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Adsorption characteristics of Ariake clays to Chromium and the effect of pH-value

机译:Ariake粘土对铬的吸附特性及pH值的影响

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Adsorption characteristics of two Ariake clays (Clay-1 and Clay-2) to chromium were investigated by batch contact tests and advection-diffusion column tests. A strong non-linear adsorption isotherm was observed from batch contact test results. When the concentration of the solution is larger than a few ppm, the amount of adsorbed chromium almost became a constant. This non-linear adsorption characteristic has been confirmed by analyzing the advection-diffusion column test results. The analysis results also revealed that the adsorption process of Ariake clays to chromium is irreversible or only partially reversible. The pH-value of the solution has a strong effect on the adsorption capacity. Reducing pH-value increases the adsorption capacity significantly, especially for pH-value from 8 to 7. Soil-to-solution ratios of 1:4, 1:10 and 1:20 were adopted to investigate the effect of soil-to-solution ratio on the adsorption characteristics. It is tentatively concluded that for the range tested, soil-to-solution ratio does not have a significant effect on the adsorption capacity of Ariake clays.
机译:通过间歇接触试验和对流扩散柱试验研究了两种Ariake粘土(Clay-1和Clay-2)对铬的吸附特性。从批量接触测试结果中观察到强烈的非线性吸附等温线。当溶液的浓度大于几ppm时,铬的吸附量几乎变为恒定。通过分析对流扩散柱的测试结果,可以确认这种非线性吸附特性。分析结果还表明,Ariake粘土对铬的吸附过程是不可逆的或仅是部分可逆的。溶液的pH值对吸附容量有很大影响。降低pH值可显着提高吸附能力,尤其是pH值从8增至7时。采用土壤与溶液的比例为1:4、1:10和1:20来研究土壤与溶液的作用比例对吸附特性的影响。初步得出结论,在所测试的范围内,土壤与溶液的比例对Ariake粘土的吸附能力没有显着影响。

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