Long-term groundwater storage changes and land subsidence development in the North China Plain (1971–2015)

Gong, Huili; Pan, Yun; Zheng, Longqun; Li, Xiaojuan; Zhu, Lin; Zhang, Chong; Huang, Zhiyong; Li, Zhiping; Wang, Haigang; Zhou, Chaofan

Long-term groundwater storage changes and land subsidence development in the North China Plain (1971–2015) | Variations à long terme du stockage des eaux souterraines et développement de l’affaissement des terrains dans la Plaine de Chine du Nord (1971–2015) Cambios en el almacenamiento de agua subterránea y en el desarrollo de subsidencia del terreno a largo plazo en la Llanura Norte de China (1971–2015) 华北平原1971–2015年地下水储量变化与地面沉降演化研究 Mudanças no armazenamento das águas subterrâneas de longo termo e desenvolvimento de subsidência de terreno na Planície do Norte da China (1971–2015)

2018

The North China Plain (NCP) has been suffering from groundwater storage (GWS) depletion and land subsidence for a long period. This paper collects data on GWS changes and land subsidence from in situ groundwater-level measurements, literature, and satellite observations to provide an overview of the evolution of the aquifer system during 1971–2015 with a focus on the sub-regional variations. It is found that the GWS showed a prolonged declining rate of −17.8 ± 0.1 mm/yr during 1971–2015, with a negative correlation to groundwater abstraction before year ~2000 and a positive correlation after ~2000. Statistical correlations between subsidence rate and the GWS anomaly (GWSA), groundwater abstraction, and annual precipitation show that the land subsidence in three sub-regions (Beijing, Tianjin, and Hebei) represents different temporal variations due to varying driver factors. Continuous drought caused intensive GWS depletion (−76.1 ± 6.5 mm/yr) and land subsidence in Beijing during 1999–2012. Negative correlations between total groundwater abstraction and land subsidence exhibited after the 1980s indicate that it may be questionable to infer subsidence from regional abstraction data. Instead, the GWSA generally provides a reliable correlation with subsidence. This study highlights the spatio-temporal variabilities of GWS depletion and land subsidence in the NCP under natural and anthropogenic impacts, and the importance of GWS changes for understanding land subsidence development.

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