首页> 外文期刊>European Journal of Soil Science >The phenanthrene-sorptive interface of an arable topsoil and its particle size fractions.
【24h】

The phenanthrene-sorptive interface of an arable topsoil and its particle size fractions.

机译:耕层表土的菲吸附界面及其粒径分数。

获取原文
获取原文并翻译 | 示例
           

摘要

Sorption of organic chemicals in soil is affected by the properties and availability of surfaces. These surfaces are composed of diverse mineral, organic and biological components, forming a soil's 'biogeochemical interface'. Phenanthrene was used to probe the hydrophobic sorptive capacity of the interface of an arable soil. Batch sorption experiments were carried out with the bulk soil as well as the fine (0.2-6.3 micro m) and coarse (6.3-63 micro m) particle size fractions of two arable topsoil samples with different organic matter (OM) contents from a Eutric Cambisol. The specific surface area (SSA) of the bulk soil and particle size fractions was determined by BET-N2 and EGME sorption. OM composition was characterized by solid-state 13C NMR spectroscopy. No clear relationship was found between phenanthrene sorption and SSA. We conclude that phenanthrene probes a specific fraction of the soil interface that is not well represented by the traditional methods of SSA detection such as BET-N2 and EGME sorption. The sorption behaviour of phenanthrene may therefore provide a useful additional tool to characterize the specific affinity of the soil biogeochemical interface for hydrophobic molecules. Sorption capacity for phenanthrene increased after particle-size fractionation, indicating that the reduced availability of the interface caused by the aggregated structure is important for the sorptive capacity of a soil. This should be considered when projecting data obtained from extensively treated and fractionated samples to the actual interaction with biogeochemical interfaces as they are present in soil.
机译:土壤中有机化学物质的吸附受表面性质和可用性的影响。这些表面由多种矿物,有机和生物成分组成,形成了土壤的“生物地球化学界面”。菲用于探测耕作土壤界面的疏水吸附能力。使用来自Eutric的两种具有不同有机物(OM)含量的耕作表土样品,对散装土壤以及细颗粒(0.2-6.3微米)和粗颗粒(6.3-63微米)的粒度分批进行吸附实验坎比索尔。 BET-N 2 和EGME的吸附确定了散装土壤的比表面积(SSA)和粒径分数。 OM组成由固态13 C NMR谱表征。在菲吸附和SSA之间未发现明确的关系。我们得出的结论是,菲探测了土壤界面的特定部分,而传统的SSA检测方法(如BET-N 2 和EGME吸附)不能很好地代表菲。菲的吸附行为因此可以提供有用的附加工具来表征土壤生物地球化学界面对疏水分子的特异性亲和力。粒度分级后,菲的吸附容量增加,这表明由聚集结构引起的界面可用性降低对土壤的吸附能力很重要。将经过广泛处理和分级分离的样本获得的数据投影到土壤中存在的生物地球化学界面的实际相互作用时,应考虑这一点。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号