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

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Conference proceedings 1991sia 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.

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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.978-3-642-84102-6978-3-642-84100-2

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The Use of Tertiary Creep Rates in Ice at High Strains in Compression and Shear the strain required will be large, but ultimately, a steady state constant creep rate condition with anisotropy compatible with stress configuration will eventuate..Tertiary steady state creep rates are higher than the secondary isotropic creep rates which have commonly been used in the study of ic

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The Study of Fracture Toughness of Bohai Sea Ice fracture criterion would be suitable, the study of fracture problems of I-II mixed mode is necessary. The results obtained previously indicated that they coincide with the criterion established from the strain energy density factor theorem. The author had considered that during the interaction of i

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Microfracture and The Compressive Failure of Polycrystalline Iceith the ultimate collapse of the specimen proved fruitless. Additional topics include the influence of grain boundary ledges on the internal stress field in polycrystalline ice, grain and crack size measurements and some important aspects of experimental technique.

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Processes of Deformation and Fracture of Ice in Compressionent is obtained. Phenomena which lie outside the framework of the viscoelastic elements are discussed. These relate primarily to frictional movements across newly developed crack faces. Stick-slip movement is a possible mechanism in this regard. Sintering, which can be seen as the reverse of the dam

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