Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect

Abstract Background The peak suppression effect, which suppresses the argon isotope signal due to the incomplete cleaning of gas from geological samples during measurement, is found in volatile-rich samples using the ARGUS VI noble gas mass spectrometer and its sample preparation system. Such effect...

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Main Authors: Jeongmin Kim, In-Hwa Cho
Format: Article
Language:English
Published: SpringerOpen 2020-02-01
Series:Journal of Analytical Science and Technology
Subjects:
Online Access:http://link.springer.com/article/10.1186/s40543-020-00207-9
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spelling doaj-9e1253a4bea3439c9856d05d09b8755d2020-11-25T02:14:08ZengSpringerOpenJournal of Analytical Science and Technology2093-33712020-02-0111111310.1186/s40543-020-00207-9Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effectJeongmin Kim0In-Hwa Cho1Division of Earth and Environment Science, Korea Basic Science InstituteDivision of Earth and Environment Science, Korea Basic Science InstituteAbstract Background The peak suppression effect, which suppresses the argon isotope signal due to the incomplete cleaning of gas from geological samples during measurement, is found in volatile-rich samples using the ARGUS VI noble gas mass spectrometer and its sample preparation system. Such effect hampers getting the precise isotope ratio essential for the 40Ar/39Ar age calculation. Findings The addition of one hot-getter and three room-temperature getters to the sample preparation system can effectively eliminate the peak suppression effect for several milligrams of sample during argon measurement to yield highly plausible 40Ar/39Ar ages of Quaternary volcanic rocks. Conclusions The modified preparation system makes it possible to get highly precise zero-time isotope signals, and thereby a geologically plausible 40Ar/39Ar age, especially for a small amount of volatile-rich samples.http://link.springer.com/article/10.1186/s40543-020-00207-940Ar/39Ar ageNoble gas mass spectrometerQuaternaryPeak suppressionGetters
collection DOAJ
language English
format Article
sources DOAJ
author Jeongmin Kim
In-Hwa Cho
spellingShingle Jeongmin Kim
In-Hwa Cho
Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
Journal of Analytical Science and Technology
40Ar/39Ar age
Noble gas mass spectrometer
Quaternary
Peak suppression
Getters
author_facet Jeongmin Kim
In-Hwa Cho
author_sort Jeongmin Kim
title Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
title_short Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
title_full Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
title_fullStr Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
title_full_unstemmed Improvement of 40Ar/39Ar age determinations for Quaternary basaltic rocks by eliminating the peak suppression effect
title_sort improvement of 40ar/39ar age determinations for quaternary basaltic rocks by eliminating the peak suppression effect
publisher SpringerOpen
series Journal of Analytical Science and Technology
issn 2093-3371
publishDate 2020-02-01
description Abstract Background The peak suppression effect, which suppresses the argon isotope signal due to the incomplete cleaning of gas from geological samples during measurement, is found in volatile-rich samples using the ARGUS VI noble gas mass spectrometer and its sample preparation system. Such effect hampers getting the precise isotope ratio essential for the 40Ar/39Ar age calculation. Findings The addition of one hot-getter and three room-temperature getters to the sample preparation system can effectively eliminate the peak suppression effect for several milligrams of sample during argon measurement to yield highly plausible 40Ar/39Ar ages of Quaternary volcanic rocks. Conclusions The modified preparation system makes it possible to get highly precise zero-time isotope signals, and thereby a geologically plausible 40Ar/39Ar age, especially for a small amount of volatile-rich samples.
topic 40Ar/39Ar age
Noble gas mass spectrometer
Quaternary
Peak suppression
Getters
url http://link.springer.com/article/10.1186/s40543-020-00207-9
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