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实施监测分解结构:本地地衣作为 2011 年普耶韦火山事件后与连通的巴塔哥尼亚南部森林元素沉积的生物监测物——一项为期 6 年的调查(2006-2012 年)。

Implementing the monitoring breakdown structure: native lichens as biomonitors of element deposition in the southern Patagonian forest connected with the Puyehue volcano event in 2011-a 6-year survey (2006-2012).

机构信息

Department of Management, University of Rome, Sapienza, Via del Castro Laurenziano 9, 00161, Rome, Italy.

Departamento Química Nuclear, GAATEN, Comisión Nacional de Energía Atómica (CNEA), Av. del Libertador 8250, 1429, Buenos Aires, Argentina.

出版信息

Environ Sci Pollut Res Int. 2020 Nov;27(31):38819-38834. doi: 10.1007/s11356-020-10001-0. Epub 2020 Jul 6.

Abstract

This study aims to investigate the airborne elements' deposition by using native Usnea barbata lichens as biomonitors in the forested areas of Tierra del Fuego (TdF, southern Patagonia), an apparently pristine environment. The present study is linked to the volcanic eruption of the Puyehue-Cordón Caulle which started in north Patagonia in June 2011, which gives rise to long-distance transport of pollutants through the atmosphere at 1700 km from our sampling sites. The monitoring breakdown structure (MBS) was applied to three sampling campaigns in 2006 (baseline) ➔ 2011-2012 (3 and 15 months after the volcanic event, respectively). We have on purpose enhanced the information variety endowment: (i) Seventy-one referenced sites were double sampled; (ii) up to 426 composite lichen samples were collected; (iii) twenty-six elements were measured by neutron activation analysis (As, Ba, Br, Ca, Ce, Co, Cr, Cs, Eu, Fe, Hf, K, La, Lu, Na, Rb, Sb, Sc, Se, Sm, Ta, Tb, Th, U, Yb, Zn) for samples of 2011 and 2012 campaigns; (iv) thirteen common elements (As, Ba, Ca, Co, Cr, Cs, Fe, K, Na, Sb, Se, U, Zn) were determined in 2006 for the baseline comparison. The natural contamination by tephras is reflected by lichens more clearly in the 2011 campaign, where Ba, Cr, Na, Ca, Cs, and U showed higher median levels compared with the baseline campaign (2006). Ca, K, and Na were the most accumulated elements after the volcano event and could be associated with the volcanic ashes' deposition. Rare earth elements (REEs) showed no significant bioaccumulation levels between 2011 and 2012, indicating their association with higher lithogenic inputs than volcanic ashes. Using the Earth's crust as reference, nine elements (As, Ba, Br, Ca, K, Na, Sb, Se, and Zn) presented moderate/significant mean enrichment factor (EF) values (> 5). The usefulness of Usnea barbata as test species for direct biomonitoring oriented kinetic studies in areas characterized by a low human impact is confirmed. Eventually, our results confirm that TdF is not an actual pristine environment as earlier supposed.

摘要

本研究旨在利用土生土长的地衣作为生物监测器,研究火地岛(福克兰群岛,巴塔哥尼亚南部)森林地区空气中元素的沉积情况,因为该地区表面上看是一个原始环境。本研究与 2011 年 6 月在北巴塔哥尼亚开始的普耶韦-科登-卡尔内尔火山爆发有关,这次火山爆发导致污染物通过大气长距离传输至距离采样点 1700 公里的地方。监测分解结构(MBS)应用于 2006 年(基线)➔2011-2012 年(火山爆发后分别为 3 个月和 15 个月)的三次采样活动中。我们特意增强了信息多样性:(i)71 个参考点进行了重复采样;(ii)采集了多达 426 个复合地衣样本;(iii)对 2011 年和 2012 年活动的样本进行了中子活化分析(As、Ba、Br、Ca、Ce、Co、Cr、Cs、Eu、Fe、Hf、K、La、Lu、Na、Rb、Sb、Sc、Se、Sm、Ta、Tb、Th、U、Yb、Zn),共测量了 26 种元素;(iv)对 2006 年基线进行了比较,确定了 2011 年和 2012 年活动的 13 种常见元素(As、Ba、Ca、Co、Cr、Cs、Fe、K、Na、Sb、Se、U、Zn)。火山灰造成的自然污染在地衣中更为明显,2011 年的 Ba、Cr、Na、Ca、Cs 和 U 的中值水平高于基线(2006 年)。Ca、K 和 Na 是火山爆发后积累最多的元素,可能与火山灰的沉积有关。与 2011 年相比,稀土元素(REEs)在 2012 年的生物积累水平没有明显变化,表明它们与更高的岩石输入有关,而不是与火山灰有关。以地壳为参考,有九个元素(As、Ba、Br、Ca、K、Na、Sb、Se 和 Zn)的平均富集因子(EF)值(>5)表现出中等/显著富集。证实了地衣作为测试物种,可直接进行以动力学为导向的生物监测,用于人类影响较低的地区。最终,我们的研究结果证实,火地岛并非如先前认为的那样是一个原始环境。

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