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Modelling uptake into roots and subsequent translocation of neutral andionisable organic compounds

机译:模拟对根的吸收和随后易位的中性和阴离子型有机化合物的转运

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摘要

A study on uptake of neutral and dissociating organic compounds from soil solution into roots, and their subsequent translocation, was undertaken using model simulations. The model approach combines the processes of lipophilic sorption, electrochemical interactions, ion trap, advection in xylem and dilution by growth. It needs as input data, apart from plant properties, log K-ow, pK(a) and the valency number of the compound, and pH and chemical concentration in the soil solution. Equilibrium and dynamic (steady-state) models were tested against measured data from several authors, including non-electrolytes as well as weakly acidic and weakly basic compounds. Deviations from the measured values led to further development of the model approach: sorption in the central cylinder may explain the small transpiration stream concentration factor of lipophilic compounds. For non-electrolytes, the model predicted uptake and translocation with high accuracy. For acids and bases, the tendency of the results was satisfactory. The dynamic model and the equilibrium approach gave similar results for the root concentration factor. The calculation of the transpiration stream concentration factor was more accurate with the dynamic model, but still gave deviations up to factor of ten or more. The dominating process for monovalent weak electrolytes was found to be the ion trap effect.
机译:使用模型模拟研究了从土壤溶液吸收中性和离解性有机化合物到根中以及它们随后的迁移。该模型方法结合了亲脂性吸附,电化学相互作用,离子阱,木质部中的平流和通过生长稀释的过程。除了植物特性,log K-ow,pK(a)和化合物的化合价以及土壤溶液中的pH和化学浓度外,它还需要作为输入数据。针对来自几位作者的测量数据(包括非电解质以及弱酸性和弱碱性化合物)测试了平衡和动态(稳态)模型。与测量值的偏差导致模型方法的进一步发展:中心圆柱体中的吸附可能解释了亲脂性化合物的蒸腾流小浓缩因子。对于非电解质,该模型可以高精度预测吸收和转运。对于酸和碱,结果的趋势令人满意。动态模型和平衡方法对根部浓缩因子给出了相似的结果。用动态模型对蒸腾流集中因子的计算更为准确,但仍给出了高达十倍或更大的偏差。发现一价弱电解质的主要过程是离子陷阱效应。

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