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DESIGN OF A FIELD TEST FOR MEASURING THE FRACTURE TOUGHNESS OF SEA ICE

机译:测量海冰断裂韧性的现场试验

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Fracture of sea ice plays an important role in determining the ice loads on offshore structures. The importance of incorporating fracture mechanics principles into ice load calculation has long been recognised. However, any method developed based on fracture mechanics demands the knowledge of this rather important parameter, i.e., the fracture toughness of sea ice. There have been controversies about the scale invariant fracture toughness K_(IC) of sea ice for over 25 years now, e.g., K_(IC) = 115 kPam~(1/2) was reported from laboratory measurement while K_(IC) = 250 kPam~(1/2) was reported from field scale. The size of the test specimen and the loading rate are the two major issues often raised when questioning the validity of a fracture toughness test. In view of such discrepancy in the reported values of fracture toughness, the Norwegian University of Science and Technology (NTNU) hosting the research-based innovation centre (SAMCoT), is making an effort to attack this long-existing problem. Two field tests in Svea at Spitsbergen are planned in the winters of 2015 and 2016. The rationale of the test is rather straightforward, i.e., we shall fracture a large enough ice floe with fast enough loading rate. The test in 2015 is a preparatory campaign for the main testing campaign in 2016. Based on existing fracture mechanics knowledge and precursors' experience with fracture toughness test, this paper describes the design process of the first test campaign with emphasis on the theoretical analysis. Interesting results regarding the size and loading rate requirement are obtained. By this paper, we hope to expose our work at this early stage to discussions, suggestions and criticism from worldwide experts in the field. Based on this test design, the first test campaign shall be carried out between March 20th-27th, 2015, after which we report the test results in a different paper separately.
机译:海冰断裂起着决定对海上结构的冰荷载重要的作用。结合断裂力学原理入冰负荷计算的重要性长期以来被认可。然而,任何方法开发了基于断裂力学要求这个相当重要的参数,即海冰断裂韧性的知识。已经有关于海冰的尺度不变断裂韧性K_(IC)超过25年的争议现在,例如,K_(IC)= 115〜kPam(1/2)从实验室测量报告而K_(IC)= 250 kPam〜(1/2)中的溶液从场规模的报道。试样的尺寸和负荷率都在质疑一个断裂韧性测试的有效性时,经常提出的两个主要问题。鉴于断裂韧性的报告值这样的差异,主持研究为基础的创新中心(SAMCoT)科学技术的挪威大学(师大),正努力去攻击这个长期存在的问题。在两个的Svea现场测试在斯匹次卑尔根计划于2015年和2016年冬天测试的基本原理相当简单,即我们将断裂足够大的浮冰有足够快的负荷率。在2015年的测试是基于现有的断裂力学知识和前体与断裂韧性的测试经验,在2016年的主要测试的竞选筹备活动,本文介绍了重点在理论分析的第一个测试活动的设计过程。获得关于尺寸和负荷率要求有趣的结果。通过本文,我们希望在这个早期阶段的讨论,建议和从该领域全球专家的批评暴露我们的工作。在此基础上测试设计,第一个测试活动将3月20日至27日,2015年,在这之后我们分别报告在不同的纸张上的测试结果之间进行。

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