Non-basal dislocations should be accounted for in simulating ice mass flow

被引:21
作者
Chauve, T. [1 ]
Montagnat, M. [1 ]
Piazolo, S. [2 ,3 ,4 ]
Journaux, B. [1 ]
Wheeler, J. [5 ]
Barou, F. [6 ]
Mainprice, D. [6 ]
Tommasi, A. [6 ]
机构
[1] Univ Grenoble Alpes, CNRS, IRD, G INP,IGE, F-38000 Grenoble, France
[2] Macquarie Univ, ARC Ctr Excellence Core Crust Fluid Syst CCFS, N Ryde, NSW 2109, Australia
[3] Macquarie Univ, GEMOC, Dept Earth & Planetary Sci, N Ryde, NSW 2109, Australia
[4] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England
[5] Univ Liverpool, Dept Earth & Ocean Sci, Sch Environm Sci, Liverpool L69 3GP, Merseyside, England
[6] Univ Montpellier, CNRS, Geosci Montpellier, F-34095 Montpellier, France
关键词
non-basal dislocations in ice; Weighted Burgers Vectors; cryo-EBSD; crystal plasticity; ELECTRON BACKSCATTER DIFFRACTION; MODELING VISCOPLASTIC BEHAVIOR; STRAIN-GRADIENT PLASTICITY; FULL-FIELD PREDICTIONS; DYNAMIC RECRYSTALLIZATION; MISORIENTATION ANALYSIS; POLYCRYSTALLINE ICE; COLUMNAR ICE; SIMPLE SHEAR; POLAR ICE;
D O I
10.1016/j.epsl.2017.06.020
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Prediction of ice mass flow and associated dynamics is pivotal at a time of climate change. Ice flow is dominantly accommodated by the motion of crystal defects - the dislocations. In the specific case of ice, their observation is not always accessible by means of the classical tools such as X-ray diffraction or transmission electron microscopy (TEM). Part of the dislocation population, the geometrically necessary dislocations (GNDs) can nevertheless be constrained using crystal orientation measurements via electron backscattering diffraction (EBSD) associated with appropriate analyses based on the Nye (1950) approach. The present study uses the Weighted Burgers Vectors, a reduced formulation of the Nye theory that enables the characterization of GNDs. Applied to ice, this method documents, for the first time, the presence of dislocations with non-basal [c] or < c + a > Burgers vectors. These [c] or (c + a) dislocations represent up to 35% of the GNDs observed in laboratory-deformed ice samples. Our findings offer a more complex and comprehensive picture of the key plasticity processes responsible for polycrystalline ice creep and provide better constraints on the constitutive mechanical laws implemented in ice sheet flow models used to predict the response of Earth ice masses to climate change. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:247 / 255
页数:9
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