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Kinetics of arsenic release from naturally contaminated soils at half saturation moisture by various extractants

机译:各种萃取剂在半饱和水分下自然受污染土壤的砷释放的动力学

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Kinetic studies on arsenic (As) release from soils are commonly performed using soils spiked or artificially contaminated with As at soil to solution ratios of 1:10 to 1:50 by mass, which make the conditions of study very different from the prevailing field situations. In this study, the kinetics of As release were investigated using different extractants including 1M K_2HPO_4, 0.5M Na_3C_6H_5O_7, 1M NaOH, 1M NH_4F, and 1M (NH_4)_2SO_4 in five naturally As-contaminated soils (80-1680 mg total AsAg) at half saturation moisture over a long period of time (15 min-60 d). Six kinetic models were employed to fit the data. Results indicated that the trend of As release was initially rapid followed by a slow release with K_2HPO_4, (NH_4)_2SO_4 and Na_3C_6H_5O_7 solutions, whereas with NaOH and NH_4F an increasing As release was followed by a decreasing trend at longer times, and a considerable amount of the released As was re-adsorbed or precipitated. The order of the cumulative amounts of As released by extractants was K_2HPO_4 > Na_3C_6H_5O_7 > NaOH > NH_4F > (NH_4)_2SO_4. The percentage of total As released during the reaction time was less than 3% for all extractants except K2HPO4, which was between 4.0 and 8.5% in different soils. Therefore, much lower extractability of As occurred in the naturally As-contaminated soils at half saturation moisture than has previously been reported for soils spiked or artificially contaminated with As at lower soil to solution ratios (1:10 to 1:50) suggests that caution should be exercised in extending or applying the results of As release studies on artificially contaminated soils to naturally contaminated soils for remediation purposes. Finally among six kinetic models, only the power function and the simplified Elovich models described the release data satisfactorily.
机译:砷(AS)从土壤中释放的动力学研究通常使用尖刺或人工污染的土壤以1:10至1:50质量污染的土壤进行,这使得研究的条件与现行场地截然不同。在这项研究中,使用不同的萃取剂研究了作为释放的动力学,其中包括含有1M K_2HPO_4,0.5M Na_3C_6H_5O_7,11M NaOH,1M NH_4F和1M(NH_4)_2SO_4在5个天然污染的土壤(80-1680毫克asag)半饱和水分在很长一段时间内(15 min-60d)。采用六种动力学模型来拟合数据。结果表明,作为释放的趋势最初是快速的,然后用K_2HPO_4,(NH_4)_2SO_4和NA_3C_6H_5O_7解决方案缓慢释放,而在NaOH和NH_4F随后随后随后的趋势越来越大,并且相当多的趋势作为重新吸附或沉淀的释放。萃取剂释放的累积量的顺序是K_2HPO_4> Na_3C_6H_5O_7> NaOH> NH_4F>(NH_4)_2SO_4。除K2HPO4之外的所有提取物的反应时间内释放的总量的百分比小于3%,其在不同土壤中的4.0%和8.5%之间。因此,在半饱和水分的天然污染的土壤中发生的可提取性远远低于先前据报道的刺激或人为污染的土壤,以在较低的土壤中对溶液比例(1:10至1:50)表明谨慎应在延长或申请释放研究人工污染的土壤的结果,以进行自然污染的土壤进行修复目的。最后在六种动力学模型中,只有功率功能和简化的ELOVICH模型令人满意地描述了释放数据。

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