Different Scale Observation Sites of Snow Melt Runoff in Typical Black Soil Area

WANG Ping; LI Hao; CHEN Qiang; CHEN Shuai; XUN Jin-zhong; SONG Chun-yu; ZHANG Xing-yi

doi:10.13961/j.cnki.stbctb.2014.05.051

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Different Scale Observation Sites of Snow Melt Runoff in Typical Black Soil Area

- Different Scale Observation Sites of Snow Melt Runoff in Typical Black Soil Area
- Bulletin of Soiland Water Conservation Vol. 33, Issue 5, Pages: 244-247(2014)
- 作者机构：
  
  1. 黑龙江省水土保持科学研究所,黑龙江,哈尔滨,150070
  2. 中国科学院东北地理与农业生态研究所, 黑土生态重点实验室,黑龙江,哈尔滨,150081
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2014.05.051
  CLC：
- Published：2014
- 稿件说明：
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WANG Ping, LI Hao, CHEN Qiang, et al. Different Scale Observation Sites of Snow Melt Runoff in Typical Black Soil Area[J]. Bulletin of Soiland Water Conservation, 2014, 33(5): 244-247.
DOI：

WANG Ping, LI Hao, CHEN Qiang, et al. Different Scale Observation Sites of Snow Melt Runoff in Typical Black Soil Area[J]. Bulletin of Soiland Water Conservation, 2014, 33(5): 244-247. DOI： 10.13961/j.cnki.stbctb.2014.05.051.

摘要

通过对典型黑土区坡面、微型小流域和小流域3个尺度观测场地连续4 a的融雪监测

比较分析了融雪径流发生特征及其所占的比例。结果表明

该区融雪发生和持续时间取决于日最高气温和冬季总降雪量。降雪径流系数远大于降雨径流系数

部分年融雪径流量多于降雨径流量

坡面尺度的径流系数高于小流域尺度的径流系数。小流域的融雪径流最能代表汇入河流中的雪水量。降雪径流系数年际波动大

范围为3%~83.6%

融雪径流量占全年降水径流量的59.3%

在径流观测中不容忽视。

Abstract

The snow melt runoff in different scale observation sites of slope

mini watershed and small watershed were monitored during past four years in the typical black soil area of Northeast China. The results showed that the beginning and duration of snow melt runoff was determined by the daily maximum temperature and the amount of snowfall in the winter. The runoff coefficient of snowfall was much larger than that of rainfall

and the annual amount of snow melt runoff was even more than that of rainfall in some years. The runoff coefficient in slope scale was larger than that in watersheds. The amount of snow melt runoff in small watershed could figure out the amount of snow melt into river. The runoff coefficient of snow had a large fluctuation

from 3 percent to 83.6 percent during the past four years

and annual mean runoff of snow melt was 59.3 percent of runoff of precipitation. Hence

the snow melt runoff can not be neglected in runoff monitoring.

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references

水利部,中国科学院,中国工程院.中国水土流失防治与生态安全:东北黑土区卷[M].北京:科学出版社,2010:67-72.

周琳.中国气候丛书:东北气候[M].北京:气象出版社,1991:55.

刘海亮,蔡体久,满秀玲,等.小兴安岭主要森林类型对降雪、积雪和融雪过程的影响[J].北京林业大学学报,2012,34(2):20-25.

李华,蔡体久,盛厚才,等.凉水自然保护区雪化学特征分析[J].水土保持学报,2008,22(4):107-110.

车涛,李新.1993-2002年中国积雪水资源时空分布与变化特征[J].冰川冻土,2005,27(1):64-67.

Waldner P A, Schneebeli M.Effect of snow structure on water flow and solute transport[J]. Hydrological Processes, 2004,18(7):1271-1290.

唐克丽,史立人,史德明,等.中国水土保持[M].北京:科学出版社,2004:146-150.

Martínez-Casasnovas J A, Ramos M C, Ribes-Dasi M. Soil erosion caused by extreme rainfall events:Mapping and quantification in agricultural plots from very detailed digital elevation models[J]. Geoderma, 2002,105(1/2):125-140.

焦剑,谢云,林燕,等.东北地区融雪期径流及产沙特征分析[J].地理研究,2009,28(2):233-243.

Zuzel J F, Allmaras R R, Greenwalt R. Runoff and soil erosion on frozen soils in northeastern Oregon[J]. Journal of Soil and Water Conservation, 1982,37(6):351-354.

王鹏,穆振侠.KM河流域融雪径流与积雪面积-气温关系分析[J].水资源与水工程学报,2013,23(4):28-31.

孟令钦,李勇.东北黑土区沟蚀研究与防治[J].中国水土保持,2009(12):40-42.

范昊明,武敏,周丽丽,等.融雪侵蚀研究进展[J].水科学进展,2013,24(1):146-152.

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