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Modeling water flow and bacterial transport in undisturbed lysimeters under irrigations of dairy shed effluent and water using HYDRUS-1D

机译:使用HYDRUS-1D在灌溉牛奶场废水和水的情况下在不受干扰的测渗仪中模拟水流量和细菌迁移

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摘要

HYDRUS-1D was used to simulate water flow and leaching of fecal coliforms and bromide (Br) through six undisturbed soil lysimeters (70 cm depth by 50 cm diameter) under field conditions. Dairy shed effluent (DSE) spiked with Br was applied to the lysimeters, which contained fine sandy loam layers. This application was followed by fortnightly spray or flood water irrigation. Soil water contents were measured at four soil depths over 171 days, and leachate was collected from the bottom. The post-DSE period simulations yielded a generally decreased saturated water content compared to the pre-DSE period, and an increased saturated hydraulic conductivity and air-entry index, suggesting that changes in soil hydraulic properties (e.g. via changes in structure) can be induced by irrigation and seasonal effects. The single-porosity flow model was successful in simulating water flow under natural climatic conditions and spray irrigation. However, for lysimeters under flood irrigation, when the effect of preferential flow paths becomes more significant, the good agreement between predicted and observed water contents could only be achieved by using a dual-porosity flow model. Results derived from a mobile-immobile transport model suggest that compared to Br, bacteria were transported through a narrower pore-network with less mass exchange between mobile and immobile water zones. Our study suggests that soils with higher topsoil clay content and soils under flood irrigation are at a high risk of bacteria leaching through preferential flow paths. Irrigation management strategies must minimize the effect of preferential flow to reduce bacterial leaching from land applications of effluent.
机译:HYDRUS-1D用于模拟田间条件下通过六个未扰动土壤溶渗仪(深度70厘米,直径50厘米)的粪便大肠菌群和溴化物(Br)的水流和淋滤。将掺有溴的乳制品废水(DSE)应用于渗漏计,该渗漏计包含细砂壤土层。每两周进行一次喷洒或洪水灌溉。在171天的时间里,在四个土壤深度处测量了土壤含水量,并从底部收集了渗滤液。与DSE之前的时期相比,DSE以后的时期模拟产生的饱和水含量通常降低,并且饱和的水力传导率和空气进入指数增加,这表明可以引起土壤水力特性的变化(例如,通过结构的变化)受灌溉和季节影响。单孔渗流模型成功地模拟了自然气候条件和喷灌条件下的水流。但是,对于洪水灌溉下的渗漏计,当优先流动路径的影响变得更加显着时,只有通过使用双孔隙度流动模型才能实现预测含水量与观测含水量之间的良好一致性。流动不动的运输模型得出的结果表明,与Br相比,细菌通过较窄的孔网运输,流动和不动水区之间的质量交换较少。我们的研究表明,表土粘土含量较高的土壤和洪水灌溉下的土壤极有可能通过优先流动路径浸出细菌。灌溉管理策略必须最大程度地减少优先流量的影响,以减少从土地应用废水中产生的细菌浸出。

著录项

  • 来源
    《Water Research》 |2010年第4期|1050-1061|共12页
  • 作者单位

    Faculty of Agriculture and Life Sciences and CSEQ, PO Box 84, Lincoln University, Lincoln 7647, Canterbury, New Zealand;

    Institute of Environmental Science & Research, PO Box 29-181, Christchurch, New Zealand;

    Faculty of Agriculture and Life Sciences and CSEQ, PO Box 84, Lincoln University, Lincoln 7647, Canterbury, New Zealand;

    Department of Environmental Sciences, University of California Riverside, CA, USA;

    Faculty of Agriculture and Life Sciences and CSEQ, PO Box 84, Lincoln University, Lincoln 7647, Canterbury, New Zealand;

    Institute of Environmental Science & Research, PO Box 29-181, Christchurch, New Zealand;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    modeling; dual porosity; bacterial transport; undisturbed lysimeter;

    机译:造型;双重孔隙细菌运输;不受干扰的测渗仪;
  • 入库时间 2022-08-17 13:49:30

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