三江平原浅层地下水超采问题探讨(二)  

Status Overdraft of Groundwater on Sanjiang Plain(2)

作　　者：袁斌 杜绍敏[2] 杨伟清[3] 赵卫 施树有 高洋 姚章村 

机构地区：[1]黑龙江省创业农场,富锦156321 [2]黑龙江大学水利电力学院,哈尔滨150086 [3]黑龙江省友谊农场,友谊156911 [4]黑龙江省850农场,虎林158400 [5]黑龙江省宝山农场,桦川154350 [6]黑龙江农垦水务局,哈尔滨150036 [7]黑龙江农垦勘测设计研究院,佳木斯154002

出　　处：《黑龙江水专学报》2008年第1期18-21,共4页Journal of Heilongjiang Hydraulic Engineering College

基　　金：国家"九五"科技攻关项目(96-004-02-03-01)

摘　　要：三江平源浅层地下水超采问题探讨[1](1)以地下水位下降速度判断后,再采用"控制地下水位"判断"超采问题",故定"探讨(二)"。由于确定地区控制地下水位研究较少,笔者以地下水理想水位与埋深理念确定临界和限制水位埋深比较安全。从三江平原全部、分区、典型农场几个尺度分析三江平原地下水大量开采至今,地下水位均处于理想水位埋深中,尚不到"临界水位或埋深",更谈不上达"限制水位或埋深",尚有开发潜力。The problem of groundwater overexploitation in the article of ＂discussion I ＂ was analysed by the exploitation rate of groundwater. The problem of groundwater overexploitation once more will be discussed by the restrained groundwater table. The limit research on restrained groundwater table＇s confirmation was made, to confirm the critical and restrained groundwater table on the basis of ideal groundwater table and buried depth theory will be helpful. Partitions and typical farms of Sanjiang Plain, the groundwater table were in perfect condition since the groundwater was mined on large scale and the groundwater sill had tremendous development potential.

关 键 词：理想水位 临界水位 限制水位 降水补给 江河激发补给 

分 类 号：P641.8[天文地球—地质矿产勘探] X523[天文地球—地质学]