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中国东北一个 maar 湖沉积物岩芯中多环芳烃的沉积记录:历史大气沉降的证据

Sedimentary record of polycyclic aromatic hydrocarbons in a sediment core from a maar lake, Northeast China: evidence in historical atmospheric deposition.

作者信息

Guan Yu-Feng, Sun Jian-Lin, Ni Hong-Gang, Guo Jian-Yang

机构信息

State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China.

出版信息

J Environ Monit. 2012 Sep;14(9):2475-81. doi: 10.1039/c2em30461a. Epub 2012 Jul 30.

Abstract

A maar lake is an excellent ecosystem to study the atmospheric deposition of pollutants, as its contaminants are primarily by atmospheric deposition. In this study, a sediment core from Sihailongwan Maar Lake, Northeast China, was collected and the historical atmospherically deposited polycyclic aromatic hydrocarbons (PAHs) were analyzed. The concentrations of TPAHs (the sum of the US EPA proposed 16 priority PAHs, excluding naphthalene and pyrene) ranged from 473.9 to 2289 ng g(-1) with a slow increasing stage in the deeper sediments and a sharp increasing stage in the upper sediments. The input rate of TPAHs, especially that of PAH(9) (the sum of fluoranthene, benzo(a)anthracene, chrysene, benzo(b)fluoranthene, benzo(k)fluoranthene, benzo(a)pyrene, indeno(1,2,3-cd)pyrene, dibenzo(ah)anthrathene, and benzo(ghi)perylene), correlated well to the Chinese historical socioeconomic data. This indicates that sediment PAHs were mainly derived from human activities and PAH(9) can be regarded as a better indicator of the local socioeconomic development. Source identification suggested that PAHs were originated primarily from mixed sources (e.g., coal and biomass burning and petroleum combustion), except for perylene which was mostly of diagenetic origin. In addition, the down-core PAHs profile clearly illustrated that PAHs sources in Northeast China experienced a transformation from low- and moderate temperature to high-temperature combustion processes, especially after the late 1980s. Additionally, an ecological risk assessment using two redefined biological thresholds (TEQ(ERL) and TEQ(ERM)) indicated that most of the PAHs measured in the present sediment core would not cause an immediate toxic effect; only FLU and PHEN are a potential source of concern for biological impairment.

摘要

玛珥湖是研究污染物大气沉降的优良生态系统,因为其污染物主要来自大气沉降。本研究采集了中国东北四海龙湾玛珥湖的一根沉积岩芯,并对历史时期大气沉降的多环芳烃(PAHs)进行了分析。总多环芳烃(TPAHs,即美国环保署提议的16种优先多环芳烃之和,不包括萘和芘)浓度范围为473.9至2289 ng g(-1),在较深沉积物中有一个缓慢增长阶段,在上层沉积物中有一个急剧增长阶段。TPAHs的输入速率,尤其是PAH(9)(荧蒽、苯并(a)蒽、 Chrysene、苯并(b)荧蒽、苯并(k)荧蒽、苯并(a)芘、茚并(1,2,3-cd)芘、二苯并(ah)蒽和苯并(ghi)苝之和)与中国历史社会经济数据具有良好的相关性。这表明沉积物中的多环芳烃主要源自人类活动,并且PAH(9)可被视为当地社会经济发展的一个更好指标。源解析表明,多环芳烃主要源自混合源(如煤炭和生物质燃烧以及石油燃烧),除苝主要源自成岩作用。此外,沉积岩芯中多环芳烃的垂向分布清楚地表明,中国东北地区的多环芳烃源经历了从低温和中温燃烧过程到高温燃烧过程的转变,尤其是在20世纪80年代后期之后。此外,使用两个重新定义的生物阈值(TEQ(ERL)和TEQ(ERM))进行的生态风险评估表明,在本沉积岩芯中测得的大多数多环芳烃不会造成即时毒性效应;只有芴和菲是生物损害的潜在关注源。

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