[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.

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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