首页> 外文期刊>The Journal of foot and ankle surgery: official publication of the American College of Foot and Ankle Surgeons >Mineral Density and Penetration Strength of the Subchondral Bone Plate of the Talar Dome: High Correlation and Specific Distribution Patterns
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Mineral Density and Penetration Strength of the Subchondral Bone Plate of the Talar Dome: High Correlation and Specific Distribution Patterns

机译:塔拉圆顶软骨下骨板的矿物质密度和穿透强度:高相关性和特定的分布模式。

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The subchondral bone plate plays an important role in stabilizing the osteochondral joint unit and in the pathomechanism of osteochondral lesions and osteoarthritis. The objective of the present study was to measure the mineral density distribution and subchondral bone plate penetration strength of the talar dome joint facet to display and compare the specific distribution patterns. Ten cadaver specimens were used for computed tomography (CT) scans, from which densitograms were derived using CT-osteoabsorptiometry, and for mechanical indentation testing from which the penetration strength was obtained. Our results showed 2 different distribution patterns for mineral density and penetration strength. Of the 10 specimens, 6 (60%) showed bicentric maxima (anteromedially and anterolaterally), and 4 (40%) showed a monocentric maximum (either anteromedially or anterolaterally). A highly significant correlation (p < .0001) for both methods confirmed that the mineral density relied on local load characteristics. In conclusion, the biomechanical properties of the subchondral bone plate of the talar dome joint facet showed specific distribution patterns. CT-osteoabsorptiometry is a reliable method to display the mineral density distribution noninvasively. We recommend CT-osteoabsorptiometry for noninvasive analysis of the biomechanical properties of the subchondral bone plate in osteochondral joint reconstruction and the prevention and treatment of osteoarthritis and osteochondral lesions. (C) 2015 by the American College of Foot and Ankle Surgeons. All rights reserved.
机译:软骨下骨板在稳定骨软骨关节单元以及骨软骨病变和骨关节炎的发病机理中起重要作用。本研究的目的是测量距骨穹顶关节面的矿物质密度分布和软骨下骨板穿透强度,以显示和比较具体的分布模式。将十个尸体标本用于计算机断层扫描(CT)扫描,使用CT骨吸收法从中得出密度图,并用于机械压痕测试,从而获得穿透强度。我们的结果显示了两种不同的矿物质密度和渗透强度分布模式。在10个标本中,有6个(60%)显示出双中心最大值(前额和前外侧),而4个(40%)显示出了单中心最大值(前额或前外侧)。两种方法的高度相关性(p <.0001)证实了矿物质密度取决于局部载荷特征。总之,距骨穹顶关节面软骨下骨板的生物力学特性表现出特定的分布模式。 CT骨吸收法是一种可靠的无创显示矿物质密度分布的方法。我们推荐使用CT骨吸收法对软骨下骨板的生物力学特性进行非侵入性分析,以进行骨软骨关节重建以及骨关节炎和骨软骨病变的预防和治疗。 (C)2015年,美国脚踝外科学院。版权所有。

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