globalchange  > 影响、适应和脆弱性
DOI: 10.5194/tc-10-3063-2016
Scopus记录号: 2-s2.0-85006759544
论文题名:
Critical investigation of calculation methods for the elastic velocities in anisotropic ice polycrystals
作者: Maurel A; , Mercier J; -F; , Montagnat M
刊名: Cryosphere
ISSN: 19940416
出版年: 2016
卷: 10, 期:6
起始页码: 3063
结束页码: 3070
语种: 英语
英文关键词: anisotropy ; borehole logging ; elastic wave ; elasticity ; glaciology ; homogeneous medium ; ice crystal ; moment tensor ; S-wave ; texture ; wave propagation ; wave velocity
英文摘要: Crystallographic texture (or fabric) evolution with depth along ice cores can be evaluated using borehole sonic logging measurements. These measurements provide the velocities of elastic waves that depend on the ice polycrystal anisotropy, and they can further be related to the ice texture. To do so, elastic velocities need to be inverted from a modeling approach that relate elastic velocities to ice texture. So far, two different approaches can be found. A classical model is based on the effective medium theory; the velocities are derived from elastic wave propagation in a homogeneous medium characterized by an average elasticity tensor. Alternatively, a velocity averaging approach was used in the glaciology community that averages the velocities from a given population of single crystals with different orientations. In this paper, we show that the velocity averaging method is erroneous in the present context. This is demonstrated for the case of waves propagating along the clustering direction of a highly textured polycrystal, characterized by crystallographic c axes oriented along a single maximum (cluster). In this case, two different shear wave velocities are obtained while a unique velocity is theoretically expected. While making use of this velocity averaging method, reference work by Bennett (1968) does not end with such an unphysical result. We show that this is due to the use of erroneous expressions for the shear wave velocities in a single crystal, as the starting point of the averaging process. Because of the weak elastic anisotropy of ice single crystal, the inversion of the measured velocities requires accurate modeling approaches. We demonstrate here that the inversion method based on the effective medium theory provides physically based results and should therefore be favored. � Author(s) 2016.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/75023
Appears in Collections:影响、适应和脆弱性
气候变化与战略

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作者单位: Institut Langevin, CNRS, ESPCI ParisTech, 1 rue Jussieu, Paris, France; Poems, CNRS, ENSTA ParisTech, INRIA, 828 boulevard des Mar�chaux, Palaiseau, France; LGGE, CNRS, Universit� Grenoble Alpes, Grenoble, France

Recommended Citation:
Maurel A,, Mercier J,-F,et al. Critical investigation of calculation methods for the elastic velocities in anisotropic ice polycrystals[J]. Cryosphere,2016-01-01,10(6)
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