CCPortal
DOI10.1029/2020JB020300
FinIrrSDA: A 3-D Model for Magnetic Shape and Distribution Anisotropy of Finite Irregular Arrangements of Particles With Different Sizes, Geometries, and Orientations
Biedermann A.R.
发表日期2020
ISSN21699313
卷号125期号:12
英文摘要The magnetic anisotropy carried by strongly magnetic particles such as magnetite or ferrofluid-filled pores is generally composed of shape anisotropy and distribution anisotropy. Their relative importance in rocks depends on numerous factors and has been discussed controversially. A major challenge in estimating their contributions so far has been that models for distribution anisotropy only exist for regular arrangements of equal particles along lines or in planes. Because magnetite grains or pores in rocks display wide ranges of orientations, shapes, and sizes in generally irregular arrangements, new models are needed to describe distribution anisotropy for more realistic grain and pore assemblies. The model presented in this study, FinIrrSDA, calculates shape and distribution anisotropy for finite irregular assemblies of unequal particles with different orientations. Input parameters are provided as a table with x, y, and z coordinates of the particle centers and the lengths and orientations of the major, intermediate, and minor axes of best fit ellipsoids. The model output consists of two susceptibility tensors: (1) the shape anisotropy tensor and (2) the total tensor combining shape and distribution anisotropies. FinIrrSDA can be applied to a wide range of input data sets, including known structures of synthetic samples, particle analyses from tomography data, and, subject to certain assumptions, 2-D images. The model will hopefully increase our understanding of the interplay between shape and distribution anisotropies in natural rocks and facilitate future interpretations of both the magnetic anisotropy carried by magnetite grains and magnetic pore fabrics. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词distribution anisotropy; magnetic fabric; magnetic pore fabric; numerical model; shape anisotropy
语种英语
来源期刊Journal of Geophysical Research: Solid Earth
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/187459
作者单位Institute of Geological Sciences, University of Bern, Bern, Switzerland
推荐引用方式
GB/T 7714
Biedermann A.R.. FinIrrSDA: A 3-D Model for Magnetic Shape and Distribution Anisotropy of Finite Irregular Arrangements of Particles With Different Sizes, Geometries, and Orientations[J],2020,125(12).
APA Biedermann A.R..(2020).FinIrrSDA: A 3-D Model for Magnetic Shape and Distribution Anisotropy of Finite Irregular Arrangements of Particles With Different Sizes, Geometries, and Orientations.Journal of Geophysical Research: Solid Earth,125(12).
MLA Biedermann A.R.."FinIrrSDA: A 3-D Model for Magnetic Shape and Distribution Anisotropy of Finite Irregular Arrangements of Particles With Different Sizes, Geometries, and Orientations".Journal of Geophysical Research: Solid Earth 125.12(2020).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Biedermann A.R.]的文章
百度学术
百度学术中相似的文章
[Biedermann A.R.]的文章
必应学术
必应学术中相似的文章
[Biedermann A.R.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。