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骨单位皮质骨骨折的微观力学

Micromechanics of osteonal cortical bone fracture.

作者信息

Guo X E, Liang L C, Goldstein S A

机构信息

Bone Bioengineering Laboratory, Columbia University, New York, NY 10027, USA.

出版信息

J Biomech Eng. 1998 Feb;120(1):112-7. doi: 10.1115/1.2834290.

Abstract

Microcracks have been associated with age-related bone tissue fragility and fractures. The objective of this study was to develop a simple osteonal cortical bone model and apply linear elastic fracture mechanics theory to understand the micromechanics of the fracture process in osteonal cortical bone and its dependence on material properties. The linear fracture mechanics of our composite model of cortical bone, consisting of an osteon and interstitial bone tissue, was characterized in terms of a stress intensity factor (SIF) near the tip of a microcrack. The interaction between a microcrack and an osteon was studied for different types of osteons and various spacing between the crack and the osteon. The results of the analysis indicate that the fracture mechanics of osteonal cortical bone is dominated by the modulus ratio between the osteon and interstitial bone tissue: A soft osteon promotes microcrack propagation toward the osteon (and cement line) while a stiff one repels the microcrack from the osteon (and cement line). These findings suggest that newly formed, low-stiffness osteons may toughen cortical bone tissue by promoting crack propagation toward osteons. A relatively accurate empirical formula also was obtained to provide an easy estimation of the influence of osteons on the stress intensity factor.

摘要

微裂纹与年龄相关的骨组织脆性和骨折有关。本研究的目的是建立一个简单的骨单位皮质骨模型,并应用线弹性断裂力学理论来理解骨单位皮质骨骨折过程的微观力学及其对材料特性的依赖性。我们的皮质骨复合模型由一个骨单位和间质骨组织组成,其线性断裂力学通过微裂纹尖端附近的应力强度因子(SIF)来表征。针对不同类型的骨单位以及裂纹与骨单位之间的各种间距,研究了微裂纹与骨单位之间的相互作用。分析结果表明,骨单位皮质骨的断裂力学主要由骨单位与间质骨组织之间的模量比决定:软质骨单位会促进微裂纹向骨单位(以及黏合线)扩展,而硬质骨单位则会使微裂纹从骨单位(以及黏合线)处排斥开。这些发现表明,新形成的、低刚度的骨单位可能通过促进裂纹向骨单位扩展来增强皮质骨组织。还获得了一个相对准确的经验公式,以便轻松估算骨单位对应力强度因子的影响。

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