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Protein-polysaccharide composite design via molecular engineering: tailored fat mimetics for multifunctional food applications. [PDF]
Food Chem XZhang A +8 more
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Breaking the ice: Fracture angles with viscous-plastic sea ice rheologies
, 2021 openaire +1 more source
Journal of Geophysical Research: Oceans, 2022 As the sea‐ice modeling community is shifting to advanced numerical frameworks, developing new sea‐ice rheologies, and increasing model spatial resolution, ubiquitous deformation features in the Arctic sea ice are now being resolved by sea‐ice models ...
Einar Olason +2 more
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A review of ice rheology for ice sheet modelling
Cold Regions Science and Technology, 1989Abstract Ice core and borehole studies along flowlines in ice sheets show that the ice crystal structure and flow properties evolve together with strain and rotation along the particle paths. Laboratory studies of initially isotropic polycrystalline ice show that the changes in crystal structure and flow properties of the ice sheets can be simulated ...
W.F. Budd, T.H. Jacka
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1998
Laboratory measurements of the brittle and ductile behavior of several of the major icy planetary building materials have been made: water ice phases I through VI, ices in the ammonia-water system, mixtures of water ice plus particulates, and methane clathrate.
W. B. Durham, S. H. Kirby, L. A. Stern
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Laboratory measurements of the brittle and ductile behavior of several of the major icy planetary building materials have been made: water ice phases I through VI, ices in the ammonia-water system, mixtures of water ice plus particulates, and methane clathrate.
W. B. Durham, S. H. Kirby, L. A. Stern
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Annual Review of Fluid Mechanics, 2008
The polar oceans of Earth are covered by sea ice. On timescales much greater than a day, the motion and deformation of the sea ice cover (i.e., its dynamics) are primarily determined by atmospheric and oceanic tractions on its upper and lower surfaces and by internal ice forces that arise within the ice cover owing to its deformation.
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The polar oceans of Earth are covered by sea ice. On timescales much greater than a day, the motion and deformation of the sea ice cover (i.e., its dynamics) are primarily determined by atmospheric and oceanic tractions on its upper and lower surfaces and by internal ice forces that arise within the ice cover owing to its deformation.
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Stability of the Viscous-Plastic Sea Ice Rheology
Journal of Physical Oceanography, 1995The large-scale two-dimensional theology of a sea ice pack arises from the local contact forces between ; adjacent floes in convergence. It is conventionally modeled by a viscous-plastic constitutive relation to reflect the low or zero stress in a divergent flow field and the rate-independent ridging process in convergence. The authors demonstrate how,
Gray, Nico; id_orcid 0000-0003-3554-0499 +2 more
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A finite-element treatment of sea ice dynamics for different ice rheologies
International Journal for Numerical and Analytical Methods in Geomechanics, 1998Summary: The effects of four different rheologies on the evolution of a large-scale sea ice pack are determined and compared. Two rheologies are of viscous-plastic form, and two are viscous fluid relations. The initial pack domain is rectangular, and the motion is driven by wind stress and resisted by ocean drag.
Schulkes, R. M.S.M. +2 more
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