首页 | 本学科首页   官方微博 | 高级检索  
     

黄土高原典型流域河川径流水文情势变化及其归因分析
引用本文:张舒羽,赵广举,穆兴民,田鹏,高鹏,孙文义. 黄土高原典型流域河川径流水文情势变化及其归因分析[J]. 水土保持通报, 2021, 41(4): 1-8
作者姓名:张舒羽  赵广举  穆兴民  田鹏  高鹏  孙文义
作者单位: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;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;中国科学院 水利部 水土保持研究所, 陕西 杨凌 712100;西北农林科技大学 资源与环境学院, 陕西 杨凌 712100
基金项目:国家重点研发计划项目“黄河水沙变化机理与趋势预测”(2016YFC0402401);国家自然科学基金项目(42077076;42077075);中国科学院“西部之光”项目(XAB2017A03)
摘    要:[目的]分析黄土高原典型流域河川径流水文情势变化及其原因,为该区域水土保持与水资源高效利用提供科学支撑.[方法]选取渭河支流散渡河与无定河支流大理河为研究区,利用甘谷站和绥德站1965-2018年的气象水文资料,采用线性回归、Mann-Kendall检验、累积距平和双累积曲线法分析散渡河和大理河的径流变化特征及其驱动因...

关 键 词:黄土高原  河川径流  水文变化指标  RVA法  水土保持  驱动因素
收稿时间:2021-03-28
修稿时间:2021-04-25

Hydrologic Regime Change and Its Attribution Analysis of River Runoff in Typical Watershed on Loess Plateau
Zhang Shuyu,Zhao Guangju,Mu Xingmin,Tian Peng,Gao Peng,Sun Wenyi. Hydrologic Regime Change and Its Attribution Analysis of River Runoff in Typical Watershed on Loess Plateau[J]. Bulletin of Soil and Water Conservation, 2021, 41(4): 1-8
Authors:Zhang Shuyu  Zhao Guangju  Mu Xingmin  Tian Peng  Gao Peng  Sun Wenyi
Affiliation:State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China;State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, Shaanxi 712100, China;Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling, Shaanxi 712100, China;College of Resource and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China
Abstract:[Objective] The hydrologic regime change in typical watershed on Loess Plateau was studied, and its attribution analysis was carried out, in order to provide scientific support for soil and water conservation and efficient utilization of water resources in different regions of the Loess Plateau. [Methods] Sandu River (a tributary of Weihe River) and Dali River (a tributary of Wuding River) were selected as the study areas, and the traits in variations of streamflow and their driving factors from 1965 to 2018 were analyzed based on meteorological and hydrological data at Gangu and Suide hydrological stations by using the linear regression, Mann-Kendall test, accumulated anomaly, and double mass curve methods. The improved range of variability approach was employed to analyze the impact of the hydrological alterations in different river by soil and water conservation dominated by terracing and damming. [Results] The annual runoff showed significant decreasing trends(p<0.01) and the abrupt changes occurred in around 1990s in Sandu River and Dali River. The alteration degree of runoff in Sandu River was high (90.12%) and in Dali River was moderate (60.66%) calculated by the improved range of variability approach (RVA) method. Among 32 indicators of hydrologic alteration (IHA), the rise and fall rate of flow were affected most significantly. [Conclusion] In the Sandu River (dominated by terracing), both the magnitude of monthly median flow and the annual minimum flow decreased dramatically, timing of annual minimum flow delayed and duration of low pulses increased. In the Dali River (dominated by damming), the magnitude of monthly median flow depended on the seasonal alteration. The annual 1-day and 3-day minimum flow increased and frequency of low pulses declined.
Keywords:Loess Plateau  river runoff  indicators of hydrologic alteration (IHA)  range of variability approach (RVA)  soil and water conservation  driving factors
点击此处可从《水土保持通报》浏览原始摘要信息
点击此处可从《水土保持通报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号