高梯度磁选法测定土壤中重金属

R. Rikers, P. Rem, W. Dalmijn, A. Honders
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引用次数: 9

摘要

近年来,污染土壤特别是重金属污染土壤的土壤净化效率预测已成为一个重要问题。这些方法未能正确预测效率,导致了经济损失和处罚。本文介绍了一种对重金属污染土壤的传统表征方法的补充,提高了所要做出的质量基本决策。该方法是基于磁分离,使用弗朗茨等动力分离器(FIS)进行本研究。FIS分离出含有重金属的土壤颗粒,以便对这些与土壤清洁有关的颗粒进行更详细的研究。例如,对四种污染土壤进行了测试,这些土壤对土壤清洁行业来说是一个问题。实验表明,每种土壤都有自己的磁性,可以看作是一种指纹。两种土壤的密度测量结果表明,密度接近于中、高压下分离的石英密度。
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Characterization of Heavy Metals in Soil by High Gradient Magnetic Separation
In recent years forecasting soil cleaning efficiencies of polluted soil, especially those contaminated with heavy metals, has become an important issue. Failure of the methods to predict the right efficiency has resulted in financial losses and penalties. This article describes an addition to the traditional characterization methods for soils contaminated by heavy metals, improving the quality of the basic decisions to be made. The method is based on magnetic separation using a Frantz Isodynamic Separator (FIS) for this study. The FIS isolates soil particles containing heavy metals so that these particles, which are relevant for soil cleaning, can be studied in more detail. Four contaminated soils were tested, for example, soils that were a problem for the soil-cleaning industry. The experiments indicate that each soil has its own magnetic properties that should be regarded as a fingerprint. Density measurements of two soils show that densities approach the quartz density separated at moderate and high ma...
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