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Adsorption of tungstate on kaolinite: adsorption models and kinetics

机译:钨酸酯对高岭土的吸附:吸附模型和动力学

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摘要

The adsorption characteristics of tungstate onto kaolinite have been studied using batch experiments under ambient temperature. The effects of various operating variables, viz. , contact time, initial concentration, solution pH, ionic strength and competitive anions, have been investigated. The optimum contact time needed to reach equilibrium was found to be 48 h. Tungstate adsorption isotherms fitted well with both Langmuir and Freundlich models and the maximal adsorption capacity of the kaolinite sample is 35.54 mmol kg ~(?1) . Tungstate adsorption increases in the pH range of 3–5 and reaches a maximum at an average equilibrium pH of 4.24, but decreases from 83.7% to 10.6% as the pH increases from 5.35 to 11.03. Tungstate adsorption increases from 71.9% to 89.4% as ionic strength increases from 0.001 M to 0.1 M NaCl. As the P/W molar ratio increases from 0 to 10, tungstate adsorption decreases from 24.38 mmol kg ~(?1) to 21.61 mmol kg ~(?1) , while phosphate adsorption increases from ?2.09 mmol kg ~(?1) to 27.45 mmol kg ~(?1) . These results demonstrate that tungstate might be adsorbed onto tungstate-specific adsorption sites of the kaolinite minerals, mainly via inner-sphere complexation.
机译:在环境温度下使用批量实验研究了钨酸丁酯对高岭土的吸附特性。各种操作变量,viz的影响。已经研究了接触时间,初始浓度,溶液pH,离子强度和竞争阴离子。发现达到均衡所需的最佳接触时间为48小时。钨酸盐吸附等温线与Langmuir和Freundlich模型很好,并且高岭石样品的最大吸附能力为35.54mmol kg〜(?1)。钨酸盐吸附在3-5的pH范围内增加,并且平均平衡pH值为4.24的最大值,但由于pH从5.35增加到11.03,因此从83.7%降低至10.6%。钨酸盐吸附从71.9%增加到89.4%,因为离子强度从0.001μm增加至0.1μm。随着P / W摩尔比从0到10增加,钨酸盐吸附从24.38mmol kg〜(β1)降低至21.61mmol kg〜(?1),而磷酸盐吸附从α2.09mmolkg〜(?1)增加到27.45 mmol kg〜(?1)。这些结果表明,钨酸酮可以吸附在高岭石矿物质的钨酸盐特异性吸附位点上,主要是通过内球络络合。

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