首页> 外文期刊>Transactions of the ASABE >Implementation of biopore and soil fecal bacteria fate and transport routines in the Root Zone Water Quality Model (RZWQM).
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Implementation of biopore and soil fecal bacteria fate and transport routines in the Root Zone Water Quality Model (RZWQM).

机译:在根区水质模型(RZWQM)中实施生物孔和土壤粪便细菌的命运和运输程序。

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Surface runoff and infiltration are primary fecal bacteria transport mechanisms occurring in agricultural fields following manure application. The presence of macropores and biopores notably increases water infiltration, decreases surface runoff, and allows fecal bacteria and water to rapidly bypass the soil matrix during rainfall or irrigation events. This research incorporated fecal bacteria transport and biopore routines into the Root Zone Water Quality Model (RZWQM) to simulate flow and fecal bacteria transport though the soil, to subsurface drainage, and in runoff. Flow, soil fecal bacteria transport routines, and the influence of macropores and biopores on E. coli transport were evaluated based on a series of soil column experiments (28x50x85 cm) with two contrasting soil types (loamy sand and sandy loam) in which artificial, open surface connected biopores were created at two different lengths (55 cm and 65 cm). In addition, simulation of fecal bacteria transport in runoff was evaluated from a series of 2x2 m plot experiments treated with poultry litter and subjected to two rainfall storm event intensities. The new routines improved RZWQM's capability to predict rapid flow (e.g., shape of the hydrograph, time to peak, and flow breakthrough; Nash-Sutcliffe efficiency index ranged between 0.65 and 0.75 for model validation) and soil fecal bacteria transport, e.g., absolute error for the simulated event mean concentrations (EMCs) ranged between 4% and 109%. Fecal bacteria transport concentrations were underestimated in some cases, but the modified model captured the trend in concentrations observed during the soil column and plot experiments. The updated model is a simple prediction tool capable of simulating fecal bacteria transport in runoff and subsurface drainage with and without the presence of biopores.
机译:地表径流和渗透是粪肥施用后在农业领域中发生的主要粪便细菌运输机制。大孔和生物孔的存在显着增加了水的渗透,减少了地表径流,并使粪便细菌和水在降雨或灌溉事件中迅速绕过土壤基质。这项研究将粪便细菌的运输和生物孔例程纳入了根区水质模型(RZWQM),以模拟粪便细菌通过土壤,地下排水和径流的流动和粪便细菌的运输。流量,粪便中细菌的运输程序以及大孔和生物孔对 E的影响。根据一系列土壤柱实验(28x50x85厘米)对两种土壤类型(壤土和壤土)进行对比,评估了大肠杆菌的运输,其中在两个不同的长度(55厘米和55厘米)处创建了人造的,开放的表面连接的生物孔65厘米)。此外,还通过一系列用家禽垫料处理并经历了两次降雨暴雨事件强度的2x2 m地块实验评估了粪便细菌在径流中的迁移模拟。新的例程提高了RZWQM预测快速流量的能力(例如,水位图的形状,达到峰值的时间和流量突破;用于模型验证的Nash-Sutcliffe效率指数在0.65至0.75之间)和土壤粪便细菌的运输(例如,绝对误差)对于模拟事件,平均浓度(EMC)在4%至109%之间。在某些情况下,粪便细菌的运输浓度被低估了,但是修改后的模型捕获了在土壤柱和样地试验期间观察到的浓度趋势。更新后的模型是一个简单的预测工具,能够模拟有无生物孔存在时径流和地下排水中粪便细菌的运输。

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