中雅库特(东西伯利亚)永久冻土带和水流关键组分中18O和D的稳定同位素

IF 0.7 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Led i Sneg-Ice and Snow Pub Date : 2019-09-21 DOI:10.15356/2076-6734-2019-3-414

A. Galanin, M. Pavlova, T. Papina, A. N. Eyrikh, N. Pavlova

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引用次数: 0

摘要

A.A. Galanin1*， M.R. Pavlova1, T.S. Papina2, A.N. Eyrikh2, N.A. Pavlova1 [j] .俄罗斯科学院西伯利亚分所，melnikov冻土研究所，雅库茨克，俄罗斯;2俄罗斯科学院西伯利亚分院水与环境问题研究所，俄罗斯巴尔瑙尔*agalanin@gmail . .com收稿日期:2018年12月8日/修改日期:2019年3月24日/收稿日期:2019年6月13日

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Stable isotopes of 18O and D in key components of water flows and the permafrost zone of Central Yakutia (Eastern Siberia)

Stable isotopes of 18O and D in key components of water flows and the permafrost zone of Central Yakutia (Eastern Siberia) A.A. Galanin1*, M.R. Pavlova1, T.S. Papina2, A.N. Eyrikh2, N.A. Pavlova1 1Melnikov Permafrost Institute, Siberian Branch, Russian Academy of Sciences, Yakutsk, Russia; 2Institute for Water and Environmental Problems, Siberian Branch, Russian Academy of Sciences, Barnaul, Russia *agalanin@gmail .com Received December 8, 2018 / Revised March 24, 2019 / Accepted June 13, 2019

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来源期刊

Led i Sneg-Ice and Snow GEOSCIENCES, MULTIDISCIPLINARY-

CiteScore

1.50

自引率

42.90%

发文量

审稿时长

8 weeks

期刊介绍： The journal was established with the aim of publishing new research results of the Earth cryosphere. Results of works in physics, mechanics, geophysics, and geochemistry of snow and ice are published here together with geographical aspects of the snow-ice phenomena occurrence in their interaction with other components of the environment. The challenge was to discuss the latest results of investigations carried out on Russia’s territory and works performed by Russian investigators together with foreign colleagues. Editorial board works in collaboration with Glaciological Association that is professional community of specialists in glaciology from all republics of the Former Soviet Union which are now new independent states. The journal serves as a platform for the presentation and discussion of new discoveries and results which help to elucidate the state of the Earth’s cryosphere and the characteristics of the evolution of the snow-ice processes and phenomena under the current conditions of rapid climate change.