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 inApplied mathematics and mechanics Vol. 34; no. 4; pp. 405 - 416
Main Author 武晓刚 陈维毅 王旦霞
Format Journal Article
LanguageEnglish
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
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ISSN0253-4827
1573-2754
DOI10.1007/s10483-013-1680-x

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Abstract 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.
AbstractList An extended and reasonable stress boundary condition at an osteon exterior wall is presented to solve the model proposed by Rémond 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.
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.
An extended and reasonable stress boundary condition at an osteon exterior wall is presented to solve the model proposed by RACOmond 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.
Author 武晓刚 陈维毅 王旦霞
AuthorAffiliation College of Mechanics, Taiyuan University of Technology, Taiyuan 030024, P. R. China College of Mathematics, Taiyuan University of Technology, Taiyuan 030024, P. R. China
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CitedBy_id crossref_primary_10_1007_s11433_014_5577_z
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Cites_doi 10.1063/1.1721956
10.1016/j.medengphy.2010.02.001
10.1016/j.jbiomech.2005.08.005
10.1163/157361109789017005
10.1016/S0021-9290(99)00210-9
10.1007/s10237-011-0287-1
10.1016/S0020-7683(98)00105-X
10.1016/j.mechrescom.2004.10.003
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10.1016/j.crme.2009.06.033
10.1016/S0020-7683(98)00101-2
10.1007/BF02368235
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Issue 4
Keywords osteon
bone fluid flow
92C10
transverse isotropy
R318.01
poroelasticity
pressure
74L15
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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.
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  year: 2009
  ident: 1680_CR14
  publication-title: Multidiscipline Modeling in Materials and Structures
  doi: 10.1163/157361109789017005
SSID ssj0004744
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Snippet 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...
An extended and reasonable stress boundary condition at an osteon exterior wall is presented to solve the model proposed by Rémond and Naili. The obtained...
An extended and reasonable stress boundary condition at an osteon exterior wall is presented to solve the model proposed by RACOmond and Naili. The obtained...
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SubjectTerms Amplitudes
Applications of Mathematics
Biocompatibility
Biomedical materials
Classical Mechanics
Computational fluid dynamics
Fluid flow
Fluid- and Aerodynamics
Fluids
Mathematical Modeling and Industrial Mathematics
Mathematical models
Mathematics
Mathematics and Statistics
Partial Differential Equations
Walls
单位
孔隙
应力边界条件
弹性行为
数学模型
检查
流体压力
流体速度
Title Mathematical osteon model for examining poroelastic behaviors
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Volume 34
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