东北尼罗三角洲土壤对锰和镉的吸附特性研究

H. A. Ahmed, S. A. Abou EL-Enan, T. Mosalm, A. Hassan
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引用次数: 0

摘要

本文研究了尼罗三角洲东北部某些土壤中锰和镉的吸附特性与土壤性质之间的关系。本研究在7种不同的重粘土质地土壤剖面上进行。为了实现这一目标,我们对采集的土壤样品最重要的理化性质进行了详细的研究,然后进行了定量的特异性吸附实验。锰和镉离子在钠存在下的特异性吸附。作为一价阳离子,钙作为二价阳离子,可以看出,添加浓度越高,锰和镉的比吸附越高,由直线方程可以看出,而钠作为单阳离子的作用,由于有机质和粘土含量的存在,有利于锰和镉在表层而不是在亚表层的吸附。在钙存在的情况下,锰和镉的吸附比降低,因为钙作为二元阳离子占据了吸附复合物上的所有交换位点。然而,在钙存在的情况下,表层的吸附量比次表层的吸附量要大,这是由于表层的有机质和粘土含量比次表层高。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Specific Adsorption of Manganese and Cadmium in North East Nile Delta Soils
This study deals with the relationship between soil properties and the specific adsorption of manganese and cadmium in some soils of the north eastern Nile Delta region . This work was conducted on seven different soil profiles of heavy clay soil texture. To achieve this goal, a detailed study was conducted on the most important physical and chemical properties of the collected soil samples, then a quantitative specific adsorption experiment was carried out.The specific adsorption of manganese and cadmium ions in the presence of sodium. as a monovalent cation and calcium as a divalent cation and as shown on that the higher the added concentration, the higher the specific adsorption as shown by the straight line equation on for manganese and cadmium, while the role of Sodium as a single cation helps the adsorption of manganese and cadmium in the superficial layers rather than the sub-surface layers due to the presence of organic matter and clay content. In the presence of calcium, the specific adsorption of manganese and cadmium decreased, as calcium occupies all exchange sites on the adsorption complex as a binary cation. However in the presence of calcium The adsorption increased in the surface layers than in the sub-surface layers due to the presence of organic matter and clay content in the surface layer than the sub-surface layer.
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