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

• Published in: Hydrogeology journal Vol. 26; no. 5; pp. 1417 - 1427
• Main Authors: Gong, Huili, Pan, Yun, Zheng, Longqun, Li, Xiaojuan, Zhu, Lin, Zhang, Chong, Huang, Zhiyong, Li, Zhiping, Wang, Haigang, Zhou, Chaofan
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01-08-2018; Springer Nature B.V
• Subjects: Annual precipitation; Anthropogenic factors; Aquatic Pollution; Aquifer systems; Aquifers; Correlation; Correlation analysis; Depletion; Drought; Earth and Environmental Science; Earth Sciences; Evolution; Geology; Geophysics/Geodesy; Groundwater; Groundwater depletion; Groundwater flow; Groundwater levels; Groundwater storage; Human influences; Hydrogeology; Hydrology/Water Resources; Land subsidence; Precipitation; Regional variations; Satellite observation; Satellites; Subsidence; Temporal variations; Variation; Waste Water Technology; Water Management; Water Pollution Control; Water Quality/Water Pollution; Beijing China; China; Subsidence; Drought; Over-abstraction; GRACE; China
• ISSN: 1431-2174; 1435-0157
• DOI: 10.1007/s10040-018-1768-4

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.