气候变化与人类活动对石家庄市藁城区地下水位埋深的影响分析

doi:10.13278/j.cnki.jjuese.20200147

吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (3): 854-863.doi: 10.13278/j.cnki.jjuese.20200147

气候变化与人类活动对石家庄市藁城区地下水位埋深的影响分析

闫佰忠^1,2,3,4, 孙丰博^1,2,3,4, 李晓萌^1,2,3,4, 王玉清⁵, 范成博⁵, 陈佳琦^1,2,3,4

1. 河北地质大学水资源与环境学院, 石家庄 050031;
2. 河北省高校生态环境地质应用技术研发中心, 石家庄 050031;
3. 河北省水资源可持续利用与开发重点实验室, 石家庄 050031;
4. 河北省水资源可持续利用与产业结构化协同创新中心, 石家庄 050031;
5. 河北省地质资源环境监测与保护重点实验室, 石家庄 050031

收稿日期:2020-06-21 出版日期:2021-05-26 发布日期:2021-06-07
作者简介:闫佰忠(1988—),男,副教授,博士,主要从事水文地质、地热资源等方面的研究,E-mail:jluybz@126.com
基金资助:
国家自然科学基金项目（42002251），中国博士后基金面上项目（2018M631874），河北省自然科学基金项目（D2020403022），河北省高等学校科学技术研究项目（ZD2019082），河北省地质资源环境监测与保护重点实验室开发基金项目（JCYKT202001）；河北省科技厅研发项目（18273627）

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

Yan Baizhong^1,2,3,4, Sun Fengbo^1,2,3,4, Li Xiaomeng^1,2,3,4, Wang Yuqing⁵, Fan Chengbo⁵, Chen Jiaqi^1,2,3,4

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)

摘要/Abstract

摘要： 为了探寻石家庄市藁城区地下水埋深动态变化规律，以藁城区2001—2018年的年降水量、地下水人工开采量等数据为基础，对藁城区地下水位埋深进行研究。首先采用P-Ⅲ型曲线法确定降水序列的丰、平、枯年份，分析不同降水量情况下地下水位埋深变化规律；其次，利用地下水开采潜力系数法和灰色关联度法对人工开采量和地下水位埋深的关系进行研究。结果表明：1）藁城区地下水位埋深在2001—2016年逐渐增大，在2016—2018年趋于减小，2016年为转折点；在空间上藁城区地下水位埋深呈现出北部埋深小、南部埋深大的特征，北部水位埋深较同期南部水位埋深要浅5~10 m。2）降水是驱动藁城区地下水位埋深变化的重要因素，枯水年水位埋深变幅在0.8~1.5 m之间，平水年水位埋深变幅在0.3~1.2 m之间，丰水年水位埋深变幅在0.3~1.1 m之间。主灌期（3—6月）的地下水位埋深增加速率均为cm/d级，非主灌期（7—10月）的地下水位埋深减少速率均为mm/d级。3）人工开采是驱动藁城区地下水位埋深变化的主导因素，其中农业开采量占人工开采量的80%。综上认为，藁城区一直处于严重超采状态，地下水累计超采量每增加1亿m³，地下水位埋深增加0.45 m。

关键词: 地下水位埋深, 气候变化, 人工开采, 石家庄市藁城区

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

中图分类号:

P641

闫佰忠, 孙丰博, 李晓萌, 王玉清, 范成博, 陈佳琦. 气候变化与人类活动对石家庄市藁城区地下水位埋深的影响分析[J]. 吉林大学学报(地球科学版), 2021, 51(3): 854-863.

Yan Baizhong, Sun Fengbo, Li Xiaomeng, Wang Yuqing, Fan Chengbo, Chen Jiaqi. Impact of Climate Change and Human Activities on Groundwater Depth of Gaocheng District in Shijiazhuang City[J]. Journal of Jilin University(Earth Science Edition), 2021, 51(3): 854-863.

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气候变化与人类活动对石家庄市藁城区地下水位埋深的影响分析

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

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