210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.

The results of 210Pb measurements in the lake sediment core from Antarctica are reported: the relative specific activities of 210Pb in the lake sediment were found to decrease exponentially with the depth in the study area; the sedimentation rate of the lake is about 0.072 cm/a. This paper shows tha...

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Bibliographic Details
Main Authors: Ye, Zhao, Cuihua, Xu
Format: Article in Journal/Newspaper
Language:English
Published: Polar Research Institute of China - PRIC 1997
Subjects:
Online Access:http://library.arcticportal.org/2124/
http://library.arcticportal.org/2124/1/A701.004.pdf
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spelling ftarcticportal:oai:generic.eprints.org:2124 2023-06-11T04:02:59+02:00 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica. Ye, Zhao Cuihua, Xu 1997-06 application/pdf http://library.arcticportal.org/2124/ http://library.arcticportal.org/2124/1/A701.004.pdf en eng Polar Research Institute of China - PRIC http://library.arcticportal.org/2124/1/A701.004.pdf Ye, Zhao and Cuihua, Xu (1997) 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica. Advances in Polar Science, 8 (1). pp. 33-36. Article PeerReviewed 1997 ftarcticportal 2023-04-26T22:52:43Z The results of 210Pb measurements in the lake sediment core from Antarctica are reported: the relative specific activities of 210Pb in the lake sediment were found to decrease exponentially with the depth in the study area; the sedimentation rate of the lake is about 0.072 cm/a. This paper shows that 210Pb method is applicable to Antarctic lake sediment, and during the 1960's the atmospheric nuclear tests have an effect on the rate of 210Pb deposition in Antarctica. Article in Journal/Newspaper Advances in Polar Science Antarc* Antarctic Antarctica Polar Science Polar Science Arctic Portal Library Antarctic Great Wall Station ENVELOPE(-58.970,-58.970,-62.217,-62.217)
institution Open Polar
collection Arctic Portal Library
op_collection_id ftarcticportal
language English
description The results of 210Pb measurements in the lake sediment core from Antarctica are reported: the relative specific activities of 210Pb in the lake sediment were found to decrease exponentially with the depth in the study area; the sedimentation rate of the lake is about 0.072 cm/a. This paper shows that 210Pb method is applicable to Antarctic lake sediment, and during the 1960's the atmospheric nuclear tests have an effect on the rate of 210Pb deposition in Antarctica.
format Article in Journal/Newspaper
author Ye, Zhao
Cuihua, Xu
spellingShingle Ye, Zhao
Cuihua, Xu
210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
author_facet Ye, Zhao
Cuihua, Xu
author_sort Ye, Zhao
title 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
title_short 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
title_full 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
title_fullStr 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
title_full_unstemmed 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica.
title_sort 210pb distribution characteristics in the lake sediment core at great wall station, antarctica.
publisher Polar Research Institute of China - PRIC
publishDate 1997
url http://library.arcticportal.org/2124/
http://library.arcticportal.org/2124/1/A701.004.pdf
long_lat ENVELOPE(-58.970,-58.970,-62.217,-62.217)
geographic Antarctic
Great Wall Station
geographic_facet Antarctic
Great Wall Station
genre Advances in Polar Science
Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
genre_facet Advances in Polar Science
Antarc*
Antarctic
Antarctica
Polar Science
Polar Science
op_relation http://library.arcticportal.org/2124/1/A701.004.pdf
Ye, Zhao and Cuihua, Xu (1997) 210Pb distribution characteristics in the lake sediment core at Great Wall Station, Antarctica. Advances in Polar Science, 8 (1). pp. 33-36.
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