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Pb isotope record over one century in snow from Victoria Land, Antarctica

机译:来自南极洲维多利亚州土地的雪中一个世纪以来的铅同位素记录

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摘要

Pb and Ba concentrations and Pb isotopic compositions are reported for firn core and snow pit samples from Victoria Land, Antarctica, dating from 1872 AD to 1994 AD. From variations in Pb/Ba ratios and Pb isotopic compositions, two periods of major Pb enhancements were identified, from 1891 to 1908 AD and from 1948 to 1994 AD. The earlier pollution event is attributed to Pb emissions from non-ferrous metal production and coal combustion in the Southern Hemisphere and is in excellent agreement with coincident pollution inputs reported in firn/ice cores from two other regions of Antarctica, at Coats Land and Law Dome. Using Pb isotopic systematics, it was calculated that similar to 50% of Pb deposited in Victoria Land in 1897 originated from anthropogenic emission sources. The more recent period of Pb enhancements, from 1948 to 1994 AD, corresponds to the introduction and widespread use of gasoline alkyl Pb additives in automobiles in the Southern Hemisphere, with anthropogenic Pb inputs averaging 60% of total Pb but with large uncertainty. Intra- and inter-annual variations in Pb concentrations and isotopic compositions were evaluated in snow pits samples corresponding to the period 1991-1994. Substantial variations in Pb/ Ba and Pb-206/Pb-207 ratios were detected but the absence of a regular seasonal pattern for these parameters suggests that the transport and deposition of aerosols to the Antarctic ice sheet are complex and vary from year to year. (c) 2005 Elsevier B.V. All rights reserved.
机译:据报道,来自南极洲维多利亚州的蕨类岩心和雪坑样品中的Pb和Ba浓度以及Pb同位素组成可追溯到公元1872年至1994年。从Pb / Ba比值和Pb同位素组成的变化,可以确定两个主要的Pb增强期,分别是1891年至1908年和1948年至1994年。较早的污染事件归因于南半球有色金属生产和煤炭燃烧过程中的铅排放,与南极洲另外两个地区高士地和劳顿穹顶的冰芯/冰芯中报告的同时发生的污染输入相吻合。 。使用Pb同位素系统学计算得出,1897年在维多利亚州沉积的铅中有近50%来自人为排放源。从1948年至1994年是最近的Pb增强时期,与南半球汽车中汽油烷基Pb添加剂的引入和广泛使用有关,人为的Pb输入量平均占总Pb的60%,但不确定性很大。在与1991-1994年相对应的雪坑样品中评估了Pb浓度和同位素组成的年内和年际变化。虽然检测到Pb / Ba和Pb-206 / Pb-207比率有很大变化,但是由于这些参数缺乏规律的季节性变化,这表明气溶胶向南极冰原的运输和沉积非常复杂,并且逐年变化。 (c)2005 Elsevier B.V.保留所有权利。

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