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Geophysical Study of Lowland Permafrost in Komi-Nenets Area, North-West Russia

机译:俄罗斯西北部Komi-Nenets地区低地永德冻土的地球物理研究

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We present results of a 5-years (2007-2011) project aiming to new applications of electrical and electromagnetic (EM) ground and airborne techniques in permafrost studies. The study is based on geophysical measurements made at three lowland permafrost research areas and one mountain area, laboratory measurements of sediment samples and on geological and temperature borehole data from the research sites. The study areas are situated in the Northern Komi Republic and the Nenets Autonomous Area in Northwestern Russia (fig. 1a). The field EM and electrical resistivity (ERT) sounding data were inverted to 1D and 2D electrical conductivity models. Especially the electrical models from the lowland tundra area, based on the ERT data, show a very nice correspondence with the ground temperature. The electrical conductivity data collected for typical soils and sediments, both in frozen and in unfrozen state, is the basis for advanced use and interpretation of EM techniques and EM data, and for geophysical modeling of permafrost. The conductivity data give a possibility to calculate how, for example, a particular EM system would work at different kind of permafrost areas, i.e., what scale of structures and problems could be explored by it.
机译:我们有5年(2007- 2011年)项目,旨在永久冻土研究的电气和电磁(EM)地面和机载技术,新的应用程序现在的结果。这项研究是基于三个低地多年冻土的研究领域和一个山区,沉积物样品的实验室测量,并从研究地点的地质和温度钻孔资料进行地球物理测量。该研究区位于北部科米共和​​国与涅涅茨自治区在俄罗斯西北联邦区(图1A)。领域EM和电阻率(ERT)的探测数据被反转以一维和二维导电性模型。特别是从低地苔原地区的电气模型的基础上,ERT数据,显示与地面温度非常好的对应关系。收集典型的土壤和沉积物中,无论是在冷冻和解冻中的状态电导率数据,是先进的使用和EM技术和电磁数据解释的基础,并为永久冻土地球物理模型。电导率数据给出的可能性来计算如何,例如,一个特定的EM系统将在不同类型的多年冻土区,即,什么结构和问题的规模可以用它来探索工作。

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