南水北调实施后华北平原地下水调控研究  

Research on Groundwater Regulation and Recoveryin North China Plain after the Implementation of South-to-North Water Transfer

作　　者：崔亚莉[1] 王亚斌[2] 邵景力[1] 池娅萍 林坜 

机构地区：[1]中国地质大学,北京100083 [2]天津市地质调查研究院,天津300191 [3]北达科他州立大学,美国法戈58102 [4]北京市水利自动化研究所,北京100036

出　　处：《资源科学》2009年第3期382-387,共6页Resources Science

基　　金：中国地质调查局项目“:华北平原地下水可持续利用调查评价”(编号:1212010430351)。

摘　　要：随着南水北调中线工程调水实施的日益临近,华北平原地下水开采调控研究已成为人们关注的焦点问题。本文针对华北平原地下水开采现状以及存在的环境问题,确定了优先考虑严重超采中心区及深层水减采等一系列地下水调控原则,结合地下水可采资源量,给出了南水北调实施后的地下水规划开采量。应用所建立的华北平原地下水数值模型,预测了地下水调控的恢复效果,结果显示,经过10年地下水开采调整,重点控制区内的浅层地下水中心漏斗水位有不同程度回升,石家庄漏斗年均水位上升速率2.1m/a;深层地下水漏斗影响范围也有显著缩小,德州水位回升年均上升速率为（0.8-1.5）m/a。南水北调工程对华北平原地下水的恢复具有重要的作用。It is highly serious for the shortage of water resources in North China Plain, and groundwater utilization is up to 69% of the total water supply. Consequently, groundwater table has being gradually descending due to continuous groundwater overexploitation, and many environmental-geological problems have occurred, such as land subsidence, seawater intrusion etc. With the implementation of South-to-North Water Transfer （middle route）, research on groundwater regulation in North China Plain has been under heated discussion. Considering present conditions and environmental problems of groundwater in North China Plain, we have proposed a series of rules for groundwater regulation, such as giving priority to reducing groundwater development in seriously overexploited areas and deep aquifers, and sketching out the exploitation amount of groundwater after the implementation of South-to-North Water Transfer is completed based on groundwater recoverable resources. Recovery effect of groundwater regulation has been predicted by applying groundwater numerical model in North China Plain. It can be concluded that ten years after groundwater regulation is brought into effect, the groundwater table of depression cone in shallow aquifer would recover to various degrees in major controlling areas. For example, the groundwater table in depression cone in Shijiazhuang recovers by 2.1m/a. Meanwhile, depression cone area in deep aquifer would also shrink; for instance, the groundwater table in depression cone in Dezhou recovers by 0.8-1.5m/a. The storage rate in unconfined aquifer is 17.79 ×10^8m^3/a and would recover effectively, but the confined aquifer would recover more slowly. Therefore, South-to-North Water Transfer （middle route） does great help in groundwater recovery in North China Plain. We should take good advantage of abundant water resources available from external regions and give full play to the project. Meanwhile, rules for groundwater regulation should be made to restrict the expansion and deepening of exis

关 键 词：华北平原 南水北调中线 地下水调控开采 预测 恢复 

分 类 号：P641[天文地球—地质矿产勘探]