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THE UNIVERSITY OF CALGARY Eric Snively A ... - Ohio University

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of strain energy evident in Figure 4.6 shows that the proximally constricted<br />

portion of MT III was potentially vulnerable to damage.<br />

DISCUSSION<br />

FEA direcfly supports the energy transference hypothesis<br />

The results corroborate the hypothesis that energy was transferred from MT<br />

III to adjacent elements when the metatarsus was normal to the substrate (Holtz<br />

1994a), and suggest a mechanism for this transfer. Figures 4.5 and 4.6 indicate<br />

that if energy transference did not take place, strain would become concentrated<br />

in the weakest part of the metatarsal, its fragile proximal splint. Strain parallel to<br />

the long axis of the metatarsus also occurred where distal ligament correlates are<br />

found on MT III (Figure 4.4). The concentration of bone strain energy at these<br />

locations implies that MT III wedged up between MT II and MT IV, The<br />

correspondence with ligament scars indicates that ligaments probably absorbed<br />

strain energy as MT III was displaced vertically. Strain results from the first<br />

analysis, therefore, suggest that ligaments facilitated the transfer of footfall<br />

energies along the long axis of the metatarsus.<br />

FEA results complement the tensional keystone hypothesis<br />

Results from the second analysis indicate that when the metatarsus was<br />

inclined to the substrate, ligaments would prevent damage to the splint of MT III<br />

from bending stresses. If distal ligaments were not present to damp the

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