首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Variation in soil surface roughness under different land uses in a small watershed on the Loess Plateau, China
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Variation in soil surface roughness under different land uses in a small watershed on the Loess Plateau, China

机译:中国黄土高原不同土地上土壤表面粗糙度下的土壤表面粗糙度的变化

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Soil surface roughness (SSR) significantly influences hydrological and erosion processes under different conditions. Land use and its adjustment may greatly influence SSR via altering near soil surface characteristics and tillage operations, but few studies have been performed to quantify their effects on soil surface roughness. This study was conducted to investigate the variation in soil surface roughness under different land use types, and identify the main influencing factors contributing to these changes in a small watershed on the Loess Plateau, China. Eighteen sites were selected from five typical land use types (cropland, grassland, shrub land, orchard, and woodland) to measure random roughness (RR) by a photogrammetric method. The results showed that random roughness was greatly affected by land use types, plant species, and tillage operations. The mean RR under different land use types ranged from 9.47 to 10.06 mm. Woodland had the maximum RR, followed by cropland, shrub land, orchard, and grassland. For a given land use type, RR differed significantly between different plant species. The variation in random roughness was greatly influenced by the changes in near soil surface characteristics and tillage operations induced by land use adjustment. For the testing sites without tillage operations, RR increased linearly with soil median grain size, sand content, organic matter content, plant litter coverage, litter thickness, and litter density, while it decreased linearly with soil cohesion, silt content, and clay content. For the testing sites with tillage operations, RR was dominated by tillage operations. These results are helpful to understand the potential effects of vegetation restoration on hydrological and erosion processes on hillslopes in arid and semi-arid regions.
机译:土壤表面粗糙度(SSR)显着影响不同条件下的水文和腐蚀过程。土地利用及其调整可能通过改变土壤表面特征和耕作作业来极大地影响SSR,但已经进行了很少的研究以量化其对土壤表面粗糙度的影响。进行了该研究以研究不同土地利用类型下的土壤表面粗糙度的变化,并确定中国黄土高原上小流域对这些变化有助于这些变化的主要影响因素。从五种典型的土地使用类型(农田,草地,灌木土地,果园和林地)中选择了十八位点,以通过摄影测量方法测量随机粗糙度(RR)。结果表明,随机粗糙度受到土地利用类型,植物物种和耕作作业的大大影响。不同土地利用类型下的平均RR范围为9.47至10.06 mm。林地拥有最大的RR,其次是农田,灌木土地,果园和草原。对于给定的土地使用类型,RR在不同植物物种之间有显着差异。随机粗糙度的变化极大地受到土地使用调整诱导的近地表特性和耕作操作的变化。对于没有耕作操作的测试部位,RR随着土壤中间粒度,砂含量,有机物质含量,植物凋落物覆盖,凋落物厚度和凋落物密度而导致线性增加,同时它与土壤内聚力,淤泥含量和粘土含量线性降低。对于具有耕作操作的测试站点,RR以耕作操作为主。这些结果有助于了解植被恢复对干旱和半干旱地区山坡上水文和侵蚀过程的潜在影响。

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