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过去 250 年来日本高山湖泊中金属沉积的沉积记录:东亚地区空气中 Sb 和 In 的近期富集。

Sedimentary records of metal deposition in Japanese alpine lakes for the last 250 years: recent enrichment of airborne Sb and In in East Asia.

机构信息

Senior Research Fellow Center, Ehime University, 2-5 Bunkyo-cho, Matsuyama 790-8577, Japan.

出版信息

Sci Total Environ. 2013 Jan 1;442:189-97. doi: 10.1016/j.scitotenv.2012.10.037. Epub 2012 Nov 22.

Abstract

Concentrations of 18 elements, including Sb, In, Sn, and Bi, were measured in sediment cores from two pristine alpine lakes on Mount Hachimantai, northern Japan, representing the past 250 years. Vertical variations in concentrations are better explained by atmospheric metal deposition than by diagenetic redistribution of Fe and Mn hydroxide and organic matter. Anthropogenic metal fluxes were estimated from (210)Pb-derived accumulation rates and metal concentrations in excess of the Al-normalized mean background concentration before 1850. Anthropogenic fluxes of Sb and In showed gradual increases starting around 1900 in both lakes, and marked increases after 1980. Comparison of Sb/Pb and Pb stable isotope ratios in sediments with those in aerosols of China or northern Japan and Japanese source materials (recent traffic- and incinerator-derived dust) suggest that the markedly elevated Sb flux after 1980 resulted primarily from enhanced long-range transport in aerosols containing Sb and Pb from coal combustion on the Asian continent. The fluxes of In, Sn, and Bi which are present in Chinese coal showed increasing trends similar to Sb for both study lakes. This suggests that the same source although incinerators in Japan may not be ruled out as sources of In. The sedimentary records for the last 250 years indicate that atmospheric pollution of Sb and In in East Asia have intensified during recent decades.

摘要

对来自日本北部八幡山的两个原始高山湖泊的沉积物岩芯中 18 种元素(包括 Sb、In、Sn 和 Bi)的浓度进行了测量,这些元素反映了过去 250 年的情况。浓度的垂直变化可以更好地用大气金属沉积来解释,而不是用 Fe 和 Mn 氢氧化物和有机物的成岩再分配来解释。根据(210)Pb 衍生的积累率和 1850 年以前超过 Al 归一化平均背景浓度的金属浓度,估算了人为金属通量。两个湖泊中 Sb 和 In 的人为通量自 1900 年左右开始逐渐增加,并在 1980 年后显著增加。对沉积物中 Sb/Pb 和 Pb 稳定同位素比值与中国或日本北部气溶胶以及日本源材料(最近的交通和焚烧炉衍生尘埃)的比较表明,1980 年后 Sb 通量的显著增加主要是由于亚洲大陆燃煤气溶胶中 Sb 和 Pb 的长距离传输增强所致。在中国煤中存在的 In、Sn 和 Bi 的通量也呈现出与 Sb 相似的上升趋势,这表明同样的来源,尽管日本的焚烧炉也可能不是 In 的来源。过去 250 年的沉积记录表明,东亚地区 Sb 和 In 的大气污染在最近几十年有所加剧。

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