Zuo Qiliang, Lu Shifeier, Du Zhibin, Friis Thor, Yao Jiangwu, Crawford Ross, Prasadam Indira, Xiao Yin
Ministry Education Key Laboratory for Oral Biomedical Engineering, School of Stomatology, Wuhan University, Wuhan, 430079, People's Republic of China.
Xiamen Dental Hospital, Xiamen, Fujian Province, China.
BMC Musculoskelet Disord. 2016 Aug 24;17(1):367. doi: 10.1186/s12891-016-1226-1.
Although articular cartilage is the primary tissues affected by osteoarthritis (OA), the underlying subchondral bone also undergoes noticeable changes. Despite the growing body of research into the biophysical and mechanical properties of OA bone there are few studies that have analysed the structure of the subchondral sclerosis at the nanoscale. In this study, the composition and nano-structural changes of human osteoarthritis (OA) subchondral bone were investigated to better understand the site-specific changes.
OA bone samples were collected from patients undergoing total knee replacement surgery and graded according to disease severity (grade I: mild OA; grade IV: severe OA). Transmission electron microscopy (TEM), Electron Diffraction, and Elemental Analysis techniques were used to explore the cross-banding pattern, nature of mineral phase and orientation of the crystal lattice. Subchondral bone nano-hydroxyapatite powders were prepared and characterised using high resolution transmission electron microscopy (HR-TEM) and fourier transform infrared spectroscopy (FTIR). Subchondal bone mechanical properties were investigated using a nano-indentation method.
In grade I subchondral bone samples, a regular periodic fibril banding pattern was observed and the c-axis orientation of the apatite crystals was parallel to the long axis of the fibrils. By contrast, in grade IV OA bone samples, the bulk of fibrils formed a random and undulated arrangement accompanied by a circular oriented pattern of apatite crystals. Fibrils in grade IV bone showed non-hierarchical intra-fibrillar mineralization and higher calcium (Ca) to phosphorous (P) (Ca/P) ratios. Grade IV OA bone showed higher crystallinity of the mineral content, increased modulus and hardness compared with grade I OA bone.
The findings from this study suggest that OA subchondral sclerotic bone has an altered mineralization process which results in nano-structural changes of apatite crystals that is likely to account for the compromised mechanical properties of OA subchondral bones.
尽管关节软骨是骨关节炎(OA)影响的主要组织,但下方的软骨下骨也会发生显著变化。尽管对OA骨的生物物理和力学特性的研究越来越多,但很少有研究在纳米尺度上分析软骨下硬化的结构。在本研究中,对人类骨关节炎(OA)软骨下骨的成分和纳米结构变化进行了研究,以更好地了解特定部位的变化。
从接受全膝关节置换手术的患者中收集OA骨样本,并根据疾病严重程度进行分级(I级:轻度OA;IV级:重度OA)。使用透射电子显微镜(TEM)、电子衍射和元素分析技术来探究交叉带模式、矿物相的性质和晶格取向。制备软骨下骨纳米羟基磷灰石粉末,并使用高分辨率透射电子显微镜(HR-TEM)和傅里叶变换红外光谱(FTIR)进行表征。使用纳米压痕法研究软骨下骨的力学性能。
在I级软骨下骨样本中,观察到规则的周期性纤维带模式,磷灰石晶体的c轴取向与纤维的长轴平行。相比之下,在IV级OA骨样本中,大部分纤维形成随机且起伏的排列,并伴有磷灰石晶体的圆形取向模式。IV级骨中的纤维显示出非分层的纤维内矿化和更高的钙(Ca)磷(P)(Ca/P)比。与I级OA骨相比,IV级OA骨的矿物质含量结晶度更高,模量和硬度增加。
本研究结果表明,OA软骨下硬化骨的矿化过程发生改变,导致磷灰石晶体的纳米结构变化,这可能是OA软骨下骨力学性能受损的原因。