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    半干旱区不同植被类型及坡面对侵蚀性降雨的响应

    Response of different vegetation types and slopes to erosive rainfall in semi - arid regions

    • 摘要: 摘要:为研究半干旱区侵蚀性降雨与不同植被覆盖条件下坡面的产流产沙特征,本研究以兰州小青山坡面径流观测场为对象,设置10°和20°两种坡度、5种不同植被覆盖(裸地、土豆、胡麻、草地、柠条)径流小区。利用K-均值聚类法,对研究区2021年 - 2024年内55场侵蚀性降雨进行分类,并深入分析不同降雨类型下的坡面产流产沙特征,及降雨类型与坡面产流产沙的相关性。结果表明:(1)侵蚀性降雨共记录55次,占总降雨量的71.8 %;(2)侵蚀性降雨可分为四类:Ⅰ类雨型(中频率、小雨量、大雨强、短历时),Ⅱ类雨型(低频率、中雨量、小雨强、长历时),Ⅲ类雨型(高频率、中雨量、中雨强、中历时),Ⅳ类雨型(低频率、大雨量、大雨强、长历时);(3)各径流小区的产流产沙特性差异显著,裸地径流泥沙量最大,柠条、农地和草地相对较小,且20°坡面的整体产流产沙量高于10°坡面;(4)降雨量和降雨侵蚀力是影响产流产沙的主要因素,平均雨强和最大30 min雨强(I30)次之,降雨历时的影响相对较小。本研究分析了不同侵蚀性降雨类型下各类地表植被及坡度对坡面水土流失的影响,为半干旱地区开展水土保持和水土流失综合治理工作,提供了理论依据与实践参考。

       

      Abstract: Abstract:Background In semi-arid regions, soil erosion and water loss issues poses a significant threat to the sustainable development of local agriculture and forestry. Rainfall is a major influencing factor leading to soil erosion,and soil erosion caused by erosive rainfall mainly depends on factors such as rainfall amount, rainfall duration, and rainfall intensity. Therefore, studying the comprehensive impacts of different rainfall types and various governance measures on slope soil erosion and water loss is of extremely important practical significance for carrying out slope soil and water conservation work. Methods This study took the slope runoff observation field in Xiaoqingshan, Lanzhou as the research object, and sets up runoff plots with two slope gradients (10° and 20°) and five different vegetation covers (bare land, potato, flax, grassland, Caragana korshinskii ), Rainfall data and runoff-sediment production data from 2021 to 2024 were collected. Erosive rainfall was classified using the K-means clustering method, and an in-depth analysis was conducted on the characteristics and key influencing factors of slope runoff and sediment production under different rainfall types. Results (1) A total of 55 erosive rainfall events were recorded, accounting for 71.8 % of the total rainfall. (2) Erosive rainfall could be categorized into four distinct types: Type I (moderate frequency, low rainfall amount, high intensity, short duration), Type II (low frequency, moderate rainfall amount, low intensity, long duration), Type III (high frequency, moderate rainfall amount, moderate intensity, medium duration), and Type IV (low frequency, high rainfall amount, high intensity, long duration). Type IV rainfall exhibited the highest intensity, greatest erosivity, and generated the largest volumes of runoff and sediment compared to the other types. (3) Under different types of erosive rainfall, the characteristics of runoff and sediment production in each runoff plot varied significantly. The bare land had the highest runoff and sediment yields, while Caragana korshinskii -covered land, agricultural land, and grassland had relatively lower yields. Additionally, the overall runoff and sediment production on the 20° slope was higher than that on the 10° slope. (4) Rainfall amount and rainfall erosivity are the main factors influencing runoff and sediment production, followed by average rainfall intensity and maximum 30-minute rainfall intensity (I30), with rainfall duration having a relatively smaller impact. Conclusion This study analyzed the impacts of various surface vegetation types and slope gradients on slope soil erosion and water loss under different types of erosive rainfall, providing data support for the rational planning of vegetation planting and land use. and determining that rainfall amount and rainfall erosivity are the main factors influencing runoff and sediment production, providing scientific guidance for soil and water conservation work to allocate resources rationally. Overall, this study provides a theoretical basis for carrying out slope soil and water conservation work in semi-arid regions.

       

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