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老年人股骨颈的过度矿化。

Hypermineralization in the femoral neck of the elderly.

机构信息

Department of Materials Engineering, University of British Columbia, Vancouver, BC, Canada; Department of Biomaterials, Max Planck Institute of Colloids and Interfaces, Potsdam, Germany; Centre for Hip Health and Mobility, Vancouver, BC, Canada.

Department of Biomaterials, Max Planck Institute of Colloids and Interfaces, Potsdam, Germany.

出版信息

Acta Biomater. 2019 Apr 15;89:330-342. doi: 10.1016/j.actbio.2019.03.020. Epub 2019 Mar 12.

Abstract

Hip fragility depends on the decline in bone mass as well as changes in bone microstructure and the properties of bone mineral and organic matrix. Although it is well-established that low bone mass or osteoporosis is a key factor in hip fracture risk, it is striking to observe that 92% of 24 patients who have sustained an intracapsular hip fracture showed hypermineralization at the superior-anterior quadrant, a critical region associated with increased hip fracture risk. In-depth material studies on a total of 12 human cadaver femurs revealed increased degree of mineralization in the hypermineralized tissue: calcium weight percentage as measured by quantitative backscattered electron imaging increased by approximately 15% compared with lamellar bone; mineral-to-matrix ratio obtained by Raman microspectroscopy imaging also increased. Immunohistochemistry revealed localized type II collagen in the hypermineralized region, implying its cartilaginous nature. At the ultrastructural level, X-ray scattering revealed significantly smaller (on average 2.3 nm thick and 15.6 nm long) and less ordered bone minerals in the hypermineralized tissue. Finally, the hypermineralized tissue was more brittle than lamellar bone under hydrated state - cracks propagated easily in the hypermineralized region but stopped at the lamellar boundary. This study demonstrates that hypermineralization of femoral neck cortical bone is a source of bone fragility which is worth considering in future fracture risk assessment when the origin of hip fracture is unclear based on current evaluation standards. STATEMENT OF SIGNIFICANCE: Hypermineralization of femoral cortical bone in older adults might occur in many more hip fracture cases than presently known. Yet, this tissue remains largely unknown to the orthopedic community possibly due to coarse resolution of clinical imaging. The current study showed the hypermineralized tissue had reduced fracture resistance which could be attributed to the material changes in mineral content, organic matrix, and mineral platelets properties. It thus could be a source for fracture initiation. Consequently, we believe hypermineralization of femoral neck cortical bone should be considered in hip fragility assessment, especially when low bone mass cannot be identified as a primary contributor to hip fracture.

摘要

髋部脆弱性不仅取决于骨量的减少,还取决于骨微观结构以及骨矿物质和有机基质的特性变化。虽然众所周知,低骨量或骨质疏松症是髋部骨折风险的关键因素,但令人震惊的是,在 24 名发生囊内髋部骨折的患者中,有 92%的患者在前上象限表现出过度矿化,这是与髋部骨折风险增加相关的关键区域。对总共 12 个人体尸体股骨进行的深入材料研究表明,过度矿化组织中的矿化程度增加:通过定量背散射电子成像测量的钙重量百分比比板层骨增加了约 15%;通过 Raman 微光谱成像获得的矿物质与基质比也增加了。免疫组织化学显示,在过度矿化区域存在局部的 II 型胶原,暗示其软骨性质。在超微结构水平上,X 射线散射显示,过度矿化组织中的骨矿物质明显更小(平均厚度为 2.3nm,长度为 15.6nm)且更无序。最后,在水合状态下,过度矿化组织比板层骨更易碎——裂纹容易在过度矿化区域传播,但在板层边界处停止。本研究表明,股骨颈皮质骨的过度矿化是骨脆弱性的一个来源,当基于当前评估标准髋部骨折的起源不清楚时,在未来的骨折风险评估中值得考虑。研究意义:在老年人中,股骨皮质骨的过度矿化发生在比目前已知更多的髋部骨折病例中。然而,由于临床成像的分辨率较差,这种组织对矫形外科医生来说仍然知之甚少。本研究表明,过度矿化组织的断裂阻力降低,这可能归因于矿物质含量、有机基质和矿物质板层特性的材料变化。因此,它可能是骨折起始的一个来源。因此,我们认为在髋部脆弱性评估中应考虑股骨颈皮质骨的过度矿化,特别是当低骨量不能被确定为髋部骨折的主要原因时。

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