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Relief of mineralization pre-strains on collagen causes strains equivalent to toe-in strains observed in tensile testing of demineralized cortical bone

机译:胶原蛋白的矿化前的缓解导致在脱矿质皮质骨的拉伸试验中观察到的托管菌株的菌株

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Understanding of the mechanical behavior of bone constituents is important for modeling of the composite behavior of bone in normal and pathological cases. A common approach to study the mechanical behavior of bone collagen, a key constituent of bone, is to conduct mechanical tests on demineralized bone specimens. Demineralized cortical bone typically exhibits a non-linear toe-in region on the stressstrain curve upon tension like other non-mineralized collagenous tissues such as tendons [1, 2, 3] (Figure 1). Toe-in strains in the order of 2-4% can be observed during these tests. Bone collagen is a biological polymer and initial non-linear behavior, or increase in stiffness, is typical of disordered polymeric fibers [4, 5]. We propose that the initial non-linear tensile behavior of demineralized bone is due to the transition of bone collagen from a more disordered to a less disordered form. Our data suggest that the ordered form of the matrix is normally maintained by the presence of mineral. Therefore, bone collagen would behave differently in its composite state with mineral than is observed during tensile testing of demineralized bone. In this study, we measured the dimensional changes (length and shape) in human and bovine cortical bone upon demineralization. The strains caused by demineralization are comparable to toe-in strains during tensile testing of demineralized bone.
机译:理解骨成分的力学行为对于在正常和病理病例中骨骼复合行为的建模是重要的。研究骨胶原骨胶原的力学行为的常见方法是对脱矿质骨标本进行机械测试。脱矿化皮质骨通常在应力串曲线上表现出非线性趾部区域,其张力曲线类似于其他非矿化的胶原组织如肌腱[1,2,3](图1)。在这些测试期间,可以观察到2-4%的脚趾菌株。骨胶原是一种生物聚合物和初始非线性行为,或刚度的增加,是无序的聚合物纤维的典型[4,5]。我们提出脱矿质骨的初始非线性拉伸行为是由于骨胶原蛋白从更紊乱的骨胶原转变为较差的无序形式。我们的数据表明,矩阵的有序形式通常由矿物质的存在维持。因此,骨胶原蛋白将在其复合状态下表现不同,其在矿物化骨的拉伸试验期间观察到的矿物。在该研究中,我们在脱矿质化时测量了人和牛皮质骨中的尺寸变化(长度和形状)。脱矿质引起的菌株与脱矿质骨的拉伸试验期间的脚趾菌株相当。

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