高寒区冰泉水探析  

Analysis of ice fountain of alpine region

作　　者：维克多.瓦西里耶维奇.舍佩廖夫 戴长雷[2,3,4] 王敏[3] 苗兴亚 

机构地区：[1]俄罗斯科学院西伯利亚分院麦尔尼科夫冻土研究所,萨哈共和国雅库茨克677010 [2]黑龙江大学寒区地下水研究所,黑龙江哈尔滨150080 [3]黑龙江大学水利电力学院,黑龙江哈尔滨150080 [4]中国科学院寒区旱区环境与工程研究所冻土工程国家重点实验室,甘肃兰州730000 [5]黑龙江大学中俄联合研究生院,黑龙江哈尔滨150080

出　　处：《黑龙江水利》2016年第10期18-23,共6页

基　　金：冻土工程国家重点实验室开放基金(NO.SKLFSE201310);黑龙江省水文局项目(NO.2014230101000411)

摘　　要：高寒地区冰泉水的探析对寒区冻结层上水的研究具有重要的意义。通过对高寒区冰泉水的探析,指出:①目前对冻结层上水冰泉形成状况的研究还不够深刻;②地下水冰泉的形成受负温因素、冰冻因素、冻土因素的影响;③通过实例分析可得出:在河谷中的冻结层上地下水冰泉的形成过程具有双波峰特性,它有2个体积最大增长值;④冰泉只由季节性融化层水形成,而没有冻结层上地下水的参与。Analysis of ice fountain of alpine region is important to study the frozen groundwater of cold region. Through the analysis of the ice fountain of alpine region. It points that： （1）The current study of forming conditions of the ice fountain of the frozen groundwater is not impressive enough; （2）The formation of ground ice fountain is affected at negative temperature factors, frozen factors, permafrost factors. （3）Through the analysis of the example, in the course of the upper valley of the formation of ground ice fountain, the formation of ice fountain having a double peak characteristics, it has the largest volume increase of two values; （4）Ice fountain only consists of water spring melt layer formed by the seasonal, but not participating in frozen layer on groundwater.

关 键 词：冰泉水 季融层 冻结层 高寒区 

分 类 号：P641[天文地球—地质矿产勘探]