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Evaluation of ions retention capacity of a residual soil of Rio de Janeiro, Brazil

机译:巴西里约热内卢残留土壤的离子保留能力评估

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The paper presents the results of laboratory experiments investigating the cation and anion sorption parameters of a saprolitic residual soil from the State of Rio de Janeiro. The soil is a sandy silt with 58% of fines (%<#200 ASTM sieve), and a plasticity index Ip of 29%. The soil clay fraction is constituted by kaolinite, goethite and traces of vermiculite, and the soil is representative of the materials used for construction of liners at various industrial and domestic wastes disposal sites in Rio de Janeiro. The soil was completely characterized, including the determination of the physical and geotechnical index properties, minera-logical composition, and physico-chemical parameters such as the Cation Exchange Capacity (CEC), the soil natural pH and the Zero Point of Charge pH (ZPC), the exchangeable complex composition and the organic matter content. Distinct series of Batch tests were performed to investigate the soil sorption behaviour relative to the ions K~+, Cl~- and phosphate (occurring primarily as HPO_4~(2-)), at two pH levels, 2.5 and 6.5. The soil Zero Point of Charge is around 3.5, close to the kaolinite typical value. The residual soil sorption behaviour was also compared to pure kaolinite, goethite and hematite samples measured sorption patterns for the phosphate ion at the same pH conditions.
机译:本文介绍了研究来自里约热内卢州的腐殖质残留土壤的阳离子和阴离子吸附参数的实验室实验结果。土壤是一种沙质粉砂,有58%的细粉(%<#200 ASTM筛子),可塑性指数Ip为29%。土壤粘土部分由高岭石,针铁矿和少量ver石构成,土壤代表了里约热内卢各种工业和家庭废物处理场所用于建造衬板的材料。对土壤进行了全面表征,包括确定物理和岩土力学指标特性,矿物学组成以及理化参数,例如阳离子交换容量(CEC),土壤自然pH和零电荷点pH(ZPC) ),可交换的复杂成分和有机物含量。进行了一系列不同的批次测试,以研究在两个pH值2.5和6.5时土壤相对于离子K〜+,Cl〜-和磷酸盐(主要发生为HPO_4〜(2-))的吸附行为。土壤零电荷点约为3.5,接近高岭石的典型值。还将残留的土壤吸附行为与纯高岭石,针铁矿和赤铁矿样品在相同pH条件下测量的磷酸根离子吸附模式进行了比较。

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