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首页> 外文期刊>Water Research >GROUNDWATER CONTAMINATION DUE TO CATTLE SLURRY MODELLING INFILTRATION ON THE BASIS OF SOIL COLUMN EXPERIMENTS
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GROUNDWATER CONTAMINATION DUE TO CATTLE SLURRY MODELLING INFILTRATION ON THE BASIS OF SOIL COLUMN EXPERIMENTS

机译:基于土柱实验的牛粪泥浆模型渗入对地下水的污染

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摘要

lnfiltration into soil of contaminants present in cattle slurry was studied. Column experiments were performed in order to characterize the release of contaminants at the slurry-soil interface after surface application of slurry, with subsequent rainfall or irrigation. A gradual decrease of contaminant concentrations was observed at this interface. The shape of the release curves suggests that the release of substances from slurry can be modelled by a single-parameter release function derived from the Lapidus and Amundson solution of the convectiondispersion equation (CDE). The release process is mainly controlled by physical properties of the slurry, the soil, and their interface, on which water flow during infiltration depends. The spatial and temporal heterogeneity of water flow across the slurry-soil interface are the major causes of the observed variations in the release process between column replicates. However, good predictions of breakthrough curves (BTCs) were obtained using the release data as input for simulation of solute transport through the column. The shape of the release curve was best fitted by the release function. We compared prediction of solute transport (a) with input defined by the release function and (b) assuming rectangular-pulse input. The results show that the parameter space (soil Peclet number, release number) can be divided into two regions, one in which the assumption of rectangular pulse gives acceptable prediction of the transport through the column, and another in which this assumption is invalid.
机译:研究了牛粪中存在的污染物渗入土壤的情况。进行柱实验是为了表征表面施涂浆料后,随后的降雨或灌溉在浆料-土壤界面处污染物的释放。在该界面处观察到污染物浓度逐渐降低。释放曲线的形状表明,可以通过对流弥散方程(CDE)的Lapidus和Amundson解得到的单参数释放函数来模拟物质从浆料中的释放。释放过程主要受泥浆,土壤及其界面的物理特性控制,渗透过程中水的流动取决于该物理特性。跨泥浆-土壤界面的水流在时间和空间上的不均一性是造成色谱柱复制过程中释放过程变化的主要原因。但是,使用释放数据作为模拟溶质通过色谱柱的输入,可以获得对突破曲线(BTC)的良好预测。释放曲线的形状最适合释放功能。我们将溶质运移的预测(a)与释放函数定义的输入进行了比较,(b)假设了矩形脉冲输入。结果表明,参数空间(土壤Peclet数,释放数)可以分为两个区域,一个区域中矩形脉冲的假设给出了可接受的通过柱的传输预测,另一个区域中的该假设无效。

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