[1]戴长雷,孙思淼,叶勇.高寒区土壤包气带融雪入渗特征及其影响因素分析[J].水土保持研究,2010,17(03):269-272.
　DAI Chang-lei,SUN Si-miao,YE Yong.Analysis of Influencing Factors of Snowmelt Water Infiltration into Ground in Frigid Zone[J].Research of Soil and Water Conservation,2010,17(03):269-272.
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高寒区土壤包气带融雪入渗特征及其影响因素分析

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 17 期数: 2010年03期 页码: 269-272 栏目: 出版日期: 2010-06-20
Title:
Analysis of Influencing Factors of Snowmelt Water Infiltration into Ground in Frigid Zone
作者:
戴长雷1,2,3, 孙思淼2,3, 叶勇4
1. 哈尔滨工业大学 土木工程博士后科研流动站, 哈尔滨 150001;
2. 黑龙江大学 水利电力学院, 哈尔滨 150080;
3. 黑龙江大学 寒区地下水研究所, 哈尔滨 150080;
4. 中国水利水电科学研究院 水资源研究所, 北京 100038
Author(s):
DAI Chang-lei1,2,3, SUN Si-miao2,3, YE Yong4
1. Postdoctoral Scientific Research Station of Civil Engineering, Harbin Institute of Technology, Harbin 150001, China;
2. School of Water Conservancy & Electric-power, Heilongjiang University, Harbin 150080, China;
3. Institute of Frigid Zone Groundwater, Heilongjiang University, Harbin, 150080, China;
4. Institute of Water Resources, IWHR, Beijing 100044, China
关键词:
融雪; 入渗; 影响因素; 包气带; 寒区
Keywords:
snowmelt; infiltration; influencing factors; unsaturated zone; frigid zone
分类号:
S152.7;P941.4
摘要:
融雪入渗是寒区重要的标志性水文过程之一，其特性及影响因素对于寒区春季产汇流过程、农业灌溉及地下水模拟与利用等方面的研究都起到至关重要的作用。融雪入渗过程可以大致划分为积雪层入渗、融层入渗、冻层入渗和未冻包气带层入渗4个阶段，主要影响因素包括上述4个层位的位置规模、结构岩性、容水性质、持/给水性质、透水性质，以及其对应的积雪表面、地表面、冻层上界面、冻层下界面、地下潜水面5个界面的界面特征，同时环境影响因子对于融雪入渗过程也有一定的影响。
Abstract:
The infiltration of snowmelt water into ground, one of the most important parts and symbols of hydrologic cycle in frigid zone, is crucial to the researches on generation and confluence process of spring runoff, agricultural irrigation and groundwater simulation and management in frigid zone. It can be reduced to 4 phases: infiltration in snow cover; infiltration in soil melting layer; infiltration in soil frost layer; and infiltration in unfrozen aeration zone. Influencing factors of snowmelt water infiltration into ground can be classified into 3 types. The first are interfaces which include the snow surface, ground surface, upper bound of frost layer, below bound of frost layer and water table. The second include the situation, scale, structure, lithology characteristics, water capacity, water retention and water permeability of the 4 layers above the last are surroundings and regional factors which can also influence the process to some degree.

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备注/Memo

收稿日期:2010-2-9。
基金项目:黑龙江大学青年科学基金（QT01）；黑龙江大学博士启动基金；“十一五”国家科技支撑计划重点三级专题（2006BAB14B04-06）
作者简介:戴长雷（1978- ），男，山东郓城人，博士，副教授，主要从事寒区地下水及国际河流方向的教学及科研工作.E-mail：hydrodaichanglei@126.com

更新日期/Last Update: 1900-01-01