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Sorption of naphthalene and phenanthrene by soil humic acids

机译:土壤腐殖酸对萘和菲的吸附。

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Humic acids are a major fraction of soil organic matter (SOM), and sorption of hydrophobic organic chemicals by humic acids influences their behavior and fate in soil. A clear understanding of the sorption of organic chemicals by humic acids will help to determine their sorptive mechanisms in SOM and soil. In this paper, we determined the sorption of two hydrophobic organic compounds, naphthalene and phenanthrene by six pedogenetically related humic acids. These humic acids were extracted from different depths of a single soil profile and characterized by solid-state CP/MAS 13~C nuclear magnetic resonance (NMR). Aroma- ticity of the humic acids increased with soil depth. Similarly, atomic ratios of C/H and C/O also increased with depth (from organic to mineral horizons). All isotherms were nonlinear. Freundlich exponents (N) ranged from 0.87 to 0.95 for naphthalene and from 0.86 to 0.92 for phenanthrene. The N values of phenanthrene were consistently lower than naphthalene for a given humic acid. For both compounds, N values decreased with increasing aromaticity of the humic acids, such an inverse relationship was never reported before. These results support the dual-mode sorption model where partitioning occurs in both expanded (flexible) and condensed (rigid) domains while nonlinear sorption only in condensed domains of SOM. Sorption in the condensed domains may be a cause for slow desorption, and reduced availability and toxicity with aging.
机译:腐殖酸是土壤有机质(SOM)的主要组成部分,腐殖酸对疏水性有机化学物质的吸附会影响腐殖酸在土壤中的行为和命运。明确了解腐殖酸对有机化学物质的吸附将有助于确定它们在SOM和土壤中的吸附机理。在本文中,我们确定了六种与人为相关的腐殖酸对两种疏水性有机化合物萘和菲的吸附。这些腐殖酸是从单一土壤剖面的不同深度提取的,并具有固态CP / MAS 13〜C核磁共振(NMR)的特征。腐殖酸的芳香度随土壤深度的增加而增加。同样,C / H和C / O的原子比也随深度(从有机层到矿物层)而增加。所有等温线都是非线性的。萘的Freundlich指数(N)为0.87至0.95,菲为0.86至0.92。对于给定的腐殖酸,菲的N值始终低于萘。对于这两种化合物,N值均随着腐殖酸的芳香性增加而降低,这种反比关系以前从未报道过。这些结果支持双模式吸附模型,其中在扩展(柔性)域和压缩(刚性)域中均发生分区,而仅在SOM的压缩域中进行非线性吸附。缩合区域中的吸附可能是缓慢解吸的原因,并且会降低可用性和老化性。

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