Rhodes Angela H, Hofman Jakub, Semple Kirk T
Department of Environmental Science and the Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom.
Environ Pollut. 2008 Mar;152(2):424-30. doi: 10.1016/j.envpol.2007.06.072. Epub 2007 Sep 19.
The characteristics of natural soils often vary from those of artificial soil (e.g. OECD), which may lead to substantial differences in the bioavailability of test substances. The aim of this investigation was to characterise the development of phenanthrene catabolism in both natural and artificial soils with varying total organic carbon (TOC) content after 1, 14, 42 and 84 d soil-phenanthrene contact time. Indigenous catabolic activity was measured via the addition of 14C-phenanthrene using the respirometric soil slurry assay. Notably, the lag phases, fastest rates and total extents of 14C-phenanthrene degradation were relatively comparable in soils with similar TOC content after 1 d contact time. However, natural soils generally exhibited significantly shorter lag phases, faster rates and higher extents of mineralisation, than their artificial counterparts after 42 and 84 d contact time. Such findings suggest that the extrapolation of results from artificial soils to real/natural soils may not be straightforward.
天然土壤的特性往往与人工土壤(如经合组织规定的土壤)不同,这可能导致受试物质的生物有效性存在显著差异。本研究的目的是表征在土壤与菲接触1、14、42和84天后,总有机碳(TOC)含量不同的天然土壤和人工土壤中菲的分解代谢情况。通过使用测氧土壤泥浆试验添加14C-菲来测量原生分解代谢活性。值得注意的是,在接触1天后,TOC含量相似的土壤中,14C-菲降解的延迟期、最快降解速率和总降解程度相对相当。然而,在接触42和84天后,天然土壤的延迟期通常明显更短,降解速率更快,矿化程度更高,相比人工土壤而言。这些发现表明,将人工土壤中的结果外推至实际/天然土壤可能并非易事。