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在一个杂酚油污染场地的不同土壤层中多环芳烃的营养限制生物降解

Nutrient-limited biodegradation of PAH in various soil strata at a creosote contaminated site.

作者信息

Breedveld G D, Sparrevik M

机构信息

Norwegian Geotechnical Institute, Ullevaal Stadion, Oslo.

出版信息

Biodegradation. 2000;11(6):391-9. doi: 10.1023/a:1011695023196.

DOI:10.1023/a:1011695023196
PMID:11587443
Abstract

The effects of nutrient addition on the in situ biodegradation of polycyclic aromatic hydrocarbons in creosote contaminated soil were studied in soil columns taken from various soil strata at a wood preserving plant in Norway. Three samples were used: one from the topsoil (0-0.5 m), one from an organic rich layer (2-2.5 m) and one from the sandy aquifer (4.5-5 m). The addition of inorganic nitrogen and phosphorous stimulated the degradation of polycyclic aromatic hydrocarbons (PAHs) in the top soil and the aquifer sand. These two soils, which differed strongly in contamination levels, responded similarly to nutrient addition with the corresponding degradation of 4-ring PAHs. The ratio between available nitrogen (N) and phosphorous (P) might explain the degree of degradation observed for the 4-ring PAHs. However, the degree of degradation of 3-ring PAHs did not significantly increase after nutrient addition. An increase in the respiration rate, after nutrient addition, could only be observed in the topsoil. In the aquifer sand, 4-ring PAH degradation was not accompanied by an increase in the respiration rate or the number of heterotrophic micro-organisms. PAH degradation in the organic layer did not respond to nutrient addition. This was probably due to the low availability of the contaminants for micro-organisms, as a result of sorption to the soil organic matter. Our data illustrate the need for a better understanding of the role of nutrients in the degradation of high molecular weight hydrocarbons for the successful application of bioremediation at PAH contaminated sites.

摘要

在挪威一家木材防腐厂,从不同土壤层采集土壤柱,研究了添加营养物质对杂酚油污染土壤中多环芳烃原位生物降解的影响。使用了三个样品:一个来自表层土(0 - 0.5米),一个来自富含有机质层(2 - 2.5米),一个来自砂质含水层(4.5 - 5米)。添加无机氮和磷刺激了表层土和含水层砂中多环芳烃(PAHs)的降解。这两种污染水平差异很大的土壤,对添加营养物质的反应相似,四环PAHs相应降解。有效氮(N)与磷(P)的比例可能解释了观察到的四环PAHs的降解程度。然而,添加营养物质后三环PAHs的降解程度没有显著增加。添加营养物质后,仅在表层土中观察到呼吸速率增加。在含水层砂中,四环PAH降解并未伴随着呼吸速率或异养微生物数量的增加。有机层中的PAH降解对添加营养物质没有反应。这可能是由于污染物被土壤有机质吸附,微生物对其利用率较低。我们的数据表明,为了在PAH污染场地成功应用生物修复,需要更好地理解营养物质在高分子量烃类降解中的作用。

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