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1 School of Dentistry and College of Engineering, University of Michigan, Ann Arbor, Michigan 48104, USA
Frictional anisotropy of the basal plane of natural fluorapatite single crystals was observed; the coefficient of friction (
) in the [2110] direction (
= 0.217) was approximately 12% higher than that in the [0110] direction (
= 0.193). The load at which the ductile-to-brittle transition occurred (
) was significantly higher in the [2110] direction
= 77 gm) than in the [0110] direction
= 15 gm). A mechanism is proposed involving the maximum normal stress and probable cleavage planes.
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