首页|长冲河小流域土壤侵蚀与水文泥沙连通性分布特征及耦合关系分析

长冲河小流域土壤侵蚀与水文泥沙连通性分布特征及耦合关系分析

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[目的]为明确长冲河小流域土壤侵蚀与水文泥沙连通性的分布特征及耦合关系,为该区的水土流失治理、土壤侵蚀科学防治提供依据。[方法]通过GIS平台,采用RUSLE模型并引入连通性指数(IC)和地形湿度指数(TWI),定量评估长冲河小流域2021年的土壤侵蚀和水文泥沙连通性分布特征,探讨小流域不同坡度、土地利用、高程和坡向对不同土壤侵蚀强度、水文泥沙连通性等级的影响,并通过空间自相关分析土壤侵蚀与水文泥沙连通性的耦合关系。[结果](1)长冲河小流域平均土壤侵蚀模数为380 t/(hm2·a),土壤侵蚀强度以微度侵蚀为主,整体上由北向南逐渐加剧。(2)高水文泥沙连通性主要分布在耕地中,林草地则相反。较高值主要位于长冲河小流域坡度低、易积水的低洼平坦区域,较低值主要在陡峭山区。(3)地形因子和土地利用类型显著影响土壤侵蚀和水文泥沙连通性(p<0。01)。相对较低的土壤侵蚀强度与水文泥沙连通性等级,较高的侵蚀强度与连通性等级耕地面积占比较高,而林地和草地面积占比较小;各水文泥沙连通性等级中,5°~10°和10°~15°坡度,90。30~131。9,131。96~175。34 m高程面积占比均较多,等级越高,阳坡面积所占比例越高。(4)土壤侵蚀与水文泥沙连通性呈显著的正相关,主要体现在坡度、坡向、土地利用和高程上。[结论]提高长冲河小流域的植被覆盖度、优势度等来降低其水文泥沙连通性可以有效减少土壤侵蚀和产沙,对小流域的生态环境治理、水沙调控和水土流失科学防治等具有重要影响。
Distribution Characteristics and Coupling Relationship Between Soil Erosion and Hydrologic and Sediment Connectivity in Changchong River Basin
[Objective]To clarify the distribution characteristics and coupling relationship between soil erosion and hydrologic and sediment connectivity in Changchong River Basin,and to provide basis for soil erosion control and soil erosion prevention in this area.[Methods]By using the RUSLE model and introducing the connectivity index(IC)and topographic humidity index(TWI),the distribution characteristics of soil erosion,hydrological and sediment connectivity in the Changchong River Basin in 2021 were quantitatively evaluated by GIS platform.The effects of different slope,land use,elevation and slope direction on soil erosion intensity and hydrologic and sediment connectivity in small catchments were discussed,and the coupling relationship between soil erosion and hydrologic and sediment connectivity was analyzed through spatial autocorrelation.[Results](1)The average soil erosion modulus in the Changchong River Basin was 380 t/(hm2·a),and the soil erosion intensity was mainly slight erosion,which gradually intensified from north to south.(2)The high hydrological and sediment connectivity is mainly distributed in cultivated land,and the opposite is true in forest and grassland land.The higher value is mainly located in the low-lying flat area with low slope and easy water accumulation,while the lower value is mainly in the steep mountainous area.(3)Topographic factors and land use types significantly affected soil erosion and hydrological and sediment connectivity(p<0.01).The relatively low soil erosion intensity and hydrological and sediment connectivity levels,the higher erosion intensity and connectivity levels accounted for a higher proportion of arable land,but a smaller proportion of woodland and grassland.Among the hydrological and sediment connectivity grades,the proportion of 5°~10° and 10°~15° slope,90.30~131.96 and 131.96~175.34 m elevation area is higher.The higher the grade,the higher the proportion of sunny slope area is.(4)Soil erosion has a significant positive correlation with hydrologic and sediment connectivity,mainly reflected in slope,slope direction,land use and elevation.[Conclusion]Improving the vegetation coverage and dominance of the Changchong River Basin to reduce its hydrologic and sediment connectivity can effectively reduce soil erosion and sediment production,and has an important impact on the ecological environment management,water and sediment control,and scientific prevention and control of soil and water loss in the small watershed.

sediment connectivityhydrological connectivitysoil erosionRUSLE model

李嘉宁、张红丽、田昌园、张艺、查同刚

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北京林业大学水土保持学院,北京 100083

水利部水土保持监测中心,北京 100000

泥沙连通性 水文连通性 土壤侵蚀 RUSLE模型

2024

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2024.38(6)