首页> 美国卫生研究院文献>International Journal of Environmental Research and Public Health >Sorption of Hydrophobic Organic Compounds on Natural Sorbents and Organoclays from Aqueous and Non-Aqueous Solutions: A Mini-Review
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Sorption of Hydrophobic Organic Compounds on Natural Sorbents and Organoclays from Aqueous and Non-Aqueous Solutions: A Mini-Review

机译:疏水性有机化合物对天然吸附剂和有机粘土的水溶液和非水溶液吸附:简要综述。

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摘要

Renewed focus on the sorption of hydrophobic organic chemicals (HOCs) onto mineral surfaces and soil components is required due to the increased and wider range of organic pollutants being released into the environment. This mini-review examines the possibility of the contribution and mechanism of HOC sorption onto clay mineral sorbents such as kaolinite, and soil organic matter and the possible role of both in the prevention of environmental contamination by HOCs. Literature data indicates that certain siloxane surfaces can be hydrophobic. Therefore soils can retain HOCs even at low soil organic levels and the extent will depend on the structure of the pollutant and the type and concentration of clay minerals in the sorbent. Clay minerals are wettable by nonpolar solvents and so sorption of HOCs onto them from aqueous and non-aqueous solutions is possible. This is important for two reasons: firstly, the movement and remediation of soil environments will be a function of the concentration and type of clay minerals in the soil. Secondly, low-cost sorbents such as kaolinite and expandable clays can be added to soils or contaminated environments as temporary retention barriers for HOCs. Inorganic cations sorbed onto the kaolinite have a strong influence on the rate and extent of sorption of hydrophobic organic pollutants onto kaolinite. Structural sorbate classes that can be retained by the kaolinite matrix are limited by hydrogen bonding between hydroxyl groups of the octahedral alumosilicate sheet and the tetrahedral sheet with silicon. Soil organic carbon plays a key role in the sorption of HOCs onto soils, but the extent will be strongly affected by the structure of the organic soil matter and the presence of soot. Structural characterisation of soil organic matter in a particular soil should be conducted during a particular contamination event. Contamination by mining extractants and antibiotics will require renewed focus on the use of the QSAR approaches in the context of the sorption of HOCs onto clay minerals from aqueous and non-aqueous solutions.
机译:由于越来越多的有机污染物被释放到环境中,因此需要重新关注疏水性有机化学物质(HOC)在矿物表面和土壤成分上的吸附。这篇小型综述探讨了HOC吸附在粘土矿物吸附剂(例如高岭土)和土壤有机质上的贡献和机理,以及两者在防止HOC污染环境中的可能作用。文献数据表明某些硅氧烷表面可以是疏水的。因此,即使在土壤有机物含量较低的情况下,土壤也可以保留HOC,其程度取决于污染物的结构以及吸附剂中粘土矿物的类型和浓度。粘土矿物可以被非极性溶剂润湿,因此HOCs可以从水溶液和非水溶液中吸附到它们上面。这很重要,原因有两个:首先,土壤环境的移动和修复将取决于土壤中粘土矿物的浓度和类型。其次,可以将低成本吸附剂(例如高岭石和可膨胀粘土)添加到土壤或受污染的环境中,作为HOC的临时保留屏障。吸附到高岭石上的无机阳离子对疏水性有机污染物吸附到高岭石上的速率和程度有很大影响。可被高岭石基质保留的结构性山梨酸酯类别受八面体铝硅酸盐片和四面体片与硅的羟基之间的氢键限制。土壤有机碳在HOCs吸附到土壤上起着关键作用,但是有机碳物质的结构和烟灰的存在会严重影响有机碳的含量。在特定的污染事件中应对特定土壤中的土壤有机质进行结构表征。采矿中提取剂和抗生素的污染将需要重新关注使用QSAR方法将HOC吸附到水溶液和非水溶液中的粘土矿物上。

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