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Submarine permafrost in the Laptev sea

机译:潜水艇在Laptev海中的Permafrost

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The article presents results of permafrost scientific research in theKhatanga bay of the Laptev sea. Field works were organized in earlyspring 2017 by Rosneft Oil Company with participation of LomonosovMoscow State University, Far Eastern Federal University and ArcticResearch Centre. Research included geocryological drilling for subseapermafrost from the land fast ice, geophysical surveys and laboratorytests of thawed and frozen rock monoliths. In order to obtaininformation about subsea permafrost 13 core wells were drilled fromthe land fast ice in the Nordvik bay (sea depth ~15 m) to a depth of 50m with. Core data helped to define thermal characteristics of more than300 permafrost monoliths. With the means of special equipment morethan 1000 points of electromagnetic soundings were processed.Laboratory studies of the obtained samples combined withelectromagnetic sounding information allowed to construct thepermafrost horizon in the Nordvik bay and its immersion’s behavior toa depth of 200 m. Estimation of the permafrost distribution to thedepths of 500 m is presented in the paper as well as permafrostthickness dynamics simulation for 50 years.
机译:本文提出了多年冻土科学研究的结果Kakatanga湾的Laptev海。现场工程早期组织2017年春季由Rosneft Loc公司参与Lomonosov莫斯科国立大学,远东联邦大学和北极研究中心。研究包括海底的地理统计钻探来自土地快速冰,地球物理调查和实验室的永久冻土解冻和冷冻岩石雄性的测试。为了获得有关Hemafrost 13核井井的信息Nordvik湾的土地快速冰(海景〜15米)深度为50m。核心数据有助于定义更多的热特性300多年冻土的雄黄。用特殊设备的手段更多处理了1000点电磁探测。所获得的样品的实验室研究结合电磁探测信息允许构建诺德维克湾的永久冻土地平线及其浸入行为深度为200米。估计永久冻土分布对本文介绍了500米的深度以及永久冻土厚度动力学模拟50年。

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