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无定河输沙量变化及其原因分析

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根据无定河干流白家川、赵石窑水文站1956-2005年的年降水量、年径流量和年输沙量资料,采用线性回归分析、游程检验、Kendall秩次相关检验和Spearman秩次相关检验以及有序聚类法分析了降水、径流和输沙量的变化。结果表明:①白家川、赵石窑两站年输沙量均呈显著下降趋势,且序列中均存在趋势分量和跳跃分量;②白家川、赵石窑两站年输沙量和年径流量的变异点基本同步;③白家川、赵石窑两站累计输沙量的减幅都大于累计径流量的,而年输沙量和年径流量的相关性较强,说明输沙量受径流的影响较大;④人类活动是导致流域输沙量减少的主要因素。
Analysis of Sediment Changes and Its Reasons of the Wuding River
According to the annual precipitation,runoff and sediment discharge data of Baijiachuan and Zhaoshiyao hydrological stations in Wuding River basin from 1956 to 2005,the paper analyzed the changes of the precipitation,runoff and sediment discharge with linear regression analysis, runs test,Kendall rank correlation test,Spearman rank correlation test and orderly cluster method. The results show that:a)The annual sediment discharge of the Baijiachuan and Zhaoshiyao hydrological stations is decreased significantly and there are trend component and jump components in the sequence;b)The annual runoff and sediment discharge changes are synchronized in Baijiachuan and Zhaoshiyao hydrological stations;c)The cumulative amount of sediment yield in the Baijiachuan and Zhaoshiyao hydrological stations are significantly lower than that of the trend of the cu-mulative amount of runoff,and the the annual sediment yield and the annual runoff has a strong correlation,and shows that runoff has a great im-pact on sediment discharge;d)Human activities is the main factor of the sediment's change in Wuding River basin.

trend analysisjumping analysissediment dischargeWuding River

马雪菲、张鑫

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西北农林科技大学水利与建筑工程学院,陕西杨凌712100

趋势分析 跳跃分析 输沙量 无定河

国家“863”计划项目“十二五”国家科技支撑计划项目西北农林科技大学基本科研创新重点项目

141102092011BAD29B01Z109021202

2014

人民黄河
水利部黄河水利委员会

人民黄河

北大核心
影响因子:0.494
ISSN:1000-1379
年,卷(期):2014.(8)
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