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Modeling gypsifereous soil infiltration rate under different sprinkler application rates and successive irrigation events

机译:不同喷洒量和连续灌溉条件下的石膏状土壤入渗速率模拟

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The marked reduction in infiltration rate caused by formation of a soil seal due to water droplets impact on gypsifereous soil surface is a well-known phenomenon, but is rarely considered in infiltration models, especially under center-pivot irrigation systems. A simple empirical model based on the Kostiakov equation was developed. The model was applied to center-pivot irrigation system for soils with different gypsum contents [60.0 (G1), 137.6 (G2), 275.2 (G3), 314.2 (G4), and 486.0 (G5) g kg(-1)] under two sprinkler application rates (84.6 mm h(-1) for R3000 red-plate sprinkler and 47.3 mm h(-1) for R3000 orange-plate sprinkler) and eight successive irrigation events. The impacts of sprinkler droplets kinetic energy as well as specific power on soil surface sealing were evaluated also. A good agreement (P 0.05) between the measured and predicted infiltration rate values was obtained. (C) 2015 Elsevier B.V. All rights reserved.
机译:由于水滴影响到吉普赛人的土壤表面而形成的土壤封盖导致的入渗速率显着降低是一种众所周知的现象,但是在入渗模型中,尤其是在中心枢轴灌溉系统下,很少考虑到这种现象。建立了基于Kostiakov方程的简单经验模型。该模型应用于以下条件下的中心枢轴灌溉系统,该土壤具有不同的石膏含量:[60.0(G1),137.6(G2),275.2(G3),314.2(G4)和486.0(G5)g kg(-1)]两种喷头施用率(R3000红板喷头为84.6 mm h(-1),R3000橙板喷头为47.3 mm h(-1))和八次连续灌溉事件。还评估了洒水小滴动能以及比功率对土壤表面密封的影响。在测得的渗透率值和预测的渗透率值之间取得了良好的一致性(P <0.05)。 (C)2015 Elsevier B.V.保留所有权利。

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