日本地球惑星科学連合2018年大会

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[EE] Eveningポスター発表

セッション記号 A (大気水圏科学) » A-HW 水文・陸水・地下水学・水環境

[A-HW22] 水循環・水環境

2018年5月24日(木) 17:15 〜 18:30 ポスター会場 (幕張メッセ国際展示場 7ホール)

コンビーナ:長尾 誠也(金沢大学環日本海域環境研究センター)、町田 功(産業技術総合研究所地質調査総合センター)、飯田 真一(国立研究開発法人森林研究・整備機構森林総合研究所森林研究部門森林防災研究領域水保全研究室、共同)、林 武司(秋田大学教育文化学部)

[AHW22-P13] Long-term groundwater storage changes and land subsidence development in the North China Plain (1971-2015)

Huili Gong1,2Yun Pan1,2、*Longqun Zheng1,2Xiaojuan Li1,2Lin Zhu1,2Chong Zhang3,4Zhiyong Huang5Zhiping Li6Haigang Wang7Chaofan Zhou1,2 (1.Beijing Laboratory of Water Resources Security, Capital Normal University, Beijing 100048, China.、2.College of Resource Environment and Tourism, Capital Normal University, Beijing 100048, China.、3.State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China、4.Institute of Land Surface System and Sustainable Development, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, China、5.Department of Earth Sciences, The University of Hong Kong, Hong Kong, China.、6.Beijing Institute of Hydrogeology and Engineering Geology, Beijing 100048, China.、7.China Geological and Environmental Monitoring Institute, Beijing 100081, China.)

キーワード:Over-abstraction, Subsidence, Drought, GRACE, InSAR

The North China Plain (NCP) has been suffering from groundwater storage (GWS) depletion and land subsidence for a long period. This paper collects data of 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 shows a prolonged declining rate of -17.8±0.1 mm/yr during 1971-2015, with a negative (positive) correlation to groundwater abstraction before (after) 2000s. Statistical correlations between subsidence rate and 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 driven 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 1980s indicating 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.