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• W2754726109 abstract "빙하코어의 전기 전도도는 주로 얼음의 산성도에 의하여 결정되는 것으로 알려져 있다. 빙하코어의 산성도를 두드러지게 증가시키는 대표적인 물질로는 화산활동에 의해 대기로 방출된 H2SO4, HNO3, HCl, HF가 있다. 따라서 전기 전도도 측정법(electrical conductivity measurement, ECM)을 빙하코어에 적용하였을 때 관찰되는 뚜렷한 피크들은 과거 화산활동을 지시할 수 있다. 만일 분출 시기가 알려진 화산 활동이 확인된다면 이를 빙하코어의 연대측정에 활용할 수 있다. 본 연구에서는 2013-2014년 남극 하계 시기에 한-이태리 공동시추 프로그램을 통하여 동남극 GV7(70°41" @default.
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• W2754726109 date "2017-08-30" @default.
• W2754726109 modified "2023-09-25" @default.
• W2754726109 title "Electrical Conductivity Characteristics of a Shallow Ice Core from GV7, East Antarctica" @default.
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• W2754726109 doi "https://doi.org/10.14770/jgsk.2017.53.4.521" @default.
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