Multi-surface failure criterion for saline ice in the brittle regime

In this paper, the development of a 3-D failure criterion for saline ice is presented. The need for such general 3-D failure formulation stems from the fact that, during ice-ship interactions, ice undergoes a complex state of deformation and stress before it fails and breaks away, and the use of the...

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Published in:Cold Regions Science and Technology
Main Author: Derradji-Aouat, A.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2003
Subjects:
Online Access:https://doi.org/10.1016/S0165-232X(02)00093-9
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:8895600 2023-05-15T14:58:15+02:00 Multi-surface failure criterion for saline ice in the brittle regime Derradji-Aouat, A. 2003 text https://doi.org/10.1016/S0165-232X(02)00093-9 https://nrc-publications.canada.ca/eng/view/object/?id=a1a0ce0e-1af3-44db-b511-4dbcf7a840bd https://nrc-publications.canada.ca/fra/voir/objet/?id=a1a0ce0e-1af3-44db-b511-4dbcf7a840bd unknown Cold Regions Science and Technology, Volume: 36, Issue: 1-3, Publication date: 2003, Pages: 47–70 doi:10.1016/S0165-232X(02)00093-9 report_number:IR-2003-05 failure criterion failure envelope multi-surface failure strength yield true triaxial sea ice freshwater ice iceberg ice article 2003 ftnrccanada https://doi.org/10.1016/S0165-232X(02)00093-9 2021-09-01T06:21:17Z In this paper, the development of a 3-D failure criterion for saline ice is presented. The need for such general 3-D failure formulation stems from the fact that, during ice-ship interactions, ice undergoes a complex state of deformation and stress before it fails and breaks away, and the use of the uniaxial strength of ice to compute impact ice loads may lead to inaccurate load calculations and non-conclusive results. In recent years, with the availability of High Power Computers (HPC), numerical methods are being used more than ever before in marine and ice engineering problems. Numerical models based on computational techniques such as finite elements, boundary elements and discrete elements require 3-D constitutive models and failure criteria to represent the behavior of the materials involved (such as the behavior of the ship structure, ice, and water "fluid"). At high-speed mpacts (strain rates >10-3 s-1), ice behaves as a linear elastic material with a brittle mode of failure. Previously, Derradfi-Aouat [Derradji-Aouat, A., 2000. A unified failure envelope for isotropic freshwater ice and iceberg ice.ASME/OMAE-2000, Int. Conference on Offshore Mechanics and Arctic Engineering, Polar and Arctic section New Orleans, US, PDF file # OMAW-2000-P?A # 1002] developed a unified 3-D failure envelope for both fresh water isotropic ice and iceberg ice. In this paper, that formulation is extended to include failure of saline ice (in addition to fresth water ice and iceberg ice.) The results of a significant number of true triaxial tests using Laboratory Grown Ice (LGSI) were obtained from the open literature. The results of these tests formed a database that enables the existing failure model [Derradji-Aouat, A., 2000. A unified failure envelope for isotropic freshwater ice and iceberg ice. ASME/OMAE-2000, Int. Conference on Offshore Mechancis and Arctic Engineering, Polar and Arctic section, New Orleans, US, PDF file # OMAE-2000-P/A # 1002] to be extended from the isotropic fresh water ice and iceberg ice to columnar saline ice. Mroz's [J. Mech. Phys. Solids 15 (1967) 163] concept for the multi-surface failure theory is used in both studies (the present study, for saline ice, as well as in the previous study, for the fresh water isotropic ice and iceberg ice). It appears that the same set of the equations is applicable to the failure of all three types of ice. The possibility of the existence of a universal and general failure criterion for all types of ice is discussed. The validation of the present multi-surface failure criterion was discussed on the basis of comparisions between predicted failure curves and actual true triaxial test results. An overall discrepancy of predicted versus measured strength values of less than 20% was calculated. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Arctic Iceberg* Sea ice National Research Council Canada: NRC Publications Archive Arctic Orleans ENVELOPE(-60.667,-60.667,-63.950,-63.950) Cold Regions Science and Technology 36 1-3 47 70
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language unknown
topic failure criterion
failure envelope
multi-surface failure
strength
yield
true triaxial
sea ice
freshwater ice
iceberg ice
spellingShingle failure criterion
failure envelope
multi-surface failure
strength
yield
true triaxial
sea ice
freshwater ice
iceberg ice
Derradji-Aouat, A.
Multi-surface failure criterion for saline ice in the brittle regime
topic_facet failure criterion
failure envelope
multi-surface failure
strength
yield
true triaxial
sea ice
freshwater ice
iceberg ice
description In this paper, the development of a 3-D failure criterion for saline ice is presented. The need for such general 3-D failure formulation stems from the fact that, during ice-ship interactions, ice undergoes a complex state of deformation and stress before it fails and breaks away, and the use of the uniaxial strength of ice to compute impact ice loads may lead to inaccurate load calculations and non-conclusive results. In recent years, with the availability of High Power Computers (HPC), numerical methods are being used more than ever before in marine and ice engineering problems. Numerical models based on computational techniques such as finite elements, boundary elements and discrete elements require 3-D constitutive models and failure criteria to represent the behavior of the materials involved (such as the behavior of the ship structure, ice, and water "fluid"). At high-speed mpacts (strain rates >10-3 s-1), ice behaves as a linear elastic material with a brittle mode of failure. Previously, Derradfi-Aouat [Derradji-Aouat, A., 2000. A unified failure envelope for isotropic freshwater ice and iceberg ice.ASME/OMAE-2000, Int. Conference on Offshore Mechanics and Arctic Engineering, Polar and Arctic section New Orleans, US, PDF file # OMAW-2000-P?A # 1002] developed a unified 3-D failure envelope for both fresh water isotropic ice and iceberg ice. In this paper, that formulation is extended to include failure of saline ice (in addition to fresth water ice and iceberg ice.) The results of a significant number of true triaxial tests using Laboratory Grown Ice (LGSI) were obtained from the open literature. The results of these tests formed a database that enables the existing failure model [Derradji-Aouat, A., 2000. A unified failure envelope for isotropic freshwater ice and iceberg ice. ASME/OMAE-2000, Int. Conference on Offshore Mechancis and Arctic Engineering, Polar and Arctic section, New Orleans, US, PDF file # OMAE-2000-P/A # 1002] to be extended from the isotropic fresh water ice and iceberg ice to columnar saline ice. Mroz's [J. Mech. Phys. Solids 15 (1967) 163] concept for the multi-surface failure theory is used in both studies (the present study, for saline ice, as well as in the previous study, for the fresh water isotropic ice and iceberg ice). It appears that the same set of the equations is applicable to the failure of all three types of ice. The possibility of the existence of a universal and general failure criterion for all types of ice is discussed. The validation of the present multi-surface failure criterion was discussed on the basis of comparisions between predicted failure curves and actual true triaxial test results. An overall discrepancy of predicted versus measured strength values of less than 20% was calculated. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Derradji-Aouat, A.
author_facet Derradji-Aouat, A.
author_sort Derradji-Aouat, A.
title Multi-surface failure criterion for saline ice in the brittle regime
title_short Multi-surface failure criterion for saline ice in the brittle regime
title_full Multi-surface failure criterion for saline ice in the brittle regime
title_fullStr Multi-surface failure criterion for saline ice in the brittle regime
title_full_unstemmed Multi-surface failure criterion for saline ice in the brittle regime
title_sort multi-surface failure criterion for saline ice in the brittle regime
publishDate 2003
url https://doi.org/10.1016/S0165-232X(02)00093-9
https://nrc-publications.canada.ca/eng/view/object/?id=a1a0ce0e-1af3-44db-b511-4dbcf7a840bd
https://nrc-publications.canada.ca/fra/voir/objet/?id=a1a0ce0e-1af3-44db-b511-4dbcf7a840bd
long_lat ENVELOPE(-60.667,-60.667,-63.950,-63.950)
geographic Arctic
Orleans
geographic_facet Arctic
Orleans
genre Arctic
Iceberg*
Sea ice
genre_facet Arctic
Iceberg*
Sea ice
op_relation Cold Regions Science and Technology, Volume: 36, Issue: 1-3, Publication date: 2003, Pages: 47–70
doi:10.1016/S0165-232X(02)00093-9
report_number:IR-2003-05
op_doi https://doi.org/10.1016/S0165-232X(02)00093-9
container_title Cold Regions Science and Technology
container_volume 36
container_issue 1-3
container_start_page 47
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