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首页> 外文期刊>Revista Caatinga >ABORDAGEM WEPP EM EROS?O DO SOLO PARA BACIAS HIDROGRáFICAS DO SEMIáRIDO BRASILEIRO
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ABORDAGEM WEPP EM EROS?O DO SOLO PARA BACIAS HIDROGRáFICAS DO SEMIáRIDO BRASILEIRO

机译:巴西半导体水文盆地土壤侵蚀的WEPP方法

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Soil erosion is a major environmental problem in many parts of the world and represents a serious problem for sustainable agriculture and the environment, with direct and indirect impacts on soil quality and fertility. This study aimed to use the Water Erosion Prediction Project (WEPP) model to estimate rill erosion and determine soil physical and hydraulic properties, which are essential to investigate its performance. To this end, an experiment was carried out in the Exu Creek watershed, in Serra Talhada, semi -arid region of Pernambuco State (Brazil), under increasing flow rates: T1: 5.87 L min-1; T2: 12.10 L min-1; T3: 20.33 L min1; and T4: 27.57 L min-1. Liquid and solid discharges were sampled for determination and characterization of hydraulic parameters in preformed rill flows. Reynolds numbers between 2,019 and 6,929 and Froude numbers below 1 found in this study attest to occurrence of erosive rills. Soil losses due to rill erosion increased as flow rates increased. Rill erodibility was 0.0011 kg N-1 s-1, and critical shear stress (tc) was 1.91 Pa, collapsing rill sidewalls and increasing local uplift, wet perimeter, and rill hydraulic radius.
机译:土壤侵蚀是世界许多地区的主要环境问题,对可持续农业和环境来说是一个严重的问题,对土壤质量和生育的直接和间接影响。本研究旨在利用水腐蚀预测项目(WEPP)模型来估算瑞尔腐蚀,并确定土壤物理和液压性能,这对于研究其性能至关重要。为此,在exu Creek流域中进行了一个实验,位于Pernambuco国家(巴西)的SERRA Talhada,在流量速率下,在增加的流量率:T1:5.87 L MIN-1; T2:12.10 L min-1; T3:20.33 l min1;和t4:27.57 l min-1。取样液体和固体排出,用于测定和表征在预制脊流动中的液压参数。在本研究中发现的2,019和6,929和6,929之间的雷诺数和弗劳德数证明了腐蚀性腐蚀的发生。随着流量速度的增加,由于胚胎腐蚀而导致的土壤损失增加。 RILL EroDibility为0.0011千克N-1 S-1,临界剪切应力(TC)为1.91Pa,折叠岩侧壁和增加局部隆起,湿周长和脊柱液压半径。

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