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基于Budyko方程的小理河流域径流响应研究

巩瑶 莫淑红 李子龙 沈冰

西安理工大学学报2018,Vol.34Issue(4):439-446,8.
西安理工大学学报2018,Vol.34Issue(4):439-446,8.DOI:10.19322/j.cnki.issn.1006-4710.2018.04.010

基于Budyko方程的小理河流域径流响应研究

Study on runoff response in Xiaolihe basin based on Budyko equation

巩瑶 1莫淑红 1李子龙 2沈冰1

作者信息

  • 1. 西安理工大学 省部共建西北旱区生态水利国家重点实验室, 陕西 西安 710048
  • 2. 三门峡市水利勘测设计有限责任公司, 河南 三门峡 472000
  • 折叠

摘要

Abstract

The impact of environmental changes on runoff is comprehensive, and it is necessary to quantitatively distinguish the contribution of climate changes and human activities to runoff.In this paper, the precipitation, potential evapotranspiration and runoff in Xiaolihe basin were studied.The Mann-Kendall method was used to analyze the trends of the hydrometeorological elements above, the sequential clustering method and sliding Ttest were used to diagnose runoff abrupt change points, and the Budyko equation was used to quantitatively calculate the impact of climate and human activities on runoff changes.The results showed that runoff in Xiaolihe basin has a abrupt change point in 1988;compared with the multi-year average runoff depth from 1978to 1997, the annual runoff from 1998to 2010had a decrease of 7.06mm, and human activities lead to a reduce of 13.7mm, while climate changes resulted in an increase of 6.64mm.By comparing the results by the method for the sloop change ratio of cumulative quantity to Budyko equation, it is proved that both conclusions are similar, that human activities are the main reason leading to the decrease in runoff in Xiaolihe basin, and that the quantitative analysis of Budyko equation in Loess Plateau region is applicable.

关键词

气候变化/人类活动/径流响应/Budyko方程/小理河流域

Key words

climate change/human activitity/runoff response/Budyko equations/the Xiaolihe basin

分类

建筑与水利

引用本文复制引用

巩瑶,莫淑红,李子龙,沈冰..基于Budyko方程的小理河流域径流响应研究[J].西安理工大学学报,2018,34(4):439-446,8.

基金项目

国家自然科学基金资助项目(51679185) (51679185)

国家重点研发计划资助项目(2017YFC0403600) (2017YFC0403600)

西安理工大学学报

OA北大核心CSTPCD

1006-4710

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