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[1]WANG Jingzhe,LIU Zhihui,YAO Junqiang,et al.Analysis on Variation Trends of Seasonal Runoff and Sediment Distribution and Synchronicity Change in Hutubi River[J].Research of Soil and Water Conservation,2016,23(05):152-157.

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Analysis on Variation Trends of Seasonal Runoff and Sediment Distribution and Synchronicity Change in Hutubi River

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 23 Number of periods: 2016 05 Page number: 152-157 Column: Public date: 2016-10-28

Title:: Analysis on Variation Trends of Seasonal Runoff and Sediment Distribution and Synchronicity Change in Hutubi River

Author(s):: WANG Jingzhe^1,2, LIU Zhihui^1,2,3,4, YAO Junqiang^1,2, GUO Xiaoyun^1,2; 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

Keywords:: Hutubi River; runoff and sediment; annual distribution

CLC:: P333

DOI:: -

Abstract:: We used the measured data of runoff and sediment discharge the years of Hutubi River Shimen Station in 1980—2011, and analyzed the distribution of Hutubi River sand years and synchronous change rule by using the index coefficient of inhomogeneous, manipulated for monthly and annual variation analysis assisted by using concentration (period) and other methods. The results showed that: (1) the runoff and sediment of different years follow the unimodal type distribution, the distribution and sediment discharge are more concentrated the distribution of the runoff since nearly 32 years; (2) the uneven coefficient of runoff and sediment, completely adjustment coefficient and concentration present the slowly rising trend, and interannual variability of runoff and sediment shows the good synchronicity, runoff and sediment concentration period also has a small upward trend, but the sediment concentration is slightly ahead of runoff because the river supply way and underlaying surface caused by comprehensive effect; (3) The non-uniform coefficient of sediment distribution is significantly higher than the runoff during the year. Complete adjustment coefficient and the change trend of non-uniform coefficient are basically identical. Change of runoff and sediment discharge in winter and spring is out of sync.

References:: [1] Petts G E, Bickerton M A, Crawford C, et al. Flow management to sustain groundwater-dominated stream ecosystems[J]. Hydrological Processes, 1999,13(3):497-513.
[2] Hannah D M, Smith B P G, Gurnell A M, et al. An approach to hydrograph classification[J]. Hydrological Processes, 2000,14(2):317-338.
[3] 郭巧玲,杨云松,畅祥生,等.1957-2008年黑河流域径流年内分配变化[J].地理科学进展,2011,30(5):550-556.
[4] 王金星,张建云,李岩,等.近50年来中国六大流域径流年内分配变化趋势[J].水科学进展,2008,19(5):656-661.
[5] 许全喜,童辉.近50年来长江水沙变化规律研究[J].水文,2012,32(5):38-47.
[6] 赵玉,穆兴民,何毅,等.1950-2011年黄河干流水沙关系变化研究[J].泥沙研究,2014(4):32-38.
[7] 刘晓燕,张建中,张原锋.黄河健康生命的指标体系[J].地理学报,2006,61(5):451-460.
[8] 许炯心.论黄河下游河道两次历史性大转折及其意义[J].水利学报,2001,7(1):1-7.
[9] 刘晓琼,刘彦随,李同昇,等.基于小波多尺度变换的渭河水沙演变规律研究[J].地理科学,2015,35(2):211-217.
[10] 郭爱军,黄强,畅建霞,等.基于Copula函数的泾河流域水沙关系演变特征分析[J].自然资源学报,2015,30(4):673-683.
[11] 黄英,刘新有.水电开发对河流水沙年内分配的影响分析[J].水科学进展,2010,21(3):385-391.
[12] 白东明,李卫红,郝兴明,等.新疆呼图壁河流域径流时序变化特征[J].中国水土保持科学,2008,5(3):19-23.
[13] 耿峻岭,高玲,陈建江,等.新疆呼图壁河流域水文特征分析[J].干旱区研究,2005,22(3):371-376.
[14] 魏天锋,刘志辉,姚俊强,等.呼图壁河径流过程对气候变化的响应[J].干旱区资源与环境,2015,29(4):102-107.
[15] 冯光扬.水文年内不均匀系数的探讨[J].山地学报,1991,9(1):27-32.
[16] 郑红星,刘昌明.黄河源区径流年内分配变化规律分析[J].地理科学进展,2003,22(6):585-590.
[17] 刘贤赵,李嘉竹,宿庆,等.基于集中度与集中期的径流年内分配研究[J].地理科学,2007,27(6):791-795.
[18] 李明正,庞春花,姜龙.新疆呼图壁河"96·7"洪水分析[J].新疆农垦科技,2009,32(2):73-75.

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