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Measurement of Sorption Isotherms with Flow-Through Reactors

机译:用流通式反应器测量吸附等温线

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摘要

Asimpleflow-through reactortechnique is described for measurements of sorption isotherms on solid environmental materials such as soils, crushed rocks, aquifer materials, or peat. The applicability of the method was established by determining copper sorption isotherms at effectively constant pH for two different soil samples. The experimental results compare favorably with independent batch and column studies. Potential advantages of the flow-through technique are exemplified by studying the sorption behavior of one soil sample that shows in batch experiments a pronounced dependence on the solid concentration (particle concentration effect). Comparison of these results with the flow-through reactor technique and independent column experiments confirms unequivocally that in this case the influence of the solid concentration is an artifact due to insufficient prewashing of the soil with the background electrolyte solution and has nothing to do with the shaking process in batch experiments. The present results indicate that incomplete removal of preadsorbed ions may often represent a major source of error in sorption studies and may be difficult to recognize in batch experiments.
机译:描述了Asimpleflow-through反应器技术,用于测量固体环境材料(例如土壤,碎石,含水层材料或泥炭)上的吸附等温线。该方法的适用性是通过确定两个不同土壤样品在有效恒定pH下的铜吸附等温线确定的。实验结果与独立的批处理和色谱柱研究相比具有优势。通过研究一种土壤样品的吸附行为,可以举例说明流通技术的潜在优势,该特性在分批实验中显示出对固体浓度(颗粒浓度效应)的明显依赖性。将这些结果与流通式反应器技术和独立柱实验的比较清楚地证实,在这种情况下,固体浓度的影响是人为因素,这是由于用背景电解质溶液对土壤进行的预洗不足,并且与晃动无关分批实验过程。目前的结果表明,不完全去除预吸附离子可能经常是导致吸附研究错误的主要根源,并且在批量实验中可能难以识别。

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