Abstract
The purpose of this study is to propose a new constitutive law for pack ice, which is not only capable of simulating the in-plane shear and out-of-plane uniaxial compression, but also capable of avoiding overestimating divergence during shear. The pack ice is treated as a two-dimensional granular plastic, obeying Coulomb's friction law with a maximum principal stress limit. During the out-of-plane uniaxial compression process the flow rule is normal, while during the in-plane shear process the flow rule is coaxial with a linearly varying dilatancy angle describing the divergence. The strength parameterizations are based on thickness and compactness of the pack ice; weakening or hardening can be achieved through advection and redistribution.
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CITATION STYLE
Wang, K. (2006). Pack ice as a two-dimensional granular plastic: A new constitutive law. In Annals of Glaciology (Vol. 44, pp. 317–320). https://doi.org/10.3189/172756406781811358
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