| 注册
首页|期刊导航|水土保持通报|黄土高原丘陵沟壑区降雨侵蚀力的时空分布与变化趋势

黄土高原丘陵沟壑区降雨侵蚀力的时空分布与变化趋势

杨淋 张建国 张建军 张勇勇

水土保持通报2025,Vol.45Issue(2):223-231,347,10.
水土保持通报2025,Vol.45Issue(2):223-231,347,10.DOI:10.13961/j.cnki.stbctb.2025.02.023

黄土高原丘陵沟壑区降雨侵蚀力的时空分布与变化趋势

Spatiotemporal distribution and variation of rainfall erosivity in hilly and gully areas of Loess Plateau

杨淋 1张建国 2张建军 1张勇勇3

作者信息

  • 1. 中国地质大学(北京)土地科学技术学院,北京 100083
  • 2. 黄河水利委员会黄河上中游管理局,陕西西安 710021
  • 3. 中国科学院西北生态环境资源研究院,中国生态系统研究网络临泽内陆河流域研究站/中国科学院内陆河流域生态水文重点实验室,甘肃兰州 730000
  • 折叠

摘要

Abstract

[Objective]The spatial and temporal distribution characteristics and variation trend of long-term sequence rainfall erosivity in loess hilly and gully region during 1970-2020 were explored,and the main driving force of soil erosion in this region and its dynamic change law were revealed,in order to provide a useful reference for formulating regional soil and water conservation prevention and control strategies and repairing fragile Loess Plateau ecosystem.[Method]Based on the rainfall data of 67 meteorological stations in the region from 1970 to 2020,a simple algorithm model based on daily rainfall,Machisplin interpolation method,Mann-Kendall method and wavelet analysis method were used to study the abrupt change point,trend change,periodicity and spatial distribution characteristics of the time series of rainfall erosive power in the hilly and gully region of Loess Plateau in the middle reaches of the Yellow River.[Results]The average annual rainfall erosivity range in this region was 739.97~1749.03(MJ·mm)/(hm2·h),spatially decreasing from southeast to northwest.The overall erosive power of rainfall weakly increased interannually,with highest and lowest annual values of 1915.09 MJ and 741.18(MJ·mm)/(hm2·h)in 2013 and 1974,respectively.The rainfall erosivity intensity was markedly stronger in the warm season than in the cold season,with an average annual rainfall erosivity of 599.01~1742.95 and 27.61~171.11(MJ·mm)/(hm2·h),respectively.[Conclusion]The erosive power of rainfall in this area decreased from southeast to northwest,and the annual average erosive power of rainfall trended upward,but with notable interannual fluctuations.The increasing erosive power of rainfall in loess hilly and gully areas not only improves local climate conditions but also poses challenges to the stable functioning of local soil and water conservation measures and soil erosion control work.

关键词

降雨侵蚀力/时空变化/黄土丘陵沟壑区

Key words

rainfall erosivity/spatiotemporal changes/hilly-gullied loess region

分类

农业科学

引用本文复制引用

杨淋,张建国,张建军,张勇勇..黄土高原丘陵沟壑区降雨侵蚀力的时空分布与变化趋势[J].水土保持通报,2025,45(2):223-231,347,10.

基金项目

黄委优秀青年人才科技项目"黄土丘陵沟壑区土壤侵蚀模型参数本地化研究"(HQK-202303) (HQK-202303)

水土保持通报

OA北大核心

1000-288X

访问量0
|
下载量0
段落导航相关论文