首页> 外文期刊>European Journal of Soil Science >Multi-element stable isotopic dilution and multi-surface modelling to assess the speciation and reactivity of cadmium and copper in soil
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Multi-element stable isotopic dilution and multi-surface modelling to assess the speciation and reactivity of cadmium and copper in soil

机译:多元素稳定同位素稀释和多表面模拟,评估土壤中镉和铜的形态和反应性

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摘要

Chemical extraction, multi-element stable isotopic dilution (ID) and multi-surface modelling were used to investigate the lability of cadmium (Cd) and copper (Cu) in nine types of soil with different properties and contaminated or not with Cd and Cu. The chemical extraction and ID analyses both showed that Cd was more labile than Cu in all the soil types studied. From the ID results, 32.8-93.3% of total Cd and 14.7-71.8% of total Cu were isotopically exchangeable after 3 days of equilibration. A single extraction in 0.43 m HNO3 gave similar results to the 3-day ID assay for Cu in most of the soils and for Cd in the non-calcareous soils. However, an eight-step selective sequential extraction (SSE) procedure gave different results from the ID assay for both metals. Predictions of the multi-surface model for the amounts of Cd and Cu adsorbed, based on measured metal ion activities in the soil solution and the concentrations of reactive surfaces in the soil, agreed with the ID results. The model predicted that soil organic matter was the predominant sorbent for Cd and Cu in the soils and that manganese oxide was the least important sorbent. The contributions of iron oxides to sorption were predicted to be small except in soil with a high pH and little organic matter. The predicted sorption on different soil components did not match SSE measurements.
机译:通过化学萃取,多元素稳定同位素稀释(ID)和多表面建模研究了9种性质不同且受或未受Cd和Cu污染的土壤中镉(Cd)和铜(Cu)的不稳定性。化学提取和ID分析均表明,在所有研究的土壤类型中,Cd比Cu不稳定。根据ID结果,在平衡3天后,总Cd的32.8-93.3%和总Cu的14.7-71.8%可以同位素交换。对于大部分土壤中的Cu和非钙质土壤中的Cd,在0.43 m HNO3中的单次萃取所获得的结果与3天ID分析相似。但是,八步选择性顺序萃取(SSE)程序从两种金属的ID分析​​得出的结果不同。根据测得的土壤溶液中金属离子的活性和土壤中反应性表面的浓度,对吸附的Cd和Cu量的多表面模型的预测与ID结果一致。该模型预测,土壤有机质是土壤中Cd和Cu的主要吸附剂,而氧化锰是最不重要的吸附剂。预测铁氧化物对吸附的贡献很小,除了在具有高pH值和很少有机物的土壤中。在不同土壤成分上的预计吸附量与SSE测量值不匹配。

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