首页|平原区地下水位-水量响应关系及双控取水指标研究

平原区地下水位-水量响应关系及双控取水指标研究

扫码查看
由于不科学的地下水开发活动,导致我国部分地区地下水位下降严重,引发系列地质环境问题,迫切需要制定地下水位-水量双控管理措施,以实现地下水的可持续开发利用.然而单一的水量控制指标无法满足取水控制的科学管理需求,因此以襄阳市平原区为例,运用地下水数值模拟法,并结合不同情景的模拟预测,研究地下水位-水量的响应关系,从而确定出双控取水指标.结果表明:研究区的地下水位与开采量和降雨量呈现出良好的相关关系,随着开采强度的增大,地下水位出现明显的下降趋势,地下水位与开采量的响应关系可作为确定取水控制指标的重要依据;通过控制降水条件和超采区水位阈值,根据水位-水量响应关系计算出水位和水量阈值,得出浅层地下水在现状开采条件下的允许开采量阈值为1.16 亿m3,平均水位阈值为93.11 m;并考虑水文地质条件的空间异质性,对双控指标进行了空间差异化分区,为地下水的科学管理提供了参考依据.
Study on Groundwater Level-water Quantity Response Relationship and Dual-Control Water Withdrawal Index in Plain area
Due to unscientific groundwater development activities,the groundwater level in some areas of China has declined seriously,trig-gering a series of geo-environmental problems,and there is an urgent need to formulate the dual control management measures of groundwa-ter level-water quantity to realize the sustainable development and utilization of groundwater.However,a single water quantity control index cannot meet the scientific management demand of water withdrawal control,so this paper takes Xiangyang city plain area as an example,us-es groundwater numerical simulation method and combines the simulation prediction of different scenarios to study the response relationship of groundwater level-water quantity,so as to determine the dual-control water withdrawal index.The results show that,the groundwater lev-el in the study area shows a good correlation with the exploitation amount and rainfall.With the increase of exploitation intensity,the ground-water level shows a significant downward trend.The response relationship between groundwater level and exploitation amount can be used as an important basis for determining the control water withdrawal index.By controlling the precipitation conditions and the water level threshold of the over-exploitation area,the water level and water volume thresholds are calculated according to the water level-water volume response relationship.The permissible extraction volume threshold of shallow groundwater under the current exploitation conditions is 1.16×108 m3,and the average water level threshold is 93.11 m.Considering the spatial heterogeneity of the hydrogeological conditions,the spatially differ-entiated partitioning of the dual-control indexes is carried out,which provides a reference basis for the scientific management of groundwater.

Xiangyanggroundwaterresponse relationshipwithdrawal control indexes

李大星、罗明明、肖高欣

展开 >

中国地质大学(武汉)环境学院,湖北 武汉 430074

湖北省地质局第一地质大队,湖北 黄石 435000

襄阳 地下水 响应关系 取水控制指标

2025

中国农村水利水电
水利部中国灌溉排水发展中心 水利部农村水电及电气化发展局 武汉大学 中国国家灌溉排水委员会

中国农村水利水电

北大核心
影响因子:0.655
ISSN:1007-2284
年,卷(期):2025.(1)