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The cartilage-bone interface.

机译:软骨-骨骼界面。

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In the knee joint, the purpose of the cartilage-bone interface is to maintain structural integrity of the osteochondral unit during walking, kneeling, pivoting, and jumping--during which tensile, compressive, and shear forces are transmitted from the viscoelastic articular cartilage layer to the much stiffer mineralized end of the long bone. Mature articular cartilage is integrated with subchondral bone through a approximately 20 to approximately 250 microm thick layer of calcified cartilage. Inside the calcified cartilage layer, perpendicular chondrocyte-derived collagen type II fibers become structurally cemented to collagen type I osteoid deposited by osteoblasts. The mature mineralization front is delineated by a thin approximately 5 microm undulating tidemark structure that forms at the base of articular cartilage. Growth plate cartilage is anchored to epiphyseal bone, sometimes via a thin layer of calcified cartilage and tidemark, while the hypertrophic edge does not form a tidemark and undergoes continual vascular invasion and endochondral ossification (EO) until skeletal maturity upon which the growth plates are fully resorbed and replaced by bone. In this review, the formation of the cartilage-bone interface during skeletal development and cartilage repair, and its structure and composition are presented. Animal models and human anatomical studies show that the tidemark is a dynamic structure that forms within a purely collagen type II-positive and collagen type I-negative hyaline cartilage matrix. Cartilage repair strategies that elicit fibrocartilage, a mixture of collagen type I and type II, are predicted to show little tidemark/calcified cartilage regeneration and to develop a less stable repair tissue-bone interface. The tidemark can be regenerated through a bone marrow-driven growth process of EO near the articular surface.
机译:在膝关节中,软骨-骨骼界面的目的是在行走,跪着,枢转和跳跃过程中保持骨软骨单元的结构完整性-在此期间,拉伸,压缩和剪切力从粘弹性关节软骨层传递到长骨更硬的矿化端。成熟的关节软骨通过约20至约250微米厚的钙化软骨层与软骨下骨整合在一起。在钙化的软骨层内,垂直的软骨细胞衍生的II型胶原纤维在结构上与成骨细胞沉积的I型胶原类骨质形成胶结。成熟的矿化锋线由在关节软骨底部形成的大约5微米的波浪状潮汐结构来描绘。生长板软骨有时会通过钙化软骨和潮膜的薄层固定在骨epi骨上,而肥大性边缘不会形成潮膜,并且会经历持续的血管浸润和软骨内骨化(EO),直到骨骼成熟,生长板才能完全生长被骨头吸收。在这篇综述中,介绍了骨骼发育和软骨修复过程中软骨-骨界面的形成及其结构和组成。动物模型和人体解剖学研究表明,潮汐标记是在纯II型胶原阳性和I型胶原阴性透明软骨基质中形成的动态结构。预计引发纤维软骨(I型和II型胶原的混合物)的软骨修复策略将显示出很少的潮痕/钙化软骨再生并发展出较不稳定的修复组织-骨界面。潮标可以通过关节表面附近的EO的骨髓驱动生长过程来再生。

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