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Breaking Pattern of Semi-infinite Ice Sheets During Bending Failures Against Sloping Structures

机译:在弯曲结构的弯曲失败期间打破半无限冰盖的图案

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Y Sloping geometries are often adopted by ice-class vessels or cold region offshore structures at the waterline because of their ability to induce ice sheet bending failures. Therefore, bending failures of semi-infinite ice sheets against sloping structures have been investigated extensively. Recently, interest has grown in real-time simulations of ice-structure interactions because of their application potentials. For such purposes, analytical or semi-analytical models for bending failure events with different ice breaking patterns can be implemented into the real-time simulator for its accuracy and efficiency. Predictions of the ice breaking pattern are thus essential to the accuracy of real-time simulators since different models should be utilized for different breaking patterns. However, most existing theoretical models for semi-infinite ice sheet bending failures against sloping structures focus on the maximum ice load on the structure during the entire loading process, without conclusions on the bending failure processes (i.e., radial-before-circumferential or circumferential-before-radial cracking pattern). In this study, the criterion for breaking pattern determinations is established based on nondimensional formulae. It is found that the breaking pattern transfers from radial-before-circumferential to circumferential-before-radial cracking as the structural waterline width increases and the ice thickness decreases, with the transition point occurring when the structural waterline width is equal to 3.65 times the characteristic length of the ice sheet.
机译:Y倾斜的几何形状通常由水线的冰级船只或冷区域近海结构采用,因为它们能够诱导冰盖弯曲故障。因此,已经广泛研究了半无限冰片对倾斜结构的半无限冰片弯曲的故障。最近,由于其应用势利,利息已经在冰结构相互作用的实时模拟中发展。对于这种目的,可以在实时模拟器中实现用于弯曲失效事件的分析或半分析模型,以实现其准确性和效率。因此,冰破碎模式的预测对于实时模拟器的准确性是必不可少的,因为不同的模型应该用于不同的断裂模式。然而,用于半无限冰盖弯曲故障的最现有的理论模型,用于倾斜结构的倾斜故障关注整个装载过程中结构上的最大冰负荷,而无需结论弯曲失效过程(即,径向 - 圆周或圆周 - 径向裂缝模式)。在本研究中,基于非潜能公式建立破坏模式确定的标准。结果发现,随着结构水线宽度的增加,随着结构水线宽度等于特征的3.65倍,冰厚度降低,断裂图案从径向前径向裂缝转移到周向前径向裂缝中。当结构水线宽度等于特征的3.65倍时,发生过渡点冰盖的长度。

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