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Internal structure and porosity of ice ridges investigated at «North Pole-38» drifting station

机译:«North Pole-38»漂流站研究冰脊的内部结构和孔隙度

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The paper presents the investigation results of morphometric characteristics of three first-year ice ridges conducted in March-June 2011 at «North Pole-38» drifting station. The height of the ice ridge sail ranged within 3.3-6.1 m; keel draft, from 10.2 to 18.9 m. These studies were conducted using electric thermal drilling with computer recording of the penetration rate. Boreholes were drilled along the cross-section of the ridge crest at 0.5 m intervals. Cross-sectional profiles of ice ridges are illustrated. In each borehole, ice ridge porosity was calculated as the ratio of the length of all voids to total length of the borehole. Distribution of ice ridge porosity along the cross-section seems to be rather regular. Depth-wise distribution of volume content of solid ice phase is shown for the investigated ice ridges. Average thickness of consolidated layer of ice ridges ranged within 0.8... 2.6 m.
机译:本文介绍了2011年3月至2011年6月在“北极38”漂流站进行的3个第一年冰脊形态特征的调查结果。冰脊帆的高度在3.3-6.1 m之间;龙骨吃水,从10.2至18.9 m。这些研究是使用电热钻并通过计算机记录渗透速率进行的。沿脊顶的横截面以0.5 m的间隔钻孔。示出了冰脊的横截面轮廓。在每个钻孔中,将冰孔孔隙率计算为所有空隙的长度与钻孔总长度之比。沿横截面的冰脊孔隙度分布似乎相当规则。显示了所研究的冰脊的固态冰相体积含量的深度分布。冰脊固结层的平均厚度在0.8到2.6 m之间。

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