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Titlebook: Ice-Structure Interaction; IUTAM/IAHR Symposium Stephen Jones,Joy Tillotson,Ian J. Jordaan Conference proceedings 1991 Springer-Verlag, Ber

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书目名称Ice-Structure Interaction
副标题IUTAM/IAHR Symposium
编辑Stephen Jones,Joy Tillotson,Ian J. Jordaan
视频video
丛书名称IUTAM Symposia
图书封面Titlebook: Ice-Structure Interaction; IUTAM/IAHR Symposium Stephen Jones,Joy Tillotson,Ian J. Jordaan Conference proceedings 1991 Springer-Verlag, Ber
描述IUTAM-IAHR Symposium on Ice-Structure Interaction Professor Bez Tabarrok, Chairman of the Canadian National Committee (CNC) of the International Union of Theoretical and Applied Mechanics (IUTAM) invited Professor Derek Muggeridge to organize a symposium on ice structure interaction. Dr. Muggeridge readily agreed and prepared a proposal that was endorsed by the CNC and presented to the General Assembly Meeting of IUTAM for their consideration. This Assembly gave its approval and provided the local organizing committee with the names of individuals who were willing to serve on the Scientific Committee. Dr. Muggeridge became chairman of this committee and Dr. Ian Jordaan became co-chairman of this committee as well as chairman of the local organizing committee. The symposium followed the very successful previous meeting, chaired by Professor P. Tryde in Copenhagen, by ten years. Both symposia uti­ lized Springer-Verlag to publish their proceedings. The Faculty of En­ gineering and Applied Science at Memorial University of Newfoundland were particul{lXly pleased to host this prestigious symposium as it marked the twentieth anniversary of its Ocean Engineering Research Centre.
出版日期Conference proceedings 1991
关键词Ice Engineering; Kältetechnik; Meer; Meeresbauten-Technik; Offshore Regions Engineering; Ozeanologie; defo
版次1
doihttps://doi.org/10.1007/978-3-642-84100-2
isbn_softcover978-3-642-84102-6
isbn_ebook978-3-642-84100-2
copyrightSpringer-Verlag, Berlin Heidelberg 1991
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The Use of Tertiary Creep Rates in Ice at High Strains in Compression and Shearxamine ice deforming at <~10. s. and with no visible evidence of cracking or failure, thus strains > 20% take long times to establish in the laboratory. At these large strains, crystal anisotropy plays a most important role in the determination of creep rates..For initially isotropic ice, the concep
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Creep and Settlement of Ice Structures — A Case Historyls were related to the confirmation of heavy oil deposits beneath the bottom of a local lake called Marguerite Lake near BP’s Wolf Lake development. The three wells were about 600 m deep and required approximately 3 days to drill. Light, truck mounted drilling rigs, weighing in total about 130 tonne
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Creep Constitutive Equations for Polycrystalline Ice and Effect of Microcracking rate of polycrystalline ice is largely controlled by processes occuring on non-basal planes. Three main models describing the transient behaviour of polycrystalline ice are presented and discussed. Evidence that the occurrence of the first cracks, in the ductile-brittle transition, is related to a
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Kinetics of Microcracking and Dilatation in Polycrystalline Icemodel can be applied for constant stress as well as constant strain-rate loading conditions. It is based on intragranular dislocation creep enhanced by grain-facet size cracks produced during deformation by the embrittlement process that is caused by an intergranular sliding mechanism. Incorporation
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The Fracture Toughness of Icehness of freshwater ice. Insights and recommendations gained from this experience will be put forward. The discussion will focus on specimen size effects, the question of fracture toughness as a material property, fracture energy, and fracture mechanisms.
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Models for the Deformation Behavior of Viscoelastic Media with Distributed Damage and Their Applicabicted behavior is consistent with that of polycrystalline ice. This theory is quite different from those developed for ice by other investigators. Therefore, besides reviewing the results, we give the underlying mathematical and physical arguments. First, some aspects of linear and nonlinear viscoel
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