松花江干流佳木斯-同江段地表水与地下水转化关系分析  

Research on the Relationship between Surface Water and Groundwater Transformation in Jiamusi Tongjiang Section of Songhua River Mainstream

作　　者：杨枭 于淼 荆建宇 戴长雷[1,2,3] YANG Xiao;YU Miao;JING Jianyu;DAI Changlei(School of Hydraulic and Electric-power,Heilongjiang University,Harbin 150080,China;Institute of Cold Groundwater,Heilongjiang University,Harbin 150080,China;International Joint Laboratory of Hydrology and Hydraulic Engineering in Cold Regions of Heilongjiang Province,Harbin 150080,China)

机构地区：[1]黑龙江大学水利电力学院,黑龙江哈尔滨150080 [2]黑龙江大学寒区地下水研究所,黑龙江哈尔滨150080 [3]黑龙江省寒区水文和水利工程联合实验室,黑龙江哈尔滨150080

出　　处：《云南水力发电》2024年第10期208-211,共4页Yunnan Water Power

基　　金：三江平原水土资源优化匹配与调控技术示范项目(XDA28100105)。

摘　　要：地下水与地表水相互作用是水文循环过程中的重要环节,且松花江流域转化复杂,理解该流域地表水地下水之间的转化过程非常重要。文中利用针对流域水循环的,累计转化量法与地表水水量平衡,对松花江佳木斯同江段进行研究,分析了2020年两者之间的转化关系,即2020年9月末—12月末,1月—3月,5月—6月为地表水补给地下水。4月—5月,7月—9月为地表水补给地下水。并且用两种方法进行对比,分析了实验的可行性,是开展松花江流域水资源调查评价的基础性研究。The interaction between groundwater and surface water is an important part of the hydrological cycle,and the transformation of surface water and groundwater in the Songhua River River basin is complex.Using the cumulative conversion method for the basin water cycle and the surface water balance,the paper studied the transformation relationship between the two in the Tongjiang section of the Jiamusi River in Songhua River in 2020,that is,from the end of September to the end of December,January to March,May to June in 2020 for surface water recharge groundwater.April-may,july-september for surface water recharge groundwater.The feasibility of the experiment is analyzed by comparing the two methods,which is the basic research for the investigation and evaluation of water resources in the Songhua River River basin.

关 键 词：松花江流域 地表水 地下水 转化关系 地表水量平衡 累计转化法 

分 类 号：TV211.1[水利工程—水文学及水资源]