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The adsorption of Strontium on soils developed in arid region as influenced by clay content and soluble cations

机译:受粘土含量和可溶性阳离子的干旱地区锶对干旱地区土壤的吸附

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The retention of strontium from solutions (concentration range 2 to 30 mg/l) by soils developed under arid conditions of Iran was investigated using a batch technique. Sr sorption characteristics a clayey and a silty clay loam soil were examined at room temperature and with 0.01M CaCl_2 as a background electrolyte. Sorption processes are found to show a Freundlich-type behavior. Results indicated the clay content and ionic strength play predominant role on sorption of Sr. At soil with high soluble cations (saline-sodic soil) less strontium was adsorbed at lower concentrations of strontium due to greater competition with other cations especially with soluble Ca and Mg. Electrical conductivity and ratio of soluble Ca and Mg to total soluble cations isimportant especially in soils with high EC and SAR.
机译:使用批量技术研究了在伊朗干旱条件下产生的溶液中的溶液(浓度范围为2至30mg / L)的保留。 SR吸附特性在室温下检查粘土和粉质粘土壤土土壤,用0.01M CaCl_2作为背景电解质。发现吸附过程显示Freundlich型行为。结果表明,粘土含量和离子强度对Sr的吸附作用主要作用。由于与其他阳离子更大的竞争,在较低浓度的锶上吸附了高可溶性阳离子(盐水 - 碳化土壤)的土壤中的土壤,特别是与其他阳离子的竞争较大。可溶性Ca和Mg与总称重的电导率和比例,特别是在高EC和SAR的土壤中。

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