Common Features of Deformation Behavior Between Human Tooth Enamel and Rocks

Dmitry Zaytsev, Maxim Mezhenov, Peter Panfilov
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Abstract

The contribution of bioorganic components in the deformation behavior of a rock-like biocomposite human tooth enamel is discussed. Uniaxial compression testing and Brazilian testing (diametral compression) in liquid nitrogen (77 K) and in air at room temperature were carried out on the samples cut from human tooth enamel. It was compared with deformation behavior of some rocks (granite, serpentinite, and jasper) and plasma-sprayed Al2O3 under compression and Brazilian testing in air at room temperature. It was shown that enamel and the rocks exhibit the viscoelastic-like deformation behavior under compression, whereas their macroscopic response becomes brittle under tensile stress. Fracture surface morphology was attested as brittle in all model materials, although cracks in them all advance by the viscoelastic-like manner as a crack in a ductile metal. The contribution of viscoelastic bioorganic component in deformation behavior of enamel is detected at room temperature only because bioorganic component leaves the viscoelasticity at low temperatures. However, this contribution does not lead to changing the character of deformation behavior of the rock-like biocomposite in comparison with these rocks.
人类牙釉质与岩石变形行为的共同特征
讨论了生物有机成分对岩石状生物复合人牙釉质变形行为的影响。在液氮(77 K)和室温空气中对人牙釉质切割样品进行单轴压缩试验和巴西式(直径压缩)试验。比较了一些岩石(花岗岩、蛇纹岩和碧玉)和等离子喷涂Al2O3在室温空气压缩和巴西试验下的变形行为。结果表明,牙釉质和岩石在压缩作用下表现出粘弹性样的变形行为,而在拉应力作用下则表现出脆性的宏观响应。所有模型材料的断口形貌都被证明是脆性的,尽管它们中的裂纹都以粘弹性的方式推进,就像韧性金属中的裂纹一样。粘弹性生物有机组分对牙釉质变形行为的贡献只有在室温下才能被检测到,因为生物有机组分在低温下离开了粘弹性。然而,与这些岩石相比,这种贡献并没有导致类岩石生物复合材料变形行为特征的改变。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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