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表层河口沉积物中萘、菲和苯并[a]芘的季节性生物转化。

Seasonal Biotransformation of Naphthalene, Phenanthrene, and Benzo[a]pyrene in Surficial Estuarine Sediments.

机构信息

Biology Department, University of Massachusetts at Boston, Boston, Massachusetts 02125.

出版信息

Appl Environ Microbiol. 1989 Jun;55(6):1391-9. doi: 10.1128/aem.55.6.1391-1399.1989.

DOI:10.1128/aem.55.6.1391-1399.1989
PMID:16347932
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC202877/
Abstract

Transformation rates of naphthalene, phenanthrene, and benzo[a]pyrene in oxidized surficial sediments of a polluted urban estuary, Boston Harbor, Mass., were determined over a period of 15 months. Three sites characterized by muddy sediments were selected to represent a >300-fold range of ambient polycyclic aromatic hydrocarbon (PAH) concentration. Transformation rates were determined by a trace-level radiolabel PAH assay which accounted for PAH mineralization, the formation of polar metabolites, residue, and recovered parental PAHs in sediment slurries. Transformation rates of the model PAHs increased with increasing ambient PAH concentrations. However, turnover times for a given PAH were similar at all sites. The turnover times were as follows: naphthalene, 13.2 to 20.1 days; phenanthrene, 7.9 to 19.8 days, and benzo[a]pyrene, 53.7 to 82.3 days. At specific sites, rates were significantly affected by salinity, occasionally affected by temperature, but not affected by pH over the course of the study. Seasonal patterns of mineralization were observed for each of the PAHs at all sites. The timing of seasonal maxima of PAH mineralization varied from site to site. Seasonal potential heterotrophic activities as measured by acetate and glutamate mineralization rates did not always coincide with PAH mineralization maxima and minima, suggesting that the two processes are uncoupled in estuarine sediments.

摘要

在马萨诸塞州波士顿港污染城市河口的表层沉积物中,15 个月的时间里测定了萘、菲和苯并[a]芘的转化速率。选择了三个以泥质沉积物为特征的地点,以代表环境多环芳烃(PAH)浓度超过 300 倍的范围。转化速率通过痕量放射性标记 PAH 测定法确定,该方法考虑了 PAH 的矿化作用、极性代谢物的形成、残留物和回收的母体 PAHs 在沉积物悬浮液中的情况。模型 PAHs 的转化速率随着环境 PAH 浓度的增加而增加。然而,在所有地点,给定 PAH 的周转率相似。周转率如下:萘,13.2 至 20.1 天;菲,7.9 至 19.8 天,苯并[a]芘,53.7 至 82.3 天。在特定地点,盐度会显著影响速率,温度偶尔会影响速率,但在研究过程中 pH 不会影响速率。在所有地点,都观察到了每一种 PAH 的矿化季节性模式。PAH 矿化季节性最大值的时间从一个地点到另一个地点而有所不同。通过乙酸盐和谷氨酸矿化率测量的季节性潜在异养活性并不总是与 PAH 矿化最大值和最小值同时发生,这表明这两个过程在河口沉积物中是不耦合的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd54/202877/216840380b62/aem00099-0080-a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd54/202877/216840380b62/aem00099-0080-a.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/fd54/202877/216840380b62/aem00099-0080-a.jpg

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