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
[1] 孟素花,费宇红,张兆吉,等.华北平原地下水脆弱性评价[J].中国地质,2011,38(6):1607-1613. Meng Suhua, Fei Yuhong, Zhang Zhaoji, et al. Groundwater Vulnerability Assessment of North China Plain[J]. Geology in China, 2011, 38(6):1607-1613.
[2] 张光辉,费宇红,刘克岩,等.南水北调中线石家庄受水区地下水修复潜力及水位变化[J].地质通报,2007,26(5):583-589. Zhang Ganghui, Fei Yuhong, Liu Keyan, et al. Groundwater Potential Recovery and Water Level Variation in the Shijiazhuang Water-Receiving Area at the Central Line of the South-to-North Water Transfer Project, China[J]. Geological Bulletin of China, 2007,26(5):583-589.
[3] Wang W K, Zhang Z Y, Duan L, et al. Response of the Groundwater System in the Guanzhong Basin (Central China) to Climate Change and Human Activities[J]. Hydrogeology Journal, 2018, 26(5):1429-1441.
[4] Zhang Y, Wang J C, Jing J H, et al. Response of Groundwater to Climate Change Under Extreme Climate Conditions in North China Plain[J]. Journal of Earth Science, 2014, 25(3): 612-618.
[5] Fan J H, Liu Q, Zhang Y, et al. Dynamic Variations and Influencing Factors of Groundwater Levels in Lhasa City[J]. Wuhan University Journal of Natural Sciences,2005(4):665-673.
[6] Patil N S, Chetan N L, Nataraja M, et al. Climate Change Scenarios and Its Effect on Groundwater Level in the Hiranyakeshi Watershed[J]. Groundwater for Sustainable Development, 2020, 10: 100323.
[7] Lasagna M, Mancini S, Luca D A. Groundwater Hydrodynamic Behaviors Based on Water Table Levels to Identify Natural and Anthropic Controlling Factors in the Piedmont Plain (Italy)[J]. Science of the Total Environment, 2020, 716:137051.
[8] 冯慧敏.石家庄平原区地下水流场演变特征与尺度效应[D].北京:中国地质科学院,2015. Feng Huimin. Groundwater Flow Field Evolution Characteristic and Size Effect of Shijiazhuang Plain[D]. Beijing:Chinese Academy of Geological Sciences, 2015.
[9] 许月卿.京津以南河北平原地下水位下降驱动因子的定量评估[J].地理科学进展,2003,22(5):490-498. Xu Yueqing. Evaluation of Groundwater Level Drawdown Driving Forces in the Hebei Plain to the South of Beijing and Tianjin[J]. Progress in Geography, 2003, 22(5):490-498.
[10] 史入宇,崔亚莉,赵婕,等.滹沱河地区地下水适宜水位研究[J].水文地质工程地质,2013,40(2):36-41. Shi Ruyu, Cui Yali, Zhao Jie, et al.A Study of the Suitable Groundwater Level of the Hutuo River Area[J]. Hydrogeology & Engineering Geology, 2013, 40(2):36-41.
[11] 李雪,叶思源,宋凡,等.京津冀平原区地下水水位变化主导因素的定量识别研究[J].水文,2018,38(1):21-27. Li Xue, Ye Siyuan, Song Fan, et al. Quantitative Identification of Major Factors Affecting Groundwater Change in Beijing-Tianjin-Hebei Plain[J]. Journal of China Hydrology, 2018, 38(1):21-27.
[12] 赵自阳,李王成,王霞,等.基于主成分分析和因子分析的宁夏水资源承载力研究[J].水文,2017,37(2):64-72. Zhao Ziyang, Li Wangcheng, Wang Xia, et al. Study on Water Resources Carrying Capacity in Ningxia Based on Principal Component Analysis and Factor Analysis[J]. Journal of China Hydrology, 2017, 37(2):64-72.
[13] 闫佰忠,孙剑,王昕洲,等.基于多变量LSTM神经网络的地下水水位预测[J].吉林大学学报(地球科学版),2020,50(1):208-216. Yan Baizhong,Sun Jian, Wang Xinzhou,et al. Multivariable LSTM Neural Network Model for Groundwater Levels Prediction[J]. Journal of Jilin University (Earth Science Edition), 2020, 50(1):208-216.
[14] 王电龙,冯慧敏,田言亮,等.降水和开采变化对滹滏农业区地下水流场影响特征与机制[J].海河水利,2017(2):20-24. Wang Dianlong, Feng Huimin, Tian Yanliang, et al. Characteristics and Mechanism of Precipitation and Groundwater Exploitation Influence on Groundwater Flow Filed in Agricultural Field Hufu[J]. Haihe Water Resources, 2017(2):20-24.
[15] 石建省,王昭,张兆吉,等.华北平原深层地下水超采程度计算与分析[J].地学前缘,2010,17(6):215-220. Shi Jiansheng, Wang Zhao, Zhang Zhaoji, et al. Assessment of Over-Exploitation of Deep Groundwater in the North China Plain[J]. Earth Science Frontiers,2010,17(6):215-220.
[16] 中国地质调查局.GWI-D4地下水潜力评价技术要求[M].北京:地质出版社,2004:57-62. China Geological Survey.GWI-D4 Groundwater Potential Evaluation Technical Requirements[M]. Beijing:Geological Publishing House,2004:57-62.
[17] 张兆吉,费宇红.华北平原地下水可持续利用调查评价[M].北京:地质出版社,2009:361. Zhang Zhaoji,Fei Yuhong. Investigation and Evaluation on Sustainable Utilization of Groundwater in the North China Plain[M]. Beijing:Geological Publishing House,2009:361.
[18] 赵晓芬.灰色系统理论概述[J].吉林省教育学院学报,2011,27(3):152-154. Zhao Xiaofen. Summary of Grey System Theory[J]. Journal of Educational Institute of Jilin Province,2011,27(3):152-154.
[19] 李宝玉.吉林市区地下水位动态变化研究[D].长春:吉林大学,2020. Li Baoyu. Study on Dynamic Change of Groundwater Level in Jilin City[D].Changchun:Jilin University, 2020.
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