2007
DOI: 10.1007/s10439-007-9351-5
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A Finite Element Dual Porosity Approach to Model Deformation-Induced Fluid Flow in Cortical Bone

Abstract: Fluid flow through the osteocyte canaliculi network is widely believed to be a main factor that controls bone adaptation. The difficulty of in vivo measurement of this flow within cortical bone makes computational models an appealing alternative to estimate it. We present in this paper a finite element dual porosity macroscopic model that can contribute to evaluate the interstitial fluid flow induced by mechanical loads in large pieces of bone. This computational model allows us to predict the macroscopic flui… Show more

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Cited by 41 publications
(25 citation statements)
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References 27 publications
(49 reference statements)
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“…Two recent papers have computationally addressed the question of the two interacting porosities. Fornells et al (2007) considered a mixture theory-based dual porosity model of the PV and the PLC; the model was based on the continuum model of Khalili-Naghadesh & Valliappan (1996). In this model the two porosities are considered to be interacting on the same level as opposed to the model in this paper where the two porosities are arranged hierarchically.…”
Section: Discussionmentioning
confidence: 99%
“…Two recent papers have computationally addressed the question of the two interacting porosities. Fornells et al (2007) considered a mixture theory-based dual porosity model of the PV and the PLC; the model was based on the continuum model of Khalili-Naghadesh & Valliappan (1996). In this model the two porosities are considered to be interacting on the same level as opposed to the model in this paper where the two porosities are arranged hierarchically.…”
Section: Discussionmentioning
confidence: 99%
“…This effect can be attributed mainly to the presence of water in the pores, which is very incompressible, and to its relative difficulty to flow out of the pores upon compression; the gelled state of the SAP results in a somewhat more hindered flow, which translates into somewhat higher linear moduli. This phenomenon is known as poroelasticity, and it is typical of fluid-filled porous media under compression [33,34]. In our experiments the mechanical effect of the filling gel is manifest already at low strains, and persists in the linear deformation region.…”
Section: Discussionmentioning
confidence: 53%
“…In terms of movement and velocity, the interstitial fluid behaves differently under a cyclic mechanical loading in the PLC from its behavior in the Haversian canal. The difference of the bone fluid behavior stems from the differences in geometry and the intrinsic characteristic of each domain (Fornells et al 2007). On one hand, the Haversian canal is the large-scale porosity with roughly ten orders of magnitude greater permeability (Gardinier et al 2010) that houses blood vessels and in which pressure pulses will decay rapidly.…”
Section: The Anatomy and Physiology Of An Osteonmentioning
confidence: 99%