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Hysteretic behavior of metolachlor adsorption-desorption in soils

机译:甲草胺在土壤中吸附-解吸的滞后行为

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摘要

Adsorption and desorption of herbicides are important processes that influence the amount of herbicide retained by the soil and that which is susceptible to runoff or movement in the soil profile. In this study, we examined the adsorption and desorption characteristics of metolachlor in two Louisiana soils: Sharkey clay and Commerce loam. Kinetic batch experiments were used for a wide range of initial concentrations and reaction times (up to 504 h), After adsorption of the metolachlor, desorption took place using successive dilution. Six consecutive desorption steps (6 day) were carried out, Metolachlor adsorption and desorption results were strongly kinetic for both soils. After the six desorption steps, the average amount of metolachlor desorbed was 30.5% for the Sharkey clay and 43.9% for the Commerce loam. The amount of metolachlor desorbed was also dependent on the initial concentration. Families of desorption isotherms were represented in two ways. The first family is based on the traditional approach, in which successive desorption isotherms are presented, The second family is time-dependent desorption isotherms, which are presented for each given reaction (adsorption plus desorption) time in a manner similar to those for adsorption isotherms, Two sets of Freundlich parameters were thus derived for the desorption isotherms, Moreover, a hysteresis coefficient, based on the difference in the area between the adsorption and desorption isotherms, was proposed. This coefficient was capable of quantifying hysteresis for both types of desorption isotherms.
机译:除草剂的吸附和解吸是重要的过程,会影响土壤中所保留的除草剂的数量以及易受径流或土壤剖面移动影响的除草剂。在这项研究中,我们检查了异丙草胺在两种路易斯安那州土壤中的吸附和解吸特性:沙基粘土和商业壤土。动力学批量实验用于广泛的初始浓度和反应时间(长达504小时)。异丙甲草胺吸附后,使用连续稀释进行解吸。进行了六个连续的解吸步骤(6天),对于两种土壤,异丙甲草胺的吸附和解吸结果均为强动力学。在六个解吸步骤之后,Sharkey黏土的平均三甲草胺解吸量为30.5%,Commerce壤土的平均解吸量为43.9%。解吸的异丙甲草胺的量还取决于初始浓度。解吸等温线的家族以两种方式表示。第一个家族基于传统方法,其中介绍了连续的解吸等温线,第二个家族是随时间变化的解吸等温线,它针对每个给定的反应时间(吸附加解吸)以与吸附等温线相似的方式表示,由此推导出两组解吸等温线的弗氏参数,并且,基于吸附和解吸等温线之间的面积差异,提出了磁滞系数。该系数能够量化两种解吸等温线的磁滞。

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