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Adsorption of arsenic on soil under different soil moisture conditions

机译:不同土壤水分条件下砷在土壤上的吸附

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摘要

The adsorption study was conducted on three Japanese soils with different soil properties to characterize the adsorption pattern of Arsenic (As). Double tube method was used to find out the effect of soil moisture levels on As adsorption. For this study, besides double tube method, conventional batch method also was used. The As adsorption showed two phase kinetics. An initial and rapid adsorption was found at first hour and then gradually preceded before equilibrium in all the three soils in the case of double tube method and in clay loam and light clay soil in the case of batch method. Adsorption seemed to reach equilibrium at 24 h in both methods, though the initial adsorbate load was not the same at the same applied concentration in the methods. Adsorption activity differed according to soil and as well as to the methods. The highest adsorption was found in clay loam soil followed by light clay and sandy loam soil. The linear model of Freundlich adsorption was found better fitted in the case of double tube method than batch method. Suggesting that, under the experimental conditions stated here, the double tube method is more appropriate to describe the adsorption of As in the three Japanese soils under normal field condition. The concentration of As in soil water was slightly increased at different moisture levels from 50%-80% which may contribute significantly to the bioavailability of As at the moisture level below maximum filed capacity.
机译:在三种具有不同土壤特性的日本土壤上进行了吸附研究,以表征砷(As)的吸附模式。采用双管法研究土壤水分水平对砷吸附的影响。对于这项研究,除了双管法外,还使用了常规的分批法。 As吸附显示出两相动力学。在开始的第一个小时发现了最初的快速吸附,然后在双管方法下在所有三种土壤中逐渐达到平衡之前逐渐吸收,而在分批方法下在粘土壤土和轻质粘土中逐渐开始吸附。两种方法的吸附似乎都在24 h达到平衡,尽管在相同的应用浓度下初始吸附物负荷并不相同。吸附活性随土壤和方法的不同而不同。在粘土壤土中吸附率最高,其次是轻质粘土和沙质壤土。发现双管法比批次法更好地拟合了Freundlich吸附的线性模型。这表明,在本文所述的实验条件下,双管法更适合描述正常田间条件下三种日本土壤中As的吸附。在水分含量从50%-80%不​​同的情况下,土壤水中的砷浓度略有增加,这可能会在水分含量低于最大填充量时显着提高砷的生物利用度。

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