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肱尺关节不匹配的力学影响——有限元分析与实验

Mechanical implications of humero-ulnar incongruity--finite element analysis and experiment.

作者信息

Merz B, Eckstein F, Hillebrand S, Putz R

机构信息

Institut Straumann, Waldenburg, Switzerland.

出版信息

J Biomech. 1997 Jul;30(7):713-21. doi: 10.1016/s0021-9290(97)00014-6.

Abstract

Previous studies show that the humero-ulnar joint is physiologically incongruous [Eckstein et al. (1995a) Anat. Rec. 243, 318-326] and exhibits a bicentric (ventro-dorsal) distribution of subchondral mineralization [Eckstein et al. (1995b) J. Orthop. Res. 13, 286-278]. We therefore asked: (1) Does humero-ulnar incongruity bring about a bicentric distribution of contact pressure? (2) Do tensile stresses occur in the subchondral bone of the trochlear notch that are in the same order of magnitude as the compressive stresses? (3) Do ventral and dorsal maxima of subchondral bone density correlate with a bicentric distribution of strain energy density? To that end, a two-dimensional finite element model was designed. The shape and material properties of the bones were based on CT and the boundary conditions selected to agree with resisted elbow extension at 90 degrees of flexion. The incongruity and contact areas were determined experimentally from casts, and the pressure distribution with Fuji Prescale film. In the model and the experiment contact stresses above 2 MPa were recorded in the ventral and dorsal parts of the joint, and values below 0.5 MPa in the depth of the notch. In the model, tensile stresses of 2.9 MPa were observed in the subchondral bone of the ulna, but not in the humerus. The subchondral strain energy density yielded a bicentric pattern in a model with homogeneous subchondral bone properties. It is shown that humero-ulnar incongruity brings about a bicentric distribution of contact pressure, a tensile stress in the notch that is in the same order of magnitude as the compressive stress, and a distribution of strain energy density that correlates with subchondral density patterns.

摘要

先前的研究表明,肱尺关节在生理上是不协调的[埃克斯坦等人(1995年a)《解剖学记录》243卷,318 - 326页],并且表现出软骨下矿化的双中心(腹侧 - 背侧)分布[埃克斯坦等人(1995年b)《矫形外科学研究杂志》13卷,286 - 278页]。因此,我们提出以下问题:(1)肱尺关节不协调是否会导致接触压力的双中心分布?(2)滑车切迹的软骨下骨中出现的拉应力是否与压应力处于相同数量级?(3)软骨下骨密度的腹侧和背侧最大值是否与应变能密度的双中心分布相关?为此,设计了一个二维有限元模型。骨骼的形状和材料特性基于CT数据,边界条件的选择与在90度屈曲时抵抗肘关节伸展的情况一致。不协调情况和接触面积通过铸型实验确定,压力分布则使用富士预敏胶片进行测量。在模型和实验中,关节腹侧和背侧记录到接触应力高于2MPa,切迹深处的值低于0.5MPa。在模型中,在尺骨的软骨下骨中观察到2.9MPa的拉应力,但在肱骨中未观察到。在具有均匀软骨下骨特性的模型中,软骨下应变能密度呈现出双中心模式。结果表明,肱尺关节不协调会导致接触压力的双中心分布、切迹中的拉应力与压应力处于相同数量级,以及应变能密度分布与软骨下密度模式相关。

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