Journal of Biomechanics
Volume 40, Issue 1 , Pages 36-45, 2007

Tensile behavior of cortical bone: Dependence of organic matrix material properties on bone mineral content

  • S.P. Kotha

      Affiliations

    • Biomedical Engineering Department, Rutgers University, 617 Bowser Road, Piscataway, NJ 08854, USA
    • Present Address: Department of Oral Biology, University of Missouri – Kansas City, Rm 432 650 E. 25th St., Kansas City, MO 64108.
  • ,
  • N. Guzelsu

      Affiliations

    • Biomedical Engineering Department, Rutgers University, 617 Bowser Road, Piscataway, NJ 08854, USA
    • University of Medicine and Dentistry of New Jersey − SOM – Biomechanics Laboratory, Science Center, 2 Medical Center Drive, Stratford, NJ 08084-1504, USA
    • Corresponding Author InformationCorresponding author. Department of Osteosciences/Biomechanics Program, UDP-Suite 1700, 42 East Laurel Road, Stratford, NJ 08084-1504, USA. Tel.: +18565662731; fax: +18565662733.

Accepted 26 November 2005. published online 23 January 2006.

Abstract 

A porous composite model is developed to analyze the tensile mechanical properties of cortical bone. The effects of microporosity (volksman's canals, osteocyte lacunae) on the mechanical properties of bone tissue are taken into account. A simple shear lag theory, wherein tensile loads are transferred between overlapped mineral platelets by shearing of the organic matrix, is used to model the reinforcement provided by mineral platelets. It is assumed that the organic matrix is elastic in tension and elastic–perfectly plastic in shear until it fails. When organic matrix shear stresses at the ends of mineral platelets reach their yield values, the stress–strain curve of bone tissue starts to deviate from linear behavior. This is referred as the microscopic yield point. At the point where the stress–strain behavior of bone shows a sharp curvature, the organic phase reaches its shear yield stress value over the entire platelet. This is referred as the macroscopic yield point. It is assumed that after macroscopic yield, mineral platelets cannot contribute to the load bearing capacity of bone and that the mechanical behavior of cortical bone tissue is determined by the organic phase only. Bone fails when the principal stress of the organic matrix is reached. By assuming that mechanical properties of the organic matrix are dependent on bone mineral content below the macroscopic yield point, the model is used to predict the entire tensile mechanical behavior of cortical bone for different mineral contents. It is found that decreased shear yield stresses and organic matrix elastic moduli are required to explain the mechanical behavior of bones with lowered mineral contents. Under these conditions, the predicted values (elastic modulus, 0.002 yield stress and strain, and ultimate stress and strain) are within 15% of experimental data.

Keywords: Cortical bone tissue, Tensile behavior, Bone mineral content (BMC), Organic phase, Composite modeling

 

PII: S0021-9290(05)00534-8

doi:10.1016/j.jbiomech.2005.11.016

Journal of Biomechanics
Volume 40, Issue 1 , Pages 36-45, 2007