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化学萃取会影响土壤腐殖质的结构和菲吸附。

Chemical extractions affect the structure and phenanthrene sorption of soil humin.

作者信息

Wang Kaijun, Xing Baoshan

机构信息

Department of Plant, Soil and Insect Sciences, University of Massachusetts, Amherst, Massachusetts 01003, USA.

出版信息

Environ Sci Technol. 2005 Nov 1;39(21):8333-40. doi: 10.1021/es050737u.

DOI:10.1021/es050737u
PMID:16294871
Abstract

Humin is a major fraction of soil organic matter and strongly affects the sorption behavior and fate of organic contaminants in soils and sediments. This study evaluated four different extraction methods for soil humins in terms of their organic carbon structural changes and the consequent effects on phenanthrene sorption. Solid-state 13C NMR demonstrated that 0.1 M NaOH exhaustively extracted humin and humin extracted with 6 M HF/HCl at 60 degrees C had a relatively high amount of aliphatic components as compared with 1 M HF-extracted humin. The treatment of 6 M HF/HCl at 60 degrees C greatly reduced carbohydrate components (50-108 ppm) from humin samples, i.e., more than 50% reduction. In addition, the humin from this 6 M HF/HCl treatment contained relatively more amorphous poly(methylene) domains than the humins extracted by other methods. With the respect to phenanthrene sorption, the linearity of sorption isotherm (N) and sorption affinity (Koc) varied markedly among the humin samples extracted by different methods. The NaOH exhaustively extracted humin had the most nonlinear sorption isotherm and the HF-extracted humin had the lowest Koc. It is concluded that humin samples from different extraction procedures exhibited substantial differences in their organic carbon structure and sorption characteristics, even though they were from the same soil. Therefore, one needs to be cautious when comparing the structural and sorption features of soil humins, especially when they are extracted differently. The 6 M HCl/HF extraction at elevated temperature is not encouraged, due to the modifications of chemical structure and physical conformation of organic matter.

摘要

胡敏素是土壤有机质的主要组分,对土壤和沉积物中有机污染物的吸附行为及归宿有强烈影响。本研究从有机碳结构变化及其对菲吸附的后续影响方面,评估了四种不同的土壤胡敏素提取方法。固态13C核磁共振表明,0.1 M NaOH能彻底提取胡敏素,与1 M HF提取的胡敏素相比,60℃下用6 M HF/HCl提取的胡敏素具有相对较高含量的脂肪族成分。60℃下用6 M HF/HCl处理极大地减少了胡敏素样品中的碳水化合物组分(50 - 108 ppm),即减少了50%以上。此外,这种6 M HF/HCl处理得到的胡敏素比其他方法提取的胡敏素含有相对更多的无定形聚亚甲基域。关于菲吸附,不同方法提取的胡敏素样品之间,吸附等温线的线性(N)和吸附亲和力(Koc)有显著差异。NaOH彻底提取的胡敏素具有最非线性的吸附等温线,HF提取的胡敏素Koc最低。得出的结论是,尽管来自同一土壤,但不同提取程序得到的胡敏素样品在有机碳结构和吸附特性方面存在显著差异。因此,在比较土壤胡敏素的结构和吸附特征时需要谨慎,尤其是当它们提取方法不同时。由于有机质化学结构和物理构象的改变,不鼓励在高温下用6 M HCl/HF进行提取。

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