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首页> 外文期刊>Organic Geochemistry: A Publication of the International Association of Geochemistry and Cosmochemistry >Distributions of polycyclic aromatic hydrocarbons in a sediment core from the north basin of Lake Biwa, Japan
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Distributions of polycyclic aromatic hydrocarbons in a sediment core from the north basin of Lake Biwa, Japan

机译:日本琵琶湖北部盆地沉积岩心中的多环芳烃分布

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摘要

We analyzed the vertical distributions of 19 polycyclic aromatic hydrocarbons (PAHs), total organic carbon (TOC), total nitrogen (TN) and stable carbon isotope ratio (δ~(13)C) in a 27cm sediment core from the north basin of Lake Biwa in order to elucidate changes in PAH sources and events possibly affecting the lake over the last few decades. Both TOC and TN increased gradually from the deepest layer (TOC, 1.2wt.%; TN, 0.14wt.%) to the uppermost layer (TOC, 4.0wt.%; TN, 0.45wt.%). The TOC/TN ratio, a useful indicator for distinguishing between aquatic and terrestrial plant sources, increased remarkably at 11-13cm (10.3-11.1 vs. 8.5-9.7 at other depths), indicating that large amounts of terrestrial material entered the lake when that layer was deposited. All PAHs except perylene gradually increased from the deepest layer, but not as clearly as TOC and TN. At 11-13cm, all PAHs except perylene transiently decreased and perylene transiently increased. Since the PAH ratios used for the elucidation of sources did not change greatly throughout the core, we consider that the major source of PAHs in the lake has not changed during the last few decades. The brief decrease in PAHs at 11-13cm could be the result of dilution by a large input of terrestrial material, which brought in perylene.
机译:我们分析了湖北盆地27cm沉积物中19种多环芳烃(PAHs),总有机碳(TOC),总氮(TN)和稳定碳同位素比(δ〜(13)C)的垂直分布琵琶湖是为了阐明过去几十年来PAH来源和可能影响湖泊的事件的变化。从最深的一层(TOC,1.2wt。%; TN,0.14wt。%)到最上层(TOC,4.0wt。%; TN,0.45wt。%),TOC和TN都逐渐增加。 TOC / TN比是区分水生植物和陆生植物来源的有用指标,在11-13厘米处明显增加(10.3-11.1比其他深度处的8.5-9.7),表明当沉积层。除per外,所有PAHs从最深层逐渐增加,但不如TOC和TN明显。在11-13厘米处,除per外的所有PAH均会短暂减少,而per间会短暂增加。由于用于阐明水源的多环芳烃比率在整个岩心中没有太大变化,因此我们认为湖中多环芳烃的主要来源在过去几十年中没有变化。 PAHs在11-13cm处的短暂减少可能是由于大量输入的陆上物质稀释而产生的,这带来了per。

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