[1]郭小云,刘志辉,姚俊强,等.天山北坡中小流域输沙量变化及其影响因素——以呼图壁河流域为例[J].水土保持研究,2016,23(01):145-149,154.
　GUO Xiaoyun,LIU Zhihui,YAO Junqiang,et al.Sediment Discharge Change and Its Affecting Factors of Small Watershed on the Northern Slope of Tianshan Mountains—Taking Hutubi River Basin as an Example[J].Research of Soil and Water Conservation,2016,23(01):145-149,154.
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天山北坡中小流域输沙量变化及其影响因素——以呼图壁河流域为例

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 23 期数: 2016年01期 页码: 145-149,154 栏目: 出版日期: 2016-02-28
Title:
Sediment Discharge Change and Its Affecting Factors of Small Watershed on the Northern Slope of Tianshan Mountains—Taking Hutubi River Basin as an Example
作者:
郭小云1,2, 刘志辉1,2,3,4, 姚俊强1,2,3, 魏天峰1,2
1. 新疆大学 资源与环境科学学院, 乌鲁木齐 830046;
2. 新疆大学 教育部 绿洲生态重点实验室, 乌鲁木齐 830046;
3. 新疆大学 干旱生态环境研究所, 乌鲁木齐 830046;
4. 干旱半干旱区可持续发展国际研究中心, 乌鲁木齐 830046
Author(s):
GUO Xiaoyun1,2, LIU Zhihui1,2,3,4, YAO Junqiang1,2,3, WEI Tianfeng1,2
1. School of Resources and Environment Science, Xinjiang University, Urumqi 830046, China;
2. Key Laboratory of Oasis Ecology, Ministry of Education, Xinjiang University, Urumqi 830046, China;
3. Institute of Arid Ecology and Environment, Xinjiang University, Urumqi 830046, China;
4. International Center for Desert Affairs-Research on Sustainable Development in Arid and Semi-arid Lands, Urumqi 830046, China
关键词:
输沙量; 径流量; 呼图壁河流域
Keywords:
sediment; runoff; Hutubi River Basin
分类号:
P333.4
摘要:
利用呼图壁河流域石门水文站1980—2011年实测日径流量、输沙量及降水量资料，采用Mann-Kendall非参数趋势和突变检验法、双累积曲线法等，研究了呼图壁河输沙量年内和年际变化趋势及可能的突变时间，并探讨了可能引起呼图壁河输沙量变化的影响因素。研究结果表明：呼图壁河流域输沙量年内分配极不均匀，连续最大4个月（6—9月）输沙量占全年输沙量的94.61%，7月输沙量最大，占全年输沙量的60.83%；1980—2011年输沙量总体呈增加趋势，年际尺度上呈丰枯相间的周期性变化，并在1989年发生了突变。输沙量受径流量、降雨量、大型水库和水土流失等综合影响，而径流量是影响输沙量的主要因素。流域干燥的气候和较低的植被覆盖率，加上人类对上游山区煤炭资源的过度开采，使得该区域山区突发暴雨洪水时，造成输沙量的剧增。
Abstract:
According to the measured daily runoff, sediment load and precipitation data of the Shimen hydrological station of Hutubi River Basin during the period from 1980 to 2011, we used the non-parametric Mann-Kendall trends and mutation test, and the double cumulative curve method to investigate Hutubi River monthly and annual sediment load trends and possible mutation time, and explore the factors that may affect Hutubi River sediment load change. The results show that Hutubi River Basin sediment distribution in a year is very uneven, continuous maximum four-month (June to September) sediment load accounted for 94.61% of annual sediment load; sediment load in July is the largest, accounting 60.83% of the annual sediment load; annual sediment load were increased during the period from 1980 to 2011, on the interannual scales it shows periodically changes of alternating wet and dry; and the mutation happened in 1989. Sediment load is influenced by the combined effects of runoff, rainfall, large reservoirs and soil erosion; runoff is the major factor affecting the amount of sediment. The watershed dry climate, low vegetation coverage and the human over exploitation of coal resources in the upper reaches of the mountain area make sediment load increase quickly in the mountainous region when the rainstorm floods occur suddenly.

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备注/Memo

收稿日期:2014-12-13;改回日期:2015-03-31。
基金项目:水利部公益性行业科研专项经费项目（201301103）
作者简介:郭小云(1991-),女,河南周口人,硕士研究生,研究方向为干旱区水文水资源研究。E-mail:guoxiaoyundili@126.com
通讯作者:刘志辉(1957-),男,新疆石河子人,博士,教授,主要从事干旱区水文水资源和决策支撑系统研究。E-mail:lzh@xju.edu.cn

更新日期/Last Update: 1900-01-01