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人类活动和火山喷发对 300 年格陵兰冰芯中环境高氯酸盐影响的证据。

Evidence of Influence of Human Activities and Volcanic Eruptions on Environmental Perchlorate from a 300-Year Greenland Ice Core Record.

机构信息

Department of Chemistry and Biochemistry , South Dakota State University , Avera Health and Science Center , Box 2202, Brookings , South Dakota 57007 , United States.

Department of Physical Sciences , Butte College , Oroville , California 95965 , United States.

出版信息

Environ Sci Technol. 2018 Aug 7;52(15):8373-8380. doi: 10.1021/acs.est.8b01890. Epub 2018 Jul 9.

Abstract

A 300-year (1700-2007) chronological record of environmental perchlorate, reconstructed from high-resolution analysis of a central Greenland ice core, shows that perchlorate levels in the post-1980 atm were two-to-three times those of the pre-1980 environment. While this confirms recent reports of increased perchlorate in Arctic snow since 1980 compared with the levels for the prior decades (1930-1980), the longer Greenland record demonstrates that the Industrial Revolution and other human activities, which emitted large quantities of pollutants and contaminants, did not significantly impact environmental perchlorate, as perchlorate levels remained stable throughout the 18, 19, and much of the 20 centuries. The increased levels since 1980 likely result from enhanced atmospheric perchlorate production, rather than from direct release from perchlorate manufacturing and applications. The enhancement is probably influenced by the emission of organic chlorine compounds in the last several decades. Prior to 1980, no significant long-term temporal trends in perchlorate concentration are observed. Brief (a few years) high-concentration episodes appear frequently over an apparently stable and low background (∼1 ng kg). Several such episodes coincide in time with large explosive volcanic eruptions including the 1912 Novarupta/Katmai eruption in Alaska. It appears that atmospheric perchlorate production is impacted by large eruptions in both high- and low-latitudes, but not by small eruptions and nonexplosive degassing.

摘要

一份对格陵兰中部冰芯进行高分辨率分析得出的长达 300 年(1700-2007 年)的环境高氯酸盐时间序列记录显示,1980 年后大气中的高氯酸盐含量是 1980 年前环境的两到三倍。这证实了最近关于自 1980 年以来北极雪的高氯酸盐含量增加的报告,与前几十年(1930-1980 年)相比,然而,更长的格陵兰记录表明,工业革命和其他人类活动排放了大量的污染物和污染物,并没有对环境高氯酸盐产生显著影响,因为高氯酸盐水平在 18、19 世纪以及 20 世纪的大部分时间都保持稳定。自 1980 年以来,高氯酸盐水平的增加可能是由于大气中高氯酸盐的产生增加,而不是由于直接从高氯酸盐制造和应用中释放。这种增强可能受到过去几十年有机氯化合物排放的影响。在 1980 年之前,没有观察到高氯酸盐浓度的显著长期时间趋势。短暂(几年)的高浓度事件经常出现在明显稳定和低背景(约 1ngkg)之上。其中几个事件与包括阿拉斯加 1912 年诺瓦鲁普塔/卡特迈火山爆发在内的几次大型爆炸火山爆发同时发生。似乎大气中高氯酸盐的产生受到高纬度和低纬度大型火山爆发的影响,但不受小火山爆发和非爆炸放气的影响。

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