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使用耦合稳定同位素稀释-顺序提取法研究金属污染土壤中镉的反应性

Cadmium reactivity in metal-contaminated soils using a coupled stable isotope dilution-sequential extraction procedure.

作者信息

Ahnstrom Z A, Parker D R

机构信息

Department of Environmental Sciences, University of California, Riverside 92521, USA.

出版信息

Environ Sci Technol. 2001 Jan 1;35(1):121-6. doi: 10.1021/es001350o.

Abstract

To better understand the intrinsic reactivity of Cd, four soils having diverse sources of Cd contamination (total Cd: 22-34 mg kg(-1)) were investigated using a stable isotope dilution-sequential extraction procedure (SID-SEP) during a 59-week incubation. Samples were spiked with carrier-free 111Cd and periodically extracted into five operationally defined fractions; the 111Cd:10Cd ratios were measured by inductively coupled plasma-mass spectrometry. The total labile pool of Cd (E value) was calculated as well as the labile Cd within each extracted fraction. Results for three of the soils (Cd sources: natural, sewage sludge, smelter emissions) were quite similar. The overall %E after 2-week equilibration was 35-49% of total soil Cd. Within fraction 2 (sorbed/carbonate), 70-75% of the Cd was isotopically labile, while within fraction 3 (oxidizable) only 35-41% of the Cd was labile within 2 weeks. The fourth (reducible) and fifth (residual) fractions were dominated by nonlabile Cd. Although all E values increased somewhat from 2 to 59 weeks, none of the extracted fractions reached isotopic equilibrium with the soluble/exchangeable Cd extracted during step 1. Because fractions 2 and 3 dominated the native Cd in all three soils, the total labile pool was contributed primarily (85-98%) by these two fractions. A fourth soil (mine spoil-contaminated) was demonstrably different: after 2 weeks, the overall %E was just 13 and, although 82% of the total Cd was present in the oxidizable fraction, just 2% of that was isotopically labile. The nonlability of Cd in this soil could be ascribed to the predominance of inorganic forms, most likely occluded Cd in sphalerite. No single Cd fraction from the SEP nor any combination of fractions showed a good correspondence with the size of the isotopically labile pool. Our results suggest that conventional SEPs may be of limited utility for predicting bioavailability, for example, during ecological risk assessment.

摘要

为了更好地理解镉的内在反应活性,在为期59周的培养期间,采用稳定同位素稀释-顺序提取法(SID-SEP)对四种镉污染来源不同(总镉含量:22 - 34 mg/kg)的土壤进行了研究。样品加入无载体的111Cd后,定期提取为五个操作定义的组分;通过电感耦合等离子体质谱法测量111Cd:10Cd比值。计算了镉的总活性库(E值)以及每个提取组分中的活性镉。三种土壤(镉来源:天然、污水污泥、冶炼厂排放)的结果非常相似。平衡2周后的总体E值占土壤总镉的35 - 49%。在第2组分(吸附/碳酸盐结合态)中,70 - 75%的镉具有同位素活性,而在第3组分(可氧化态)中,2周内只有35 - 41%的镉具有活性。第四(可还原态)和第五(残留态)组分主要是无活性镉。尽管所有E值从2周增加到59周时都有所上升,但在步骤1中提取的所有组分都未与可溶性/交换性镉达到同位素平衡。由于第2和第3组分在所有三种土壤中占主导地位,总活性库主要由这两个组分贡献(85 - 98%)。第四种土壤(矿山废石污染土壤)明显不同:2周后,总体E值仅为13,尽管总镉的82%存在于可氧化组分中,但其中只有2%具有同位素活性。该土壤中镉的非活性可能归因于无机形态的主导,最有可能是闪锌矿中包裹的镉。SEP中的单一镉组分或任何组分组合都与同位素活性库的大小没有良好的对应关系。我们的结果表明,传统的顺序提取法在预测生物有效性方面可能用途有限,例如在生态风险评估期间。

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