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爱尔兰泥炭地记录的近期大气污染源的锌-铅同位素和痕量金属综合评估。

Combined zinc-lead isotope and trace-metal assessment of recent atmospheric pollution sources recorded in Irish peatlands.

机构信息

Geology Department, Trinity College Dublin, Ireland.

Isotope Geochemistry, Department of Geosciences, Eberhard-Karls University Tuebingen, Germany.

出版信息

Sci Total Environ. 2019 Mar 25;658:234-249. doi: 10.1016/j.scitotenv.2018.12.049. Epub 2018 Dec 5.

Abstract

Atmospherically-fed Earth surface archives such as ombrotrophic peatlands, lake sediments, and ice consistently show an upward increase in Zn concentrations of hitherto unclear origin. Here, we present a combined stable Zn isotope and trace element (Zn, Cd, Ni, Cu, Cr, V, Ta, Pb) dataset for a historically polluted, near-urban bog (Liffey Head) from the east coast of Ireland. This peat record is compared to an archive from a rural site at the west coast of Ireland (Brackloon Wood). Both archives show a clear near-surface increase in Zn deposition, accompanied by periodic deposition in Cr, Ni, Mo, and V suggesting a co-genetic origin of these elements. In the Liffey Head site, biologic upward distillation of nutrients can be excluded as the origin of the elemental enrichments. The differences in the excess metal ratios between the two sites (e.g., Zn/Cd of 426-1564, east, and 77-106, west) are attributed to a higher contribution from traffic emissions (diesel, petrol) and oil-burning at the near-urban site, and dominant atmospheric influence from solid fossil fuel combustion emissions (e.g., mixed fuel, coal and wood) at the rural site. The Zn isotope composition in the historically-polluted Liffey Head bog evolved from δZn values of 0.72 ± 0.03‰ in the peat accumulated during the 19 century to lighter ratios (0.18 ± 0.03‰) towards the top of the monolith (i.e., recent). Zinc-isotope ratios are positively correlated with excess metal/Cd ratios and also with Pb/Pb, collectively fingerprinting the gradual change from a mining-dominated to a traffic-dominated atmospheric pollution at the east coast over the past century. A prevalent input, interpreted to represent combustion emissions from diesel engines, is observed for the past 15 years. Combined with trace elements and radiogenic Pb isotopes, the information obtained with the Zn isotope systematics adds towards an in-depth characterisation of the pollution signals.

摘要

大气补给的地表档案,如寡营养泥炭地、湖泊沉积物和冰芯,一直以来都显示出锌浓度的上升,但其来源尚不清楚。在这里,我们提供了一份来自爱尔兰东海岸历史上受到污染的近城市沼泽(利菲头)的稳定锌同位素和痕量元素(锌、镉、镍、铜、铬、钒、钽、铅)综合数据集。该泥炭记录与来自爱尔兰西海岸农村地区的档案( Brackloon Wood )进行了比较。两个档案都显示出锌沉积在近地表的明显增加,同时周期性地沉积铬、镍、钼和钒,表明这些元素具有共同的成因。在利菲头遗址,生物向上蒸馏营养物质可以排除是元素富集的起源。两个地点之间的过量金属比值差异(例如,东部的 Zn/Cd 为 426-1564,西部为 77-106)归因于近城市站点交通排放(柴油、汽油)和燃油燃烧的较高贡献,以及农村站点大气中主要受到固体化石燃料燃烧排放(如混合燃料、煤和木材)的影响。历史上受到污染的利菲头沼泽中的锌同位素组成从 19 世纪积累的泥炭中 δZn 值 0.72±0.03‰演变为较轻的比值(0.18±0.03‰),向单体的顶部(即最近)变化。锌同位素比值与过量金属/Cd 比值呈正相关,也与 Pb/Pb 呈正相关,共同显示了过去一个世纪来东海岸从采矿为主向交通为主的大气污染的逐渐变化。过去 15 年来,观察到一种普遍的输入,被解释为来自柴油发动机的燃烧排放。结合微量元素和放射性铅同位素,锌同位素系统获得的信息有助于深入了解污染信号。

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