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Finite Element Simulations of Unconsolidated Keel Actions from First-Year Ice Ridges. - A Comparison of a Numerical Model and Analytical Equations from ISO 19906:2010

机译:第一年冰山脊未固结龙骨作用的有限元模拟。 -ISO 19906:2010中的数值模型和解析方程的比较

摘要

The thesis aimed for an assessment of the current standard for determination of the keel rubble actions from a first-year ice ridge. ISO 19906:2010 (2010) gives regulations for determination of these loads, based on the work of Dolgopolov et al. (1975). The assessment involved a comparison of the ISO recommendations with the results from a numerical finite element (FE) model. Particularly the effect of the width of the structure was a target of investigation. The FE model used the theory of a Continuum Breakage Mechanism (CBM) to describe the rubble keel s material behaviour. The material model was implemented as a user-defined subroutine (developed by Sergey A. Kulyakhtin), and the FE analyses were performed in the ABAQUS software. It was modelled as a coupled Eulerian-Lagrangian (CEL) analysis. This type of analyses are advantageous for large deformations and fluid flows etc., in accordance with the behaviour of an ice ridge. In comparison, the analytical model rests on a Mohr-Coulomb yielding criterion. It was mainly focused on the direct comparison of the two models (the analytical and the numerical) by the predicted keel actions. This parameter compared easily, regardless of the material model in use. In other words, the comparison of the material models came indirectly through the comparison of the keel actions. The reaction forces from the numerical model are highly dependent on the prescribed keel velocities. An increased keel velocity yielded reaction forces that approached the analytical results from Dolgopolov et al. (1975), but it also seemed to spoil the accuracy of the energy balance.The FE model proved to give a linear fit just as the ISO standards, but it was a gentle slope compared to the analytical suggestions. For every unit length increase in structural width, the ISO predicted more than twice (approximately 2.5 times) the keel actions from the FE model. This comparison applies for the FE model with a predefined keel velocity of 2000 mm/s. In addition, the order of magnitude of the maximum forces were significantly lower than the ISO predictions. It means that the FE model and the corresponding keel actions showed a two-way effect compared to the ISO suggestions. It implied that the ISO standard suggests too high keel actions from the unconsolidated part, and the width had less to say for the total force than stated in the standards.
机译:本文旨在评估当前标准,以确定从第一年的冰山脊龙骨瓦砾作用。 ISO 19906:2010(2010)根据Dolgopolov等人的工作给出了确定这些载荷的规定。 (1975)。评估包括将ISO建议与数值有限元(FE)模型的结果进行比较。特别是结构宽度的影响是研究的目标。有限元模型使用连续破坏机制(CBM)的理论来描述瓦砾龙骨的材料行为。材料模型作为用户定义的子例程(由Sergey A. Kulyakhtin开发)实现,并且FE分析在ABAQUS软件中进行。它被建模为欧拉-拉格朗日耦合分析(CEL)。根据冰脊的行为,这种类型的分析有利于大变形和流体流动等。相比之下,分析模型基于Mohr-Coulomb屈服准则。主要侧重于通过预测的龙骨作用直接比较两个模型(分析模型和数值模型)。无论使用哪种材料模型,都可以轻松比较此参数。换句话说,通过龙骨作用的比较间接地进行了材料模型的比较。数值模型产生的反作用力高度依赖于规定的龙骨速度。龙骨速度的增加产生的反作用力接近Dolgopolov等人的分析结果。 (1975年),但它似乎也破坏了能量平衡的准确性。FE模型被证明与ISO标准一样具有线性拟合,但与分析建议相比,它是一个平缓的斜率。对于结构宽度每单位长度的增加,ISO预测FE模型的龙骨作用将超过两倍(大约2.5倍)。该比较适用于具有2000 mm / s的预定义龙骨速度的FE模型。此外,最大作用力的数量级明显低于ISO的预测。这意味着与ISO建议相比,有限元模型和相应的龙骨作用表现出双向效应。这暗示着ISO标准暗示了来自未固结部分的龙骨作用过高,并且对于总力而言宽度不能说是标准中规定的那样。

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    Grevsgård Sjur Moe;

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  • 年度 2015
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