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降雨类型对砒砂岩区不同土地利用类型坡面产流产沙的影响OA

Impacts of rainfall types on slope runoff and sediment yield under different land use types in Pisha sandstone area

中文摘要英文摘要

[目的]探明砒砂岩区天然降雨条件下不同土地利用类型坡面产流产沙特征,为该区水土流失防控和流域生态综合治理工作提供理论和数据支撑.[方法]以内蒙古伊金霍洛旗砒砂岩区小流域为研究区,基于该区2018-2023年天然降雨产流产沙观测数据,对该区降雨类型进行划分,研究天然降雨特征与不同地类产流产沙量的关系,以降雨特征和坡度建立不同地类产流产沙模型.[结果]①降雨类型可划为3类.Ⅰ类降雨为短历时中雨,是研究区主要的降雨形式,占降雨总次数的 80.6%;Ⅱ类降雨为中历时大雨,降雨发生频率较低,占降雨总次数的18.6%;Ⅲ类降雨为长历时中雨,发生频率最低,占降雨总次数的0.8%;Ⅰ型和Ⅱ型降雨分别占研究区坡面径流总量的39%和40%,是研究区坡面径流的主要来源.Ⅰ型降雨占研究区坡面产沙总量的81%,是研究区坡面产沙的主要来源;②不同雨型下,5º和10º坡面产沙规律整体呈:Ⅰ型降雨>Ⅱ型降雨>Ⅲ型降雨的规律,产流规律整体呈:Ⅱ型降雨>Ⅰ型降雨>Ⅲ型降雨的规律.15º坡面产流产沙规律整体呈:Ⅰ型降雨>Ⅱ型降雨>Ⅲ型降雨的规律.不同地类坡面产流产沙规律整体呈:裸地>耕地>草地>林地的规律.[结论]土地利用类型和坡度的交互作用是影响Ⅰ型降雨产流量的主要因素;土地利用类型、坡度单因素和交互作用对Ⅱ型降雨产流产沙量均有影响;土地利用类型是影响Ⅲ型降雨产流量的主要因素.构建的不同土地利用类型下降雨与产流产沙量模型,可运用于砒砂岩不同土地利用类型土壤侵蚀模拟研究.

[Objective]The characteristics of slope runoff and sediment yield of different land use types under natural rainfall conditions in the Pisha sandstone area were explored,in order to provide theoretical and data support for the prevention and control of soil erosion and the comprehensive ecological management of watersheds in this area.[Methods]Taking the small watershed of the Pisha sandstone area in Yijinhuoluo Banner of Inner Mongolia as a study area,based on the observation data of natural rainfall runoff and sediment yield in this area from 2018 to 2023,the rainfall types in this area were classified,the relationship between natural rainfall characteristics and runoff and sediment yield of different land use types was analyzed,and the runoff and sediment yield models of different land use types were established based on rainfall characteristics and slope gradient.[Results]① The rainfall types were classified into three categories.Type Ⅰ rainfall was short-duration moderate rainfall,which was the dominant rainfall type in the study area,accounting for 80.6%of the total rainfall events.Type Ⅱ rainfall was medium-duration heavy rainfall,with a relatively low frequency,accounting for 18.6%of the total rainfall events.Type Ⅲ rainfall was long-duration moderate rainfall,with the lowest frequency,accounting for 0.8%of the total rainfall events.Type Ⅰ and Type Ⅱ rainfall accounted for 39%and 40%of the total slope runoff in the study area,respectively,serving as the main sources of slope runoff.Type Ⅰ rainfall accounted for 81%of the total slope sediment yield in the study area,which was the main source of slope sediment yield.② Under different rainfall types,the sediment yield patterns on 5° and 10° slopes followed the overall order of Type Ⅰ rainfall>Type Ⅱ rainfall>Type Ⅲ rainfall,while the runoff patterns followed the order of Type Ⅱrainfall>Type Ⅰ rainfall>Type III rainfall.The runoff and sediment yield patterns on a 15° slope both followed the order of Type I rainfall>Type Ⅱ rainfall>Type Ⅲ rainfall.For different land use types,the slope runoff and sediment yield patterns of different land types ranked as bare land>cultivated land>grassland>forest land.[Conclusion]The interaction between land use type and slope gradient was the main factor affecting the runoff yield of Type Ⅰ rainfall.The single factor and interaction of land use type and slope gradient both had an effect on runoff and sediment yield under Type Ⅱ rainfall.Land use type was the main factor affecting runoff under Type Ⅲ rainfall.The established models of rainfall and corresponding runoff and sediment yield of different land use types can be applied to soil erosion simulation studies for different land use types in Pisha sandstone area.

张雨佳;杨振奇;王鑫;郭建英;王小雪;李云;马海龙;张志军

水利部 牧区水利科学研究所,内蒙古 呼和浩特 010020水利部 牧区水利科学研究所,内蒙古 呼和浩特 010020水利部 牧区水利科学研究所,内蒙古 呼和浩特 010020水利部 牧区水利科学研究所,内蒙古 呼和浩特 010020伊金霍洛旗水利事业发展中心,内蒙古 鄂尔多斯 017299鄂尔多斯市水利事业发展中心,内蒙古 鄂尔多斯 017002呼和浩特市林业和草原保护中心,内蒙古 呼和浩特 010055康巴什区林业和草原事业发展中心,内蒙古 鄂尔多斯 017299

农业科技

砒砂岩区坡面产流产沙土地利用类型天然降雨

Pisha sandstone areaslope runoff and sediment yieldland use typenatural rainfall

《水土保持通报》 2026 (3)

32-40,96,10

鄂尔多斯市水利科技项目"重点水土流失区生态系统(西黑岱流域)水土保持综合整治技术集成效益评估项目"(MK22205031)内蒙古自治区"科技兴蒙"行动重点专项(2022EEDSKJXM003)中国水利水电科学研究院基本科研业务费专项(MKYW2024JK002)内蒙古自治区"英才兴蒙"工程青年拔尖人才专项培养计划项目

10.13961/j.cnki.stbctb.2026.03.011

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