-regional recovery as benefit from the MRP water diversion.
ArticleNumber 126156
Author Lei, Xiaohui
Gong, Huili
Liao, Weihong
Pan, Yun
Duan, Qingyun
Gong, Wei
Zheng, Longqun
Guo, Xueru
Xu, Lei
Moradkhani, Hamid
Zhang, Chong
Huang, Zhiyong
J.-F. Yeh, Pat
Author_xml – sequence: 1
  givenname: Chong
  surname: Zhang
  fullname: Zhang, Chong
  organization: Institute of Land Surface System and Sustainable Development, Beijing Normal University, Beijing, China
– sequence: 2
  givenname: Qingyun
  surname: Duan
  fullname: Duan, Qingyun
  email: qyduan@hhu.edu.cn
  organization: State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing, China
– sequence: 3
  givenname: Pat
  surname: J.-F. Yeh
  fullname: J.-F. Yeh, Pat
  organization: Discipline of Civil Engineering, School of Engineering, Monash University (Malaysia Campus), Malaysia
– sequence: 4
  givenname: Yun
  surname: Pan
  fullname: Pan, Yun
  organization: Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing, China
– sequence: 5
  givenname: Huili
  surname: Gong
  fullname: Gong, Huili
  organization: Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing, China
– sequence: 6
  givenname: Hamid
  surname: Moradkhani
  fullname: Moradkhani, Hamid
  organization: Center for Complex Hydrosystems Research, The University of Alabama, Tuscaloosa, AL, USA
– sequence: 7
  givenname: Wei
  surname: Gong
  fullname: Gong, Wei
  organization: Institute of Land Surface System and Sustainable Development, Beijing Normal University, Beijing, China
– sequence: 8
  givenname: Xiaohui
  surname: Lei
  fullname: Lei, Xiaohui
  organization: Sate Key Laboratory of Stimulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China
– sequence: 9
  givenname: Weihong
  surname: Liao
  fullname: Liao, Weihong
  organization: Sate Key Laboratory of Stimulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing, China
– sequence: 10
  givenname: Lei
  surname: Xu
  fullname: Xu, Lei
  organization: State Key Laboratory of Information Engineering in Surveying, Mapping, and Remote Sensing, Wuhan University, Wuhan, China
– sequence: 11
  givenname: Zhiyong
  surname: Huang
  fullname: Huang, Zhiyong
  organization: Department of Earth Sciences, The University of Hong Kong, Hong Kong, China
– sequence: 12
  givenname: Longqun
  surname: Zheng
  fullname: Zheng, Longqun
  organization: Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing, China
– sequence: 13
  givenname: Xueru
  surname: Guo
  fullname: Guo, Xueru
  organization: Department of Statistics, Beijing Normal University, Beijing, China
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Keywords Groundwater recovery
South-to-North water diversion
GRACE
Groundwater depletion
North China Plain
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Snippet •GWS recovery was observed by 617 monitoring wells in NCP after MRP operation.•GRACE detected similar patterns of GWS depletion and recovery with...
The South-to-North water diversion Middle Route Project (MRP) is expected to alleviate the long-term groundwater storage (GWS) depletion in North China Plain...
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SubjectTerms China
climate
GRACE
groundwater
Groundwater depletion
Groundwater recovery
North China Plain
satellites
South-to-North water diversion
water storage
water table
Title Sub-regional groundwater storage recovery in North China Plain after the South-to-North water diversion project
URI https://dx.doi.org/10.1016/j.jhydrol.2021.126156
https://www.proquest.com/docview/2524305097
Volume 597
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