Historical trend of polycyclic aromatic hydrocarbons in a sediment core from Osaka Bay during the Meghalayan

Kai Nils Nitzsche, Naoto F Ishikawa, Toshihiro Yoshimura, Hiroto Kajita, Hodaka Kawahata, Nanako O Ogawa, Hisami Suga, Naohiko Ohkouchi
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Abstract

Polycyclic aromatic hydrocarbons (PAHs) are produced by incomplete combustion of biomass and fossil fuel, yet PAHs have been rarely analyzed in coastal sediment cores as a tracer for human activities before industrialization. The aim of this study was to assess if the historical trend of PAHs can be related to past human activities. To this end, we have determined the concentrations of PAHs in a 9 m-long sediment core from Osaka Bay, which records history of the last 2400 years. The concentration of PAHs before the beginning of the 17th century CE, the beginning of the peaceful Edo period, was consistently low (<100 ng g−1) and mainly comprised of smoke-derived PAHs reflecting the natural background. A relative higher abundance of 4−6 ring PAHs from the early 17th century CE and a higher PAH concentration from the early 18th century CE until approximately 1800 CE agreed with a population increase, Cu smelting activities and increasing combustion of charcoal. The constant PAH concentration until the late 19th century CE overlapped with a decline in the population in the Osaka area. An increasing PAH concentration from the late 19th century CE marked the beginning of industrialization in the Modern age. The peak in PAH concentration in 1945 CE was likely caused by burning of wooden structures due to air raids on Osaka City. A second peak around 1980 CE indicated the introduction of cleaner energies. We conclude that PAHs in coastal sediment cores can be used to reconstruct past human activities.
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湄加拉湾时期大阪湾沉积岩芯中多环芳烃的历史趋势
多环芳烃(PAHs)是由生物质和化石燃料不完全燃烧产生的,但很少在沿海沉积物岩心中分析多环芳烃作为工业化之前人类活动的示踪剂。本研究的目的是评估 PAHs 的历史趋势是否与过去的人类活动有关。为此,我们测定了大阪湾 9 米长沉积物岩芯中 PAHs 的浓度,该岩芯记录了过去 2400 年的历史。在西元 17 世纪初,即和平的江户时代开始之前,多环芳烃的浓度一直很低(100 ng g-1),主要由烟雾衍生的多环芳烃组成,反映了自然背景。从公元 17 世纪早期开始,4-6 环多环芳烃的丰度相对较高,而从公元 18 世纪早期到公元 1800 年左右,多环芳烃的浓度较高,这与人口增加、铜冶炼活动和木炭燃烧增加有关。直到公元 19 世纪晚期,多环芳烃的浓度一直保持不变,这与大阪地区人口的减少相吻合。多环芳烃浓度从公元 19 世纪末开始上升,标志着现代工业化的开始。多环芳烃浓度在西元 1945 年达到峰值,这可能是由于大阪市遭受空袭,木制建筑被烧毁所致。公元 1980 年左右出现的第二个峰值表明清洁能源的引入。我们的结论是,沿海沉积岩芯中的多环芳烃可用于重建过去的人类活动。
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