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Flexural Strength of Drifting Level First-year Ice in the Barents Sea

机译:巴伦支海第一年冰层漂移强度的抗折强度

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摘要

The AARI performed ice research work in the Barents Sea during the last 10 years (1996-2006). In the course of this work great amount of material was collected on flexural strength of drifting first-year sea ice (138 cantilever beam tests, many tests of small discs). Results of data analysis for level ice are presented in this report; this analysis was performed separately for the south-eastern and north-eastern regions of the Barents Sea. Influence of different ice characteristics exerted on the flexural strength is studied (temperature, salinity, brine volume etc.). Relation is analyzed between the full-scale flexural strength of ice cover determined by the results of the cantilever tests, and the strength corresponding to the tests of small specimens. As the most reliable method of ice flexural strength determination are the cantilever tests cut out of the entire ice thickness. However, these experiments are the most labor-intensive, so the trial was made to obtain empirical relations between the physical properties of ice, strength of small specimens and full-scale flexural strength of level ice.
机译:在过去的10年中(1996-2006年),AARI在巴伦支海进行了冰研究工作。在这项工作的过程中,收集了有关漂移的第一年海冰的抗弯强度的大量材料(138悬臂梁测试,许多小圆盘测试)。本报告介绍了冰面数据分析的结果;该分析是分别对巴伦支海的东南和东北地区进行的。研究了不同冰特性对弯曲强度的影响(温度,盐度,盐水量等)。分析了由悬臂测试结果确定的冰盖的全尺寸挠曲强度与对应于小样本测试的强度之间的关系。作为确定冰层抗弯强度的最可靠方法,悬臂测试会切掉整个冰层的厚度。但是,这些实验是最费力的,因此进行了试验以获取冰的物理性质,小样本强度和水平冰的满度弯曲强度之间的经验关系。

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