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.
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)
关键词
含水层
岩性
补给
地下水位
地下调水
aquifer
lithology
recharge
groundwater level
groundwater adjustment