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甘肃省白龙江径流演变特征及归因分析

李亚鹏 张文睿 孙栋元 李斌 陈学林 高国琰

水土保持通报2025,Vol.45Issue(2):232-240,9.
水土保持通报2025,Vol.45Issue(2):232-240,9.DOI:10.13961/j.cnki.stbctb.2025.02.024

甘肃省白龙江径流演变特征及归因分析

Runoff evolution characteristics and attribution analysis of Bailong River in Gansu Province

李亚鹏 1张文睿 2孙栋元 2李斌 1陈学林 3高国琰2

作者信息

  • 1. 甘肃省农村饮水安全管理办公室,甘肃兰州 730000
  • 2. 甘肃农业大学水利水电工程学院,甘肃兰州 730070
  • 3. 甘肃省陇南水文水资源勘测中心,甘肃陇南 742500
  • 折叠

摘要

Abstract

[Objective]The variability and persistence of runoff in the Bailong River,Gansu Province were comprehensively analyzed,and the contribution rates of climate change and human activities to annual runoff variations were analyzed quantitatively,in oreder to provide a theoretical basis for water resources planning and management in the Bailong River basin.[Methods]Based on annual and monthly rainfall and runoff data from Baiyun,Zhouqu,Wudu,and Bikou Stations in the Bailong River basin from 1961 to 2021,the Mann-Kendall trend test,sliding T-test,R/S analysis,and double cumulative curve method were employed to examine the evolution characteristics of runoff and identify the driving factors behind these changes.[Results]① The annual runoff at Bailong River stations exhibited a declining trend to varying degrees,with runoff losses increasing from upstream to downstream.The linear tendency rates of runoff decline were Bikou station[-3.07×108 m3/(10 a)]>Wudu station[-1.49×108 m3/(10 a)]>Zhouqu station[-4.20×107 m3/(10 a)]>Baiyun station[-3.40× 107 m3/(10 a)].② The maximum monthly runoff in the upper reaches of the Bailong River occurred in September,whereas in the middle and lower reaches,it peaked in July.Wudu station exhibited the highest extreme ratio of annual maximum runoff.③ Abrupt change points in runoff primarily occurred in 1969 and 1994,with negative change rates at all stations.This indicates that before the abrupt change,runoff was higher than the annual average,whereas after the abrupt change,it was lower.④The Hurst index(H=0.53~0.77)suggests that runoff in the middle and lower reaches of the Bailong River will continue to decline in the future.⑤ Climate change contributed 94.85%to the reduction in watershed runoff,while human activities accounted for 5.15%.[Conclusion]The runoff in the Bailong River basin has shown a significant downward trend following abrupt changes,and this trend is expected to persist in the future.

关键词

白龙江/径流量/趋势性/归因分析/甘肃省

Key words

Bailong River/runoff volume/tendency/attribution analysis/Gansu Province

分类

地球科学

引用本文复制引用

李亚鹏,张文睿,孙栋元,李斌,陈学林,高国琰..甘肃省白龙江径流演变特征及归因分析[J].水土保持通报,2025,45(2):232-240,9.

基金项目

甘肃省高等学校青年博士基金项目"疏勒河流域社会生态水文演变过程研究"(2022QB-070) (2022QB-070)

甘肃省省级生态文明建设重点研发专项(24YFFF002) (24YFFF002)

甘肃省水利科学试验研究与技术推广项目(23GSLK092) (23GSLK092)

西汉水流域水文特性研究(甘水科外发[2017]76号) (甘水科外发[2017]76号)

水土保持通报

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