华北平原区地下水开采量估算研究  

Estimation of Groundwater Withdrawal in the North China Plain

作　　者：李玲[1] 邵景力[1] 崔亚莉[1] 杨程[1] 韩忠[1] 

机构地区：[1]中国地质大学,北京100083

出　　处：《南水北调与水利科技》2013年第5期82-85,共4页South-to-North Water Transfers and Water Science & Technology

基　　金：国家重点基础研究发展计划"973"项目(2010CB428804)

摘　　要：准确获取地下水开采量对于区域地下水资源评价和管理工作具有十分重要的意义。但由于地下水开采活动过于分散,目前管理和计量的手段不足,导致地下水开采量统计数据存在较大误差。通过建立华北平原地下水流区域数值模型,利用模拟水位与实际观测水位相拟合的方法,完成了华北平原开采量的反演估算,最终获得了华北平原2002年-2008年各年的地下水开采量,其平均年开采量为249.20亿m3。Accurate estimation of groundwater withdrawal is meaningful for the assessment and management of regional ground- water resources. However, due to the dispersive groundwater pumping and inadequate means in the current management and statistic methods,errors exist in the statistical data of groundwater withdrawal. In this study, a numerical model of regional groundwater flow in the North China Plain was developed, and the inversion estimation of groundwater withdrawal was per- formed through the fitting between the simulated and measured water levels. Finally, the groundwater withdrawals data from 2002 to 2008 were obtained and the average annual groundwater withdrawal in the NCP was 2. 492×10^10 m3.

关 键 词：华北平原 地下水 开采量 数值模型 水量均衡 反演计算 地下水流模拟 

分 类 号：P641[天文地球—地质矿产勘探]