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Study on Soil Erosion Law of Typical Small Watershed-Luoyugou Watershed in Gully Region of the Loess Plateau

机译:黄土高原沟壑区典型小流域水平分流土壤侵蚀法研究

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The basic characteristics of soil erosion in Luoyugou Small Watershed are analyzed in this paper. Based on both methods of fixed — point observation and typical investigation, the watershed is divided into 3 erosion regions, 9 erosion types and 6 erosion belts. The soil erosion amount on slopes was measured and calculated, results of which were verified by using Universal Soil Loss Equation, and moreover, the gravity erosion amount in canals was calculated and its source was analyzed, which shows that the proportion of slope to canal of annual sediment discharge is 50:50 in the years of normal sediment output, and the ratio of output and transportation of slope, canal and gravitational erosion is 1.0, 0.47 , O. 68 and the average is 0. 68 in small watershed. Accumulative ratio of output and transportation in canal presents peak value in the trunk canal of level 4. Slope is the main source of flood and fine silt, and the canal is the centralized origin of bed load and gravitational erosion. The study provides theoretical basis for farther disclosing the law of soil erosion and water loss in the gully region of the Loess Plateau.
机译:本文分析了洛登小水域土壤侵蚀的基本特征。基于两种定点观察方法和典型调查,流域分为3个侵蚀区域,9种腐蚀类型和6个侵蚀皮带。测量并计算斜坡上的土壤腐蚀量,通过使用通用土壤损失方程验证的结果,此外,计算运河的重力腐蚀量,分析其来源,表明坡度的斜坡比例年龄沉积物排放是在正常沉积物输出的多年中的50:50,坡度,运河和引力侵蚀的输出和运输比率为1.0,0.47,O. 68和平均值为0.68分。运河输出和运输的累计比例在4级柱状管中的峰值。斜坡是洪水和细淤泥的主要来源,运河是床载荷和引力侵蚀的集中起源。该研究提供了较为披露黄土高原沟壑区土壤侵蚀和水分损失规律的理论依据。

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