北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪

2008年7—9月于北极楚科奇海采集了17个站位不同深度的海水水样,用吹扫捕集与气相色谱相结合的方法分析氟氯烃CfC11(CCl3f)的含量分布,并结合温度、盐度、溶解氧等水文和海洋化学数据用于楚科奇海水的化学示踪研究.结果表明,楚科奇海表层水中CfC-11的含量在2.95--8.81 PMOl/kg之间,表层水与30 M层水还没完全混合;HEr-Ald浅滩南边为夏季太平洋入流水,而以北仍然为冬季陆架残留水;CfC-11高值进一步证实阿纳德尔水、白令海陆架水与阿拉斯加沿岸流在bArrOW峡谷混合,CfC-11低值则证实北极中层水增暖现象,CfC-11表层含量的显著增加表明楚科奇海陆坡区离岸较近...

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Main Authors: 郑淑兰, 邓永智, 袁晓婕, 李文权
Format: Article in Journal/Newspaper
Language:Chinese
Published: 2010
Subjects:
Online Access:http://dspace.xmu.edu.cn/handle/2288/104248
id ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/104248
record_format openpolar
spelling ftxiamenuniv:oai:dspace.xmu.edu.cn:2288/104248 2023-05-15T13:24:42+02:00 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪 Distribution Feature of Trichlorofluoromethane and Its Chemical Tracer Study in the North Pole of Chukchi Sea 郑淑兰 邓永智 袁晓婕 李文权 2010 http://dspace.xmu.edu.cn/handle/2288/104248 zh_CN chi 厦门大学学报(自然科学版),2010,(4):103-109 0438-0479 XDZK201004022 http://dspace.xmu.edu.cn/handle/2288/104248 楚科奇海 氟氯烃 分布特征 示踪研究 Chukchi Sea chlorofluorocarbons distribution feature trace study Article 2010 ftxiamenuniv 2020-07-21T12:24:58Z 2008年7—9月于北极楚科奇海采集了17个站位不同深度的海水水样,用吹扫捕集与气相色谱相结合的方法分析氟氯烃CfC11(CCl3f)的含量分布,并结合温度、盐度、溶解氧等水文和海洋化学数据用于楚科奇海水的化学示踪研究.结果表明,楚科奇海表层水中CfC-11的含量在2.95--8.81 PMOl/kg之间,表层水与30 M层水还没完全混合;HEr-Ald浅滩南边为夏季太平洋入流水,而以北仍然为冬季陆架残留水;CfC-11高值进一步证实阿纳德尔水、白令海陆架水与阿拉斯加沿岸流在bArrOW峡谷混合,CfC-11低值则证实北极中层水增暖现象,CfC-11表层含量的显著增加表明楚科奇海陆坡区离岸较近的地方受到河流径流的影响. Seawater samples were collected at 17 stations in the Chukchi Sea from July to September in 2008,and CCl3F(CFC-11) was measured with gas chromatography coupled with a purge-trap concentrator system.The datas of CFC-11 were used for seawater tracer study together with temperature,salinity and DO.The results showed that the concentrations of CFC-11 in surface water were 2.95 pmol/kg to 8.81 pmol/kg,and the shallower than 30 m water had not commingle entirety,and to the south of the Herald Shoal was summer Pacific Ocean water,but to the north was winter Chukchi Sea residual water.High amount of CFC-11 confirmed that the Anadyr water,Bering sea shelf water and Alaska coastal current were mixed in the Barrow Canyon,and low amount of CFC-11 approved the phenomenon of warming of middle water in north pole,the markely increase of CFC-11 in surface water meant that the less distant offshore stations had great influence by river stream. 国家自然科学基金(40276035) Article in Journal/Newspaper Anadyr Anadyr' Barrow Bering Sea Chukchi Chukchi Sea North Pole Alaska Xiamen University Institutional Repository Anadyr ENVELOPE(177.510,177.510,64.734,64.734) Anadyr’ ENVELOPE(176.233,176.233,64.882,64.882) Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) Bering Sea Chukchi Sea North Pole Pacific
institution Open Polar
collection Xiamen University Institutional Repository
op_collection_id ftxiamenuniv
language Chinese
topic 楚科奇海
氟氯烃
分布特征
示踪研究
Chukchi Sea
chlorofluorocarbons
distribution feature
trace study
spellingShingle 楚科奇海
氟氯烃
分布特征
示踪研究
Chukchi Sea
chlorofluorocarbons
distribution feature
trace study
郑淑兰
邓永智
袁晓婕
李文权
北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
topic_facet 楚科奇海
氟氯烃
分布特征
示踪研究
Chukchi Sea
chlorofluorocarbons
distribution feature
trace study
description 2008年7—9月于北极楚科奇海采集了17个站位不同深度的海水水样,用吹扫捕集与气相色谱相结合的方法分析氟氯烃CfC11(CCl3f)的含量分布,并结合温度、盐度、溶解氧等水文和海洋化学数据用于楚科奇海水的化学示踪研究.结果表明,楚科奇海表层水中CfC-11的含量在2.95--8.81 PMOl/kg之间,表层水与30 M层水还没完全混合;HEr-Ald浅滩南边为夏季太平洋入流水,而以北仍然为冬季陆架残留水;CfC-11高值进一步证实阿纳德尔水、白令海陆架水与阿拉斯加沿岸流在bArrOW峡谷混合,CfC-11低值则证实北极中层水增暖现象,CfC-11表层含量的显著增加表明楚科奇海陆坡区离岸较近的地方受到河流径流的影响. Seawater samples were collected at 17 stations in the Chukchi Sea from July to September in 2008,and CCl3F(CFC-11) was measured with gas chromatography coupled with a purge-trap concentrator system.The datas of CFC-11 were used for seawater tracer study together with temperature,salinity and DO.The results showed that the concentrations of CFC-11 in surface water were 2.95 pmol/kg to 8.81 pmol/kg,and the shallower than 30 m water had not commingle entirety,and to the south of the Herald Shoal was summer Pacific Ocean water,but to the north was winter Chukchi Sea residual water.High amount of CFC-11 confirmed that the Anadyr water,Bering sea shelf water and Alaska coastal current were mixed in the Barrow Canyon,and low amount of CFC-11 approved the phenomenon of warming of middle water in north pole,the markely increase of CFC-11 in surface water meant that the less distant offshore stations had great influence by river stream. 国家自然科学基金(40276035)
format Article in Journal/Newspaper
author 郑淑兰
邓永智
袁晓婕
李文权
author_facet 郑淑兰
邓永智
袁晓婕
李文权
author_sort 郑淑兰
title 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
title_short 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
title_full 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
title_fullStr 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
title_full_unstemmed 北极楚科奇海氟氯烃CFC-11的分布特征及其化学示踪
title_sort 北极楚科奇海氟氯烃cfc-11的分布特征及其化学示踪
publishDate 2010
url http://dspace.xmu.edu.cn/handle/2288/104248
long_lat ENVELOPE(177.510,177.510,64.734,64.734)
ENVELOPE(176.233,176.233,64.882,64.882)
ENVELOPE(-154.000,-154.000,72.500,72.500)
geographic Anadyr
Anadyr’
Barrow Canyon
Bering Sea
Chukchi Sea
North Pole
Pacific
geographic_facet Anadyr
Anadyr’
Barrow Canyon
Bering Sea
Chukchi Sea
North Pole
Pacific
genre Anadyr
Anadyr'
Barrow
Bering Sea
Chukchi
Chukchi Sea
North Pole
Alaska
genre_facet Anadyr
Anadyr'
Barrow
Bering Sea
Chukchi
Chukchi Sea
North Pole
Alaska
op_relation 厦门大学学报(自然科学版),2010,(4):103-109
0438-0479
XDZK201004022
http://dspace.xmu.edu.cn/handle/2288/104248
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