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Study of sediment movement in an irrigated maize–cotton system combining rainfall simulations, sediment tracers and soil erosion models

机译:结合降雨模拟,沉积物示踪剂和土壤侵蚀模型研究玉米-棉花灌溉系统中的泥沙运动

摘要

Although soil erosion is one of the main threats to agriculture sustainability in many areas of the world, its processes are difficult to measure and still need a better characterization. The use of iron oxides as sediment tracers, combined with erosion and mixing models opens up a pathway for improving the knowledge of the erosion and redistribution of soil, determining sediment sources and sinks. In this study, magnetite and a multivariate mixing model were used in rainfall simulations at the micro-plot scale to determine the source of the sediment at different stages of a furrow–ridge system both with (+T) and without (–T) wheel tracks. At a plot scale, magnetite, hematite and goethite combined with two soil erosion models based on the kinematic wave approach were used in a sprinkler irrigation test to study trends in sediment transport and tracer dynamics along furrow lengths under a wide range of scenarios. In the absence of any stubble cover, sediment contribution from the ridges was larger than the furrow bed one, almost 90%, while an opposite trend was observed with stubble, with a smaller contribution from the ridge (32%) than that of the bed, at the micro-plot trials. Furthermore, at a plot scale, the tracer concentration analysis showed an exponentially decreasing trend with the downstream distance both for sediment detachment along furrows and soil source contribution from tagged segments. The parameters of the distributed model KINEROS2 have been estimated using the PEST Model to obtain a more accurate evaluation. Afterwards, this model was used to simulate a broad range of common scenarios of topography and rainfall from commercial farms in southern Spain. Higher slopes had a significant influence on sediment yields while long furrow distances allowed a more efficient water use. For the control of runoff, and therefore soil loss, an equilibrium between irrigation design (intensity, duration, water pattern) and hydric needs of the crops should be defined in order to establish a sustainable management strategy.
机译:尽管水土流失是世界许多地区对农业可持续性的主要威胁之一,但其过程难以衡量,仍然需要更好地表征。使用氧化铁作为沉积物示踪剂,并结合侵蚀和混合模型,开辟了一条途径,可增进人们对土壤侵蚀和重新分布的认识,确定沉积物来源和汇。在这项研究中,磁铁矿和多元混合模型用于微观模拟规模的降雨模拟,以确定带(+ T)轮和不带(-T)轮的垄沟系统不同阶段的沉积物来源。轨道。在地块规模上,将磁铁矿,赤铁矿和针铁矿与两种基于运动波方法的土壤侵蚀模型结合起来用于喷灌试验,以研究在各种情况下沿犁沟长度的沉积物迁移和示踪剂动力学趋势。在没有残茬覆盖的情况下,来自垄的沉积物贡献比垄床的要大,几乎达到90%,而观察到带有茬的趋势相反,来自垄的沉积物的贡献(32%)比床的贡献小。 ,在微图试验中。此外,在样地尺度上,示踪剂浓度分析显示,随着下游距离的增加,沿沟渠的沉积物脱离和来自标记段的土壤源贡献均呈指数下降趋势。已使用PEST模型估算了分布式模型KINEROS2的参数,以获得更准确的评估。之后,该模型用于模拟西班牙南部商业农场的地形和降雨的各种常见场景。较高的坡度对沉积物产量有显着影响,而较长的犁沟距离使水的利用效率更高。为了控制径流并因此控制土壤流失,应确定灌溉设计(强度,持续时间,水的模式)和农作物的需水量之间的平衡,以建立可持续的管理策略。

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