首页|2001-2016年河南省平原区浅层地下水动态变化特征研究

2001-2016年河南省平原区浅层地下水动态变化特征研究

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河南省平原区20多年来地下水一直处于高强度开采状态,导致地下水位持续下降,地下水埋深不断加大,2011年以来,随着水资源条件、地下水取用水情况等因素的变化,以及南水北调中线工程河南省受水区和全省公共供水管网覆盖区地下水压采、超采区综合治理等工作的开展,平原区地下水的超采状况也发生了明显变化.选取监测数据较完整的浅层地下水监测站980处,选取时段为评价期(2001-2016年)及2017-2018年(为反映地下水的长序列变化趋势、南水北调工程和地下水压采工作的效果,进行了合理延长).经统计分析,浅层地下水动态以下降趋势为主,平均下降速率0.057 m/a,最大下降速率1.297 m/a.
Dynamic changes of shallow groundwater in the plain area of Henan Province from 2001 to 2016
In the plain area of Henan Province,groundwater has been in a state of high intensity exploitation for more than 20 years,resulting in the continuous decline of ground water table and the continuous increase of groundwater burial depth.Since 2011,with the changes of water resources conditions,groundwater withdrawal and other factors,As well as the develop-ment of underground water pressure exploitation and comprehensive treatment of over-exploitation in the receiving area of Henan Province and the covered area of the public water supply network of the middle route of the South-to-North Water Transfer project,the over-exploitation of groundwater in the plain area has also changed obviously.980 shallow groundwater monitoring stations with relatively complete monitoring data were selected,and the selected periods were the evaluation period(2001-2016)and 2017-2018(reasonably extended to reflect the long-term trend of groundwater change,the effect of the South-to-North Water diversion project and underground water pressure production).According to the statistical analy-sis,the shallow groundwater dynamic is dominated by a downward trend,with an average rate of 0.057 m/a and a maximum rate of 1.297 m/a.

groundwaterdynamic changecontrastive analysis

乐扬、李王斌

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河南省地质局生态环境地质服务中心,河南郑州 450053

郑州大学综合设计研究院有限公司,河南郑州 450000

地下水 动态变化 对比分析

2024

地下水
陕西省水工程勘察规划研究院 全国地下水信息网 陕西省水利学会

地下水

影响因子:0.219
ISSN:1004-1184
年,卷(期):2024.46(5)