[1]孙洋洋,穆兴民,高鹏,等.黄河上中游区径流量格局长期变化过程[J].水土保持研究,2017,24(03):59-64,69.
　SUN Yangyang,MU Xingmin,GAO Peng,et al.Temporal Changes in Runoff in the Upper and Middle Reaches of Yellow River[J].Research of Soil and Water Conservation,2017,24(03):59-64,69.
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黄河上中游区径流量格局长期变化过程

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 24 期数: 2017年03期 页码: 59-64,69 栏目: 出版日期: 2017-06-28
Title:
Temporal Changes in Runoff in the Upper and Middle Reaches of Yellow River
作者:
孙洋洋1, 穆兴民2,3, 高鹏2,3, 赵广举2,3, 孙文义2,3
1. 西北农林科技大学 水利与建筑工程学院, 陕西 杨凌 712100;
2. 西北农林科技大学 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨凌 712100;
3. 中国科学院 水利部 水土保持研究所, 陕西 杨凌 712100
Author(s):
SUN Yangyang1, MU Xingmin2,3, GAO Peng2,3, ZHAO Guangju2,3, SUN Wenyi2,3
1. College of Water Resources and Architectural Engineering, Northwest A & F University, Yangling, Shaanxi 712100, China;
2. Institute of Soil and Water Conservation, Northwest A & F University, Yangling, Shaanxi 712100, China;
3. Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China
关键词:
径流; 变化趋势; 集中性; 不均匀性; 黄河上中游
Keywords:
runoff; variation trend; concentration; inhomogeneity; the upper and middle reaches of the Yellow River
分类号:
TV121.4
摘要:
河川径流不仅是水资源重要的构成部分，也是自然界中水分循环的重要环节，径流量的变化直接影响区域特别是干旱区水资源的开发利用。基于黄河中游上中下三个站点（河口镇站、吴堡站以及三门峡站）1919—2013年月径流量资料，采用Spearman相关法、有序聚类法等方法分析黄河不同区间年、月径流量演变规律，揭示年径流量突变前后径流量年内集中度和不均匀性差异。结果表明：黄河上游和中游径流量因人类活动作用具有明显趋势性减小，而因气候作用表现出显著的阶段性。在径流量突变年份后，黄河上游径流量上游集中度降低，不均匀度减小，径流量年内分配趋于均匀，但黄河中游地区径流量年季不均匀性反而增大。
Abstract:
Runoff is the important water resource and element of hydrologic cycle. The change of runoff directly affects the exploitation and utilization of water resources. Based on the data of monthly runoff from 1919 to 2013 of the three sites (Heleouzhen station, Wubu station and Sanmenxia station) in the middle reaches of the Yellow River, we used modern statistical analysis methods such as Spearman correlation, Mann-Kendall rank test, sequential clustering method, to reveal the change of concentration and inhomogeneity about runoff.The results showed that the runoff of upstream and middle reaches of the Yellow River has reduced because of human activity. Meanwhile the climate impact on the runoff showed the significant stage. After runoff mutation, the concentration and inhomogeneity of runoff in the upper reaches of the Yellow River have reduced, and distribution of runoff tends to be more uniform, but inhomogeneity of runoff in the middle reaches of the Yellow River increases instead.

参考文献/References:

[1] 王彦君,王随继,苏腾.1955-2010年松花江流域不同区段径流量变化影响因素定量评估[J].地理科学进展,2014,33(1):65-75.
[2] 杨立哲,钱虹,郝璐.锡林河近50年径流变化特征及其影响因素分析[J].草业科学,2015,32(3):303-310.
[3] 蓝永超,丁永建,沈永平,等.气候变化对黄河上游水资源系统影响的研究进展[J].气候变化研究进展,2005,1(3):122-125.
[4] 穆兴民,王万忠,高鹏,赵广举.黄河泥沙变化研究现状与问题[J].人民黄河,2014,36(12):1-7.
[5] 穆兴民,李靖,王飞,等.黄河天然径流量年际变化过程分析[J].干旱区资源与环境,2003,17(2):1-5.
[6] 李二辉,穆兴民,赵广举.1919-2010年黄河上中游区径流量变化分析[J].水科学进展,2014,25(2):155-163.
[7] 毕彩霞,穆兴民,赵广举,等.渭河流域气候变化与人类活动对径流的影响[J].中国水土保持科学,2013,11(2):33-38.
[8] Sato Yoshinobu, Ma Xieyao, Matsuoka Masayuki.黄河中游长时段水量平衡分析[C]//骆向新,尚宏琦.第三届黄河国际论坛论文集郑州:黄河水利出版社,2007.
[9] 赵玉,穆兴民,何毅,蒋冲.1950-2011年黄河干流水沙关系变化研究[J].泥沙研究,2014(4):32-38.
[10] 姚文艺,冉大川,陈江南.黄河流域近期水沙变化及其趋势预测[J].水科学进展,2013,24(5):607-616.
[11] Ran L S, Wang S J, Fan X L. Channel change at Toudaoguai station and its responses to the operation of upstream reservoirs in the upper Yellow River[J]. Journal of Geographical Sciences, 2010,20(2):231-247.
[12] 普发贵. Mann-Kendall检验法在抚仙湖水质趋势分析中的应用[J].环境科学导刊,2014,33(6):83-87.
[13] 梁艳琴.横山岭水库流域径流量变化趋势及成因分析[J].河北工程技术高等专科学校学报,2014(1):4-7,20.
[14] 汤奇成,程天文,李秀云.中国河川月径流的集中度和集中期的初步研究[J].地理学报,1982,37(4):383-393.
[15] 刘德林,刘贤赵,张继平.大沽夹河流域径流年内分配特征的量化研究[J].水土保持研究,2006,13(6):107-114.
[16] 徐东霞,章光新.嫩江径流年内变化特征分析[J].干旱区资源与环境,2009,23(7):48-51.
[17] 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.
[18] 赵广举,穆兴民,田鹏,等近60年黄河中游水沙变化趋势及其影响因素分析[J].资源科学,2012,34(6):1070-1078.
[19] 穆兴民,徐学选,陈霁巍.黄土高原生态水文研究[M].北京:中国林业出版社,2001.
[20] 范利杰,穆兴民,赵广举,等近50a嘉陵江流域径流变化特征及影响因素[J].水土保持通报,2013,33(1):12-17.
[21] 马柱国.黄河径流量的历史演变规律及成因[J].地球物理学报,2015,48(6):1270-1275.
[22] 渭河流域水资源规划[R].郑州:水利部黄河水利委员会勘测规划设计研究院,2003:32-35.

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　Wang Yuke,Li Li,Fu Zuo,et al.A STUDY ON THE BENEFIT OF SOIL AND WATER CONSERVATION FOR ENERGY FOREST[J].Research of Soil and Water Conservation,1992,(03):70.
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　Shi Shengxin,Jiang Dingsheng.Impacts of Several Soil and Water Conservation Measures on Strengthening Rainfall infiltration and Reducing Sediment Yield[J].Research of Soil and Water Conservation,1994,1(03):82.
[8]曹全意.黄土高原地区提高山坡地径流利用率的有效途径[J].水土保持研究,1998,5(04):31.
　Cao Quanyi.The Effective Way to Raise the Runoff Use Ratein Slope Land of Loess Plateau[J].Research of Soil and Water Conservation,1998,5(03):31.
[9]赵晓光,吴发启.坡面水蚀过程的力能体系及研究思路[J].水土保持研究,2000,7(01):23.
　ZHAO Xiao-guang,WU Fa-qi.Research Frame for Force and Energy System in Water Erosion Process in Slopes of Gully[J].Research of Soil and Water Conservation,2000,7(03):23.
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　MAO Xuesen,LIU Changming.Ground Water Changing Trends and Agriculture Sustainable Development in Taihang Mountain-foot Plain of North China[J].Research of Soil and Water Conservation,2001,8(03):147.
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　HU Hai-ying,HUANG Guo-ru,HUANG Hua-mao.Variation of Runoff at Tieling Station of Liaohe River Basin and Its Influence Factors[J].Research of Soil and Water Conservation,2013,20(03):98.

备注/Memo

收稿日期:2016-09-04;改回日期:2016-10-08。
基金项目:国家重点研发计划“黄河流域水沙多时空演变及其分异规律”（2016YFC0402240701）
作者简介:孙洋洋(1990-),女,山东枣庄人,硕士研究生,主要从事生态水文及水土保持研究。E-mail:yysun@nwsuaf.edu.cn
通讯作者:穆兴民(1961-),男,陕西华阴人,研究员,博士生导师,主要从事水土保持、生态水文方面的研究工作E-mail:xmmu@ms.iswc.ac.cn

更新日期/Last Update: 1900-01-01