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Effect of Mineral Systems Injected with Zinc Sulfide on Arsenite Removal from Aqueous Solution: Part II

机译:注入硫化锌的矿物系统对水溶液中亚砷脱除的影响:第二部分

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Mineral systems of kaolinite, montmorillonite, goethite and their mixtures were investigated to determine their effect on arsenite removal. Experimental studies include characterization and batch mode experiments. This study was in relation to solution composition and ageing relevant to streams and groundwater impacted by arsenic. Sorption isotherms indicated that sorption capacities of the different clay minerals, goethite and their mixtures were dependent on particle size, pH, particle concentration, arsenic concentration and residence time. Batch mode studies at room temperature revealed increase in sorption as pH was increased. All mineral systems exhibited increase in sorption as initial arsenic concentration increased. All mineral systems exhibited both promotive and non-promotive Cp effects. The complex behavior of mineral systems over the range of residence time investigated may be attributed to increased hydroxylation of the mineral surface and availability of thiol (≡S-H) and hydroxyl (≡Me-OH) functional groups and reactive sites.
机译:研究了高岭石,蒙脱石,针铁矿及其混合物的矿物体系,以确定它们对除砷的作用。实验研究包括表征和批处理模式实验。这项研究涉及与砷影响的溪流和地下水有关的溶液成分和老化。吸附等温线表明,不同粘土矿物,针铁矿及其混合物的吸附能力取决于颗粒大小,pH,颗粒浓度,砷浓度和停留时间。室温下的分批模式研究表明,随着pH值的增加,吸附量也会增加。随着初始砷浓度的增加,所有矿物质系统均表现出吸附增加。所有矿物系统均表现出促进性和非促进性​​Cp效应。矿物系统在所研究的停留时间范围内的复杂行为可能归因于矿物表面羟基化程度的提高以及硫醇(≡S-H)和羟基(≡Me-OH)官能团和反应位点的可用性。

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