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麦肯齐三角洲湖泊沉积物中多环芳烃的来源

Origin of polycyclic aromatic hydrocarbons in lake sediments of the Mackenzie Delta.

作者信息

Headley John V, Marsh Philip, Akre Christine J, Peru Kerry M, Lesack Lance

机构信息

National Water Research Institute, 11 Innovation Boulevard, Saskatoon, SK, Canada.

出版信息

J Environ Sci Health A Tox Hazard Subst Environ Eng. 2002 Aug;37(7):1159-80. doi: 10.1081/ese-120005979.

Abstract

The concentrations and distribution of polycyclic aromatic hydrocarbons (PAHs) were assessed in sediment cores from among 14 lakes from three regions comprising a transect across the central Mackenzie Delta. PAHs were consistently found in the lake sediments, with parent concentrations in the 20-200 ng/g range. Concentrations were generally independent of depth in the sediment cores and this pattern was similar among the 3 regions of the delta. Concentrations increased in a westerly direction among the regions. For some lakes, the concentration of PAHs decreased with decreasing flooding frequency, and decreasing sedimentation rates. For the latter, maximum concentrations occurred at shallower depths within the sediment cores as flooding frequency among the lakes decreased. The distributions of C0-C4 alkylated 2- and 3- ring PAHs were consistent with a petrogenic origin, while the corresponding distribution of 4-ring PAHs appears to be more consistent with a biogenic or pyrogenic origin. Based on relative contributions to the overall PAH budget, a petrogenic source appears to be dominant. However, the pyrene/fluoranthene ratio is more consistent with a source derived from peat. The alkylated PAH profiles are inconsistent with those in the Athabasca River system, and supports a previously published hypothesis that the contribution of PAHs from the Athabasca oil sands to the lower Mackenzie River is minimal. A double ratio plot of chrysene vs dibenzothiophene, diagnostic of weathering, suggests most weathering occurred before the sediments were deposited in the lakes, while a double ratio plot of dibenzothiophene vs phenanthrene suggests a common source of PAHs across the delta, despite differing water sources from east to west across the delta. PAH inputs to the delta appear to mirror sediment inputs documented in previous work, where high sediment input from the Mackenzie mainstem during high floods dominates the delta sediment influx and masks any influence of the Peel River.

摘要

对位于麦肯齐河三角洲中部横断面的三个地区14个湖泊的沉积物岩芯中的多环芳烃(PAHs)浓度和分布进行了评估。在湖泊沉积物中始终能检测到PAHs,母体浓度在20 - 200 ng/g范围内。浓度通常与沉积物岩芯深度无关,且这种模式在三角洲的三个地区相似。各地区PAHs浓度沿西向增加。对于一些湖泊,PAHs浓度随洪水频率降低和沉积速率降低而降低。对于后者,随着湖泊洪水频率降低,沉积物岩芯中最大浓度出现在较浅深度处。C0 - C4烷基化的二环和三环PAHs的分布与成岩来源一致,而四环PAHs的相应分布似乎更符合生物源或热解源。基于对总PAH预算的相对贡献,成岩源似乎占主导。然而,芘/荧蒽比值更符合源自泥炭的来源。烷基化PAH剖面与阿萨巴斯卡河水系中的剖面不一致,并支持了之前发表的假说,即阿萨巴斯卡油砂中的PAHs对麦肯齐河下游的贡献极小。诊断风化作用的芘与二苯并噻吩的双比值图表明,大多数风化作用发生在沉积物沉积到湖泊之前,而二苯并噻吩与菲的双比值图表明,尽管三角洲东西部水源不同,但整个三角洲PAHs有共同来源。PAHs输入到三角洲的情况似乎反映了先前工作中记录的沉积物输入情况,即高洪水期间麦肯齐河干流的高沉积物输入主导了三角洲沉积物流入,并掩盖了皮尔河的任何影响。

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