Journal of Jilin University(Earth Science Edition) ›› 2021, Vol. 51 ›› Issue (3): 854-863.doi: 10.13278/j.cnki.jjuese.20200147

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Impact of Climate Change and Human Activities on Groundwater Depth of Gaocheng District in Shijiazhuang City

Yan Baizhong1,2,3,4, Sun Fengbo1,2,3,4, Li Xiaomeng1,2,3,4, Wang Yuqing5, Fan Chengbo5, Chen Jiaqi1,2,3,4   

  1. 1. School of Water Resources & Environment, Hebei GEO University, Shijiazhuang 050031, China;
    2. Hebei Center for Ecological and Environmental Geology Research, Shijiazhuang 050031, China;
    3. Hebei Province Key Laboratory of Sustained Utilization & Development of Water Resources, Shijiazhuang 050031, China;
    4. Hebei Province Collaborative Innovation Center for Sustainable Utilization of Water Resources and Optimization of Industrial Structure, Shijiazhuang 050031, China;
    5. Hebei Key Laboratory of Geological Resources and Environment Monitoring and Protection, Shijiazhuang 050031, China
  • Received:2020-06-21 Online:2021-05-26 Published:2021-06-07
  • Supported by:
    Supported by the National Natural Science Foundation of China (42002251),the China's Post-Doctoral Science Fund (2018M631874),the Natural Science Fund Project in Hebei Province (D2020403022,D2018403040),the Scientific Research Projects of the Higher University in Hebei (ZD2019082),the Key Laboratory of Geological Resources and Environmental Monitoring and Protection Fund of Hebei Province (JCYKT201901) and the Research and Development Project of Science and Technology Department of Hebei Province (18273627)

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Abstract: In order to explore the dynamic change law of groundwater depth in Gaocheng District in Shijiazhuang, based on the data of annual precipitation and artificial exploitation of groundwater from 2001 to 2018, we conducted a study on Gaocheng District. At first, the P-Ⅲ curve method is used to determine the high, normal and low flow years of precipitation by sequence, and the change law of groundwater depth under different precipitation conditions is analyzed; Secondly, the method of groundwater exploitation potential coefficient and the method of grey correlation degree are used to study the relationship volumes leves between the artificial exploitation volume and the depth of groundwater level. The results showed that: 1) The groundwater depth in Gaocheng District gradually increased from 2001 to 2016, decreased from 2016 to 2018, and 2016 was the turning point. Spatially, it showed the characteristics of smaller depth in the north and larger depth in the south in Gaocheng District, and the water level in the north was 5-10 m lower than that in the south in the same period. 2) Precipitation is an important factor to drive the change of groundwater depth in Gaocheng District. The variation range of groundwater level is 0.8-1.5 m in low flowyear, 0.3-1.2 m in normal flow year, and 0.3-1.1 m in high flow year. The increase rate of groundwater depth in the main irrigation period (March-June) is cm/d, and the decrease rate of groundwater depth in the non-main irrigation period (July-October) is mm/d. 3) Artificial exploitation is the main factor to drive the change of groundwater depth in Gaocheng District, while agricultural exploitation accounts for 80% of the total. According to the method of potential coefficient of groundwater exploitation, Gaocheng District has been under a condition of serious over exploitation since 2001. For every 100 million m3 of accumulated overexploitation of groundwater, the buried depth of groundwater increases by 0.45 m.

Key words: groundwater depth, climate change, artificial mining, Gaocheng District in Shijiazhuang City

CLC Number: 

  • P641
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