providing physicians with a valuable and non-
invasive assessment tool for bone quality and
strength.
An independent verification of our results is of
course required and foreseen. in this context micro
finite element simulations will be setup, to correlate
our image analysis to compressive strength of the
specimens. a verification of these models will be
based on uniaxial compressive experiments of the
harvested samples, conducted only in the primary
direction (1), due to the destructive nature of the
tests.
Brown et al. (1980) and Martens et al. (1983)
performed compression tests by loading in three
directions: anterior-posterior, superior-inferior and
medial-lateral. They shown that anisotropy was
evident and increase in stiffness was found in the
regions traversed by the primary trabecular system
(Brown et al., 1980); (Martens et al., 1983).
However, in their studies bone specimens were
obtained from nonspecific regions of the entire
femoral heads. in our study we examined eight
different but well defined orientations with similar
positioning within the femoral structure. Sugita et al.
(1999) examined the differences in anisotropy in
osteoporotic bone in the primary compressive group
of the femoral head. They found increased values of
compressive stiffness in the parallel loading group
compared with the perpendicular loading group, but
the anisotropic behaviour of cancellous bone is
reduced, and the femoral head became isotropic as
the bone density decreased (e.g. in osteoporosis).
The anisotropy of vertebral bodies was also
examined in the literature. Mosekilde and Viidik
(1985), found that bone strength was greater in the
vertical than in the transverse direction.
Conclusively, we examined geometrical
anisotropy of trabecular bone and found this to
represent an important characteristic of this severely
inhomogeneous structure. the conversion of our
results with previous experimental findings,
strengthens our hypothesis that micro scale imaging
of the femoral head, at limited spatial resolution,
may be used as an indicator of both, bone strength
and anisotropy.
ACKNOWLEDGEMENTS
The authors would like to thank Dr. A. Tsouknidas
of the Aristotle University of Thessaloniki for his
contribution during the setup and preparation of this
manuscript, as well as Dr. K. Anagnostidis for
providing the bone samples.
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