1998年南极中山站海洋气溶胶的化学组成及其来源判别
从1998年3月7日至1999年3月2日历时12个月,在南极中山站连续采集52个海洋气溶胶样品,提供全部样品的13种化学元素铜、铅、锌、镉、铁、铝、锰、铬、钒、钾、钠、钙、镁含量的实测值.研究表明中山站气溶胶化学成分的含量具有季节性变化的特征.通过富集因子、相关分析、因子分析等方法判别中山站气溶胶化学成分的来源. Fifty two aerosol samples of 6~7 d duration were collected from March1998 through March1999 at the Zhongshan Station in Antarctica. The conten...
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ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/154985 2023-05-15T13:58:45+02:00 1998年南极中山站海洋气溶胶的化学组成及其来源判别 The chemical composition of marine aerosol over Zhongshan Station in Antarctica and its sources discrimination in 1998 黄自强 暨卫东 杨绪林 黄荣坦 汤荣坤 于涛 张功勋 2005-05-13 http://dspace.xmu.edu.cn/handle/2288/154985 zh_CN chi 海洋学报(中文版),2005,(03):60-67 0253-4193 SEAC200503008 http://dspace.xmu.edu.cn/handle/2288/154985 大气科学 南极 海洋气溶胶 化学组成 来源判别 atmosphere science Antarctica marine aerosol chemical composition source discrimination Article 2005 ftxiamenuniv 2020-07-21T13:00:56Z 从1998年3月7日至1999年3月2日历时12个月,在南极中山站连续采集52个海洋气溶胶样品,提供全部样品的13种化学元素铜、铅、锌、镉、铁、铝、锰、铬、钒、钾、钠、钙、镁含量的实测值.研究表明中山站气溶胶化学成分的含量具有季节性变化的特征.通过富集因子、相关分析、因子分析等方法判别中山站气溶胶化学成分的来源. Fifty two aerosol samples of 6~7 d duration were collected from March1998 through March1999 at the Zhongshan Station in Antarctica. The content of 13 chemical elements is presented:Cu,Pb,Zn,Cd,Fe,Al,Mn,Cr,V,K,Na,Ca and Mg. The study results demonstrate that the content of elements in marine aerosol at the Zhongshan Station appeared to be characteristics of seasonal variation, which were related to features of meteorological element. Meanwhile sources of the elements in the marine aerosols are discriminated using methods of enrichment factor, correlation analysis and factor analysis. 国家自然科学基金资助项目(49976022). Article in Journal/Newspaper Antarc* Antarctica Xiamen University Institutional Repository Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Zhongshan Station ENVELOPE(76.371,76.371,-69.373,-69.373) |
institution |
Open Polar |
collection |
Xiamen University Institutional Repository |
op_collection_id |
ftxiamenuniv |
language |
Chinese |
topic |
大气科学 南极 海洋气溶胶 化学组成 来源判别 atmosphere science Antarctica marine aerosol chemical composition source discrimination |
spellingShingle |
大气科学 南极 海洋气溶胶 化学组成 来源判别 atmosphere science Antarctica marine aerosol chemical composition source discrimination 黄自强 暨卫东 杨绪林 黄荣坦 汤荣坤 于涛 张功勋 1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
topic_facet |
大气科学 南极 海洋气溶胶 化学组成 来源判别 atmosphere science Antarctica marine aerosol chemical composition source discrimination |
description |
从1998年3月7日至1999年3月2日历时12个月,在南极中山站连续采集52个海洋气溶胶样品,提供全部样品的13种化学元素铜、铅、锌、镉、铁、铝、锰、铬、钒、钾、钠、钙、镁含量的实测值.研究表明中山站气溶胶化学成分的含量具有季节性变化的特征.通过富集因子、相关分析、因子分析等方法判别中山站气溶胶化学成分的来源. Fifty two aerosol samples of 6~7 d duration were collected from March1998 through March1999 at the Zhongshan Station in Antarctica. The content of 13 chemical elements is presented:Cu,Pb,Zn,Cd,Fe,Al,Mn,Cr,V,K,Na,Ca and Mg. The study results demonstrate that the content of elements in marine aerosol at the Zhongshan Station appeared to be characteristics of seasonal variation, which were related to features of meteorological element. Meanwhile sources of the elements in the marine aerosols are discriminated using methods of enrichment factor, correlation analysis and factor analysis. 国家自然科学基金资助项目(49976022). |
format |
Article in Journal/Newspaper |
author |
黄自强 暨卫东 杨绪林 黄荣坦 汤荣坤 于涛 张功勋 |
author_facet |
黄自强 暨卫东 杨绪林 黄荣坦 汤荣坤 于涛 张功勋 |
author_sort |
黄自强 |
title |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
title_short |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
title_full |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
title_fullStr |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
title_full_unstemmed |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
title_sort |
1998年南极中山站海洋气溶胶的化学组成及其来源判别 |
publishDate |
2005 |
url |
http://dspace.xmu.edu.cn/handle/2288/154985 |
long_lat |
ENVELOPE(76.371,76.371,-69.373,-69.373) ENVELOPE(76.371,76.371,-69.373,-69.373) |
geographic |
Zhongshan Zhongshan Station |
geographic_facet |
Zhongshan Zhongshan Station |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
海洋学报(中文版),2005,(03):60-67 0253-4193 SEAC200503008 http://dspace.xmu.edu.cn/handle/2288/154985 |
_version_ |
1766267083335663616 |