Mathematical osteon model for examining poroelastic behaviors
An extended and reasonable stress boundary condition at an osteon exte- rior wall is presented to solve the model proposed by Remond and Naili. The obtained pressure and fluid velocity solutions are used to investigate the osteonal poroelastic behaviors. The following results are obtained. (i) Both...
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Published in | Applied mathematics and mechanics Vol. 34; no. 4; pp. 405 - 416 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Heidelberg
Shanghai University
01.04.2013
College of Mechanics, Taiyuan University of Technology,Taiyuan 030024, P.R.China%College of Mathematics, Taiyuan University of Technology,Taiyuan 030024, P.R.China |
Subjects | |
Online Access | Get full text |
ISSN | 0253-4827 1573-2754 |
DOI | 10.1007/s10483-013-1680-x |
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Summary: | An extended and reasonable stress boundary condition at an osteon exte- rior wall is presented to solve the model proposed by Remond and Naili. The obtained pressure and fluid velocity solutions are used to investigate the osteonal poroelastic behaviors. The following results are obtained. (i) Both the fluid pressure and the velocity amplitudes are proportional to the strain amplitude and the loading frequency. (ii) In the physiological loading state, the key role governing the poroelastic behaviors of the osteon is the strain rate. (iii) At the osteon scale, the pressure is strongly affected by the permeability variations, whereas the fluid velocity is not. |
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Bibliography: | 31-1650/O1 osteon, poroelasticity, transverse isotropy, bone fluid flow, pressure Xiao-gang WU , Wei-yi CHEN , Dan-xia WANG (1 2. College of Mechanics, Taiyuan University of Technology, Taiyuan 030024, P. R. China; College of Mathematics, Taiyuan University of Technology Taiyuan 030024, P. R. China) An extended and reasonable stress boundary condition at an osteon exte- rior wall is presented to solve the model proposed by Remond and Naili. The obtained pressure and fluid velocity solutions are used to investigate the osteonal poroelastic behaviors. The following results are obtained. (i) Both the fluid pressure and the velocity amplitudes are proportional to the strain amplitude and the loading frequency. (ii) In the physiological loading state, the key role governing the poroelastic behaviors of the osteon is the strain rate. (iii) At the osteon scale, the pressure is strongly affected by the permeability variations, whereas the fluid velocity is not. ObjectType-Article-2 SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 23 |
ISSN: | 0253-4827 1573-2754 |
DOI: | 10.1007/s10483-013-1680-x |