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首页> 外文期刊>Agricultural Water Management >Runoff estimation in southern Brazil based on Smith's modified model and the Curve Number method.
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Runoff estimation in southern Brazil based on Smith's modified model and the Curve Number method.

机译:基于史密斯修正模型和曲线数法的巴西南部径流估算。

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摘要

The objective of this work was to measure and model the runoff for different soils classes at different rainfall intensities (30, 60 and 120 mm h-1) in Southern Brazil. A portable rainfall simulator with multiple nozzles was used to simulate these rainfall intensities. For each soil, the initial time and runoff rate, rainfall characteristics (total, duration and intensities), surface slope, crop residue amount and cover percentage, soil densities (bulk and particle), soil porosity (bulk, macro and micro), textural fractions (clay, silt and sand), and the initial and saturated soil water content were measured. The runoff measured was compared to Smith's modified and Curve Number (USDA-SCS) models. The cumulative runoff losses were 67, 45 and 27% of the total rainfall, for a Rhodic Paleudalf, Typic Quartzipsamment and Rhodic Hapludox, respectively. An inverse relationship was observed between initial runoff and the runoff rate, independently of the soil surface and rainfall conditions. Increasing rainfall intensity decreased the time to runoff and increased runoff rate. The Smith's modified model overestimated the cumulative runoff by about 4%. The Smith's modified model presented a better estimate for both higher and lower rainfall intensities (120 and 30 mm h-1). The SCS Curve Number model overestimated the cumulative runoff by about 34%. This large overestimate is probably due to that the model did not take into account the soil tillage system used in the field by farmers, particularly for irrigated conditions. The combination of high porosity, low bulk density and presence of crop residue on soil surface decreased runoff losses, independently of the soil texture class. Smith's modified model better estimated the surface runoff for soil with a high soil water content, and it was considered satisfactory for Southern Brazil runoff estimations. The SCS Curve Number model overestimated the cumulative runoff and its use needs adjustments particularly for no-tillage management system.
机译:这项工作的目的是测量和模拟巴西南部不同降雨强度(30、60和120 mm h -1 )下不同土壤类别的径流。使用具有多个喷嘴的便携式降雨模拟器来模拟这些降雨强度。对于每种土壤,初始时间和径流率,降雨特征(总量,持续时间和强度),表面坡度,农作物残渣量和覆盖率,土壤密度(散装和颗粒),土壤孔隙度(散装,宏观和微观),质地测量了土壤中的部分(粘土,粉砂和沙子),以及初始和饱和土壤含水量。将测得的径流与史密斯改进模型和曲线数(USDA-SCS)模型进行了比较。 Rhodic Paleudalf,Typic Quartzipsamment和Rhodic Hapludox的累积径流损失分别为总降雨量的67%,45%和27%。初始径流与径流率之间存在反比关系,与土壤表面和降雨条件无关。降雨强度的增加减少了径流时间并增加了径流率。史密斯修改后的模型高估了累积径流约4%。 Smith的修正模型对较高和较低的降雨强度(120和30 mm h -1 )都提供了更好的估计。 SCS曲线数模型高估了累积径流约34%。如此高估可能是由于该模型未考虑农民在田间使用的土壤耕作系统,特别是在灌溉条件下。高孔隙率,低堆密度和土壤表面农作物残渣的结合降低了径流损失,而与土壤质地类别无关。 Smith的修正模型可以更好地估算土壤含水量较高的土壤的地表径流,并且认为巴西南部的径流估算令人满意。 SCS曲线数模型高估了累积径流,尤其是对于免耕管理系统,其使用需求需要进行调整。

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