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首页> 外文期刊>Journal of soil & sediments >Lability and sorption of heavy metals as related to chemical, physical, and mineralogical characteristics of highly weathered soils
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Lability and sorption of heavy metals as related to chemical, physical, and mineralogical characteristics of highly weathered soils

机译:与高度风化土壤的化学,物理和矿物学特征相关的重金属的吸收和吸收

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Purpose Heavy metal lability, probably, is the most important isolated factor to cause toxicity in plants and organisms in soils. Sorption of heavy metals, in turn, affects directly the amount of their labile forms in soils. Therefore, to assess sorption and quantify labile forms of Cd, Cu, Ni, Pb, and Zn, adsorption and incubation studies were carried out. Materials and methods The adsorption experiment consisted of a 12 × 5 × 10 factorial design with 12 samples, five metals, and ten doses. An incubation experiment and metal extraction by cationic exchange resin in membrane form, with capacity to exchange 2.80 mol_ckg~(-1) dry resin, were conducted in samples from A and B horizons of six highly weathered soils from Minas Gerais, Brazil. Results and discussion The data from the adsorption experiment was fitted to nonlinear Langmuir and Freiindlich models to give the b and k constants, which were used in a correlation study with soil properties. Cationic resin was used to extract the labile metal forms of heavy metals, and low concentrations of the labile forms were determined for all metals and soils in all incubation times. Conclusions Factors that influenced Langmuir maximum adsorption and Freiindlich buffer capacity were pH andrnCEC, as chemical characteristics, and goethite or hematite contents, as mineralogical attributes. Negative charge density and hydrolyzed species formation may have been main factors related to maximum adsorption and buffer capacity for most heavy metals. Low contents of labile metal forms obtained by cationic resin extraction were attributed to high intensity of metal adsorption reaction onto soil colloids. Greatest lability was found in soils with mineralogy dominated by gibbsite and kaolinite, while lowest metal lability was determined in soils with higher hematite and goethite contents. Due to their specificities, tropical soils should have more research toward the understanding of the relationship soil vulnerability to heavy metals pollution and availability/lability of these important toxic substances in the environment.
机译:目的重金属不稳定性可能是导致土壤中的植物和生物体内毒性的最重要的孤立因素。反过来,重金属的吸附直接影响土壤中不稳定形式的数量。因此,为了评估吸附和量化Cd,Cu,Ni,Pb和Zn的不稳定形式,进行了吸附和温育研究。材料和方法吸附实验由12×5×10析因设计组成,其中包含12个样品,5种金属和10种剂量。在巴西米纳斯吉拉斯州六种高风化土壤的A和B层样品中,进行了膜形式的阳离子交换树脂的孵化实验和金属萃取,该膜能够交换2.80 mol_ckg〜(-1)干树脂。结果与讨论将吸附实验的数据拟合到非线性Langmuir和Freiindlich模型中,得到b和k常数,这些常数用于与土壤特性的相关性研究中。阳离子树脂被用于提取重金属的不稳定金属形式,并且在所有孵育时间内对所有金属和土壤测定了低浓度的不稳定形式。结论影响Langmuir最大吸附和Freiindlich缓冲容量的因素是pH和rnCEC(作为化学特性)和针铁矿或赤铁矿含量(作为矿物学属性)。负电荷密度和水解物质的形成可能是与大多数重金属的最大吸附和缓冲能力有关的主要因素。通过阳离子树脂萃取获得的不稳定金属形式含量低,归因于金属在土壤胶体上的高吸附反应强度。在以三水铁矿和高岭石为主的矿物学的土壤中发现最大的不稳定性,而在赤铁矿和针铁矿含量较高的土壤中测定的金属不稳定性最低。由于其特殊性,热带土壤应进行更多的研究,以了解土壤与重金属污染的脆弱性以及环境中这些重要有毒物质的可用性/不稳定性之间的关系。

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