三江平原地下水系统与激发补给机理新探讨  

New Research on Mechanism of Groundwater Flowing System and Stimulated Recharge in Sanjiang Plain

作　　者：曹玉生 杜绍敏[2] 安瑞强 姚章村 

机构地区：[1]黑龙江农垦勘测设计研究院,佳木斯154002 [2]黑龙江大学水利电力学院,哈尔滨150086

出　　处：《黑龙江水专学报》2008年第3期5-7,共3页Journal of Heilongjiang Hydraulic Engineering College

基　　金：国家"九五"科技攻关项目(96-004-02-03-01);垦区"九五"科技攻关项目(HVKSY1001);黑龙江教育厅科学技术面上项目(11511274)

摘　　要：通过三江平原巨大且特殊的地下水贮水结构和流动系统分析,揭示三江平原地下水系统的巨大贮水、补给、传导、调节、循环功能和各自区带之分;结合近年来三江平原大规模人工开采实际对流动系统影响分析,更直观地揭示建三江地区地下水开采后获得激发补给的机理与可能。This article comprehensively reveals the huge functions such as water storage, recharge, conduction, adjustment, recycle and area partitions by analyzing the huge and special groundwater structure and flowing system in Sanjiang Plain. With analyzing the influence of large-scale mining in recent years on groundwater flowing system in Sanjiang Plain, it also more intuitively reveals the mechanism and possibility of stimulated recharge in Jiansanjiang Area.

关 键 词：含水层 岩性 补给 地下水位 地下调水 

分 类 号：P641.8[天文地球—地质矿产勘探]