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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Laboratory studies on glyphosate transport in soils of the Maresme area near Barcelona, Spain: transport model parameter estimation.
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Laboratory studies on glyphosate transport in soils of the Maresme area near Barcelona, Spain: transport model parameter estimation.

机译:西班牙巴塞罗那附近Maresme地区土壤中草甘膦运输的实验室研究:运输模型参数估计。

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Glyphosate ([N-phosphonomethyl] glycine) is a non-selective herbicide increasingly used in agricultural and forested lands worldwide since the 1990s. Glyphosate has limited mobility in soils due to its strong adsorption, but residues of its primary metabolite aminomethylphosphonic acid (AMPA) have been found in shallow aquifers in the Netherlands. In this laboratory study, batch and column experiments were performed using two soils collected from the Maresme area near Barcelona, Spain. Measured batch sorption isotherms for glyphosate conformed to the Freundlich model. The sorption coefficients ranged from 93 to 154, suggesting that it is strongly bound to soil. Glyphosate breakthrough curves (BTCs) measured during steady, saturated water flow in soil columns showed asymmetrical behaviour, which was attributed to nonequilibrium sorption and the presence of a sink due to irreversible sorption loss. Loss of glyphosate increased with residence times, with longer columns or with slower pore-water velocities, and breakthrough occurred earlier than predicted by retardation factors calculated from batch data. A two-site equilibrium/kinetic sorption model coupled with first-order sinks was fitted to the observed glyphosate BTCs to estimate the rate parameters for nonequilibrium sorption and irreversible sorption. The transport parameters obtained by numerical simulation suggest that glyphosate sorption is a kinetic process depending on the pore-water velocities and the residence time of soil solution..
机译:草甘膦([N-膦酰基甲基]甘氨酸)是一种非选择性除草剂,自1990年代以来在全球的农业和林地中越来越多地使用。草甘膦由于其强大的吸附能力而在土壤中的流动性受到限制,但是在荷兰的浅层含水层中发现了其主要代谢产物氨基甲基膦酸(AMPA)的残留物。在此实验室研究中,使用从西班牙巴塞罗那附近的Maresme地区收集的两种土壤进行了批处理和色谱柱实验。草甘膦的分批吸附吸附等温线符合Freundlich模型。吸附系数介于93到154之间,表明它与土壤牢固结合。在土壤柱中稳定,饱和的水流过程中测得的草甘膦穿透曲线(BTC)显示出不对称行为,这归因于非平衡吸附和由于不可逆的吸附损失而导致的水槽。草甘膦的损失随停留时间的增加,色谱柱更长或更短的孔隙水速度而增加,并且突破发生的时间早于根据批次数据计算出的阻滞因子所预测的时间。将两级平衡/动力学吸附模型与一阶吸收池相结合,拟合到观察到的草甘膦BTC上,以估算非平衡吸附和不可逆吸附的速率参数。通过数值模拟获得的传输参数表明,草甘膦的吸附是一个动力学过程,取决于孔隙水的速度和土壤溶液的停留时间。

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