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Influence of interstitial bone microcracks on strain-induced fluid flow
Vu-Hieu Nguyen1, Thibault Lemaire, Salah Naili
1Université Paris-Est, Laboratoire Modélisation et Simulation Multi Echelle, MSME UMR 8208 CNRS, 61 avenue du Général de Gaulle, 94010 Créteil cedex, France. vu-hieu.nguyen@univ-paris-est.fr
Microcracks in bone tissue disrupt fluid flow within osteons, potentially altering the environment for bone cells. This study quantifies how these cracks reduce interstitial fluid velocity, impacting bone remodeling signals.
Area of Science:
- Biomedical Engineering
- Mechanobiology
- Skeletal Biology
Background:
- Microcracks stimulate bone remodeling by osteoclasts and osteoblasts.
- Microcracks are known to affect fluid flow and transport in bone tissue.
Purpose of the Study:
- To quantitatively evaluate strain-induced interstitial fluid velocities in osteons near microcracks.
- To investigate the hydro-mechanical behavior of cracked osteonal bone tissue.
Main Methods:
- Utilized Biot theory for low-frequency poroelastic modeling.
- Employed finite element analysis to simulate fluid flow and stress in cracked bone.
Main Results:
- A microcrack in interstitial bone tissue significantly reduces fluid velocity within adjacent osteons.
- A fluid-inactive zone, covering up to 10% of osteon surface, can form due to microcracks.
- The fluid environment crucial for mechanosensitive bone cells is locally altered.
Conclusions:
- Microcracks create localized fluid-inactive zones within osteons.
- These altered fluid dynamics may impact mechanotransduction and bone remodeling processes.
- The findings highlight the mechanical influence of microcracks on the osteonal microenvironment.
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