Havdrup T, Hulth A, Telhag H
Acta Orthop Scand. 1976 Jun;47(3):345-50. doi: 10.3109/17453677608992003.
Specimens of the joint surfaces of the tibia from patients with OA and RA were exposed were examined for bone mineralization, bone formation, osteoid tissue and bone resorption. Judging from the appearance of the osteoblasts in OA the sclerotic changes are mainly focal with relatively little osteogenesis. No osteoclasia was seen in the sclerotic areas. Breakdown of the mineralized cartilage is followed by the development of cysts with highly cellular connective tissue with high osteoblastic activity and osteoclasia. Osteoid tissue is relatively sparse. The changes in RA are more diffuse with a more active osteoblastic activity and widespread zones of osteoid tissue as well as resorption by osteoclasts. It appears as if the increased uptake of 85Sr in OA is more dependent on the occurrence of relatively inert osteosclerosis than on a rapid turnover of the bone tissue.
对骨关节炎(OA)和类风湿关节炎(RA)患者的胫骨关节面标本进行暴露处理,检查其骨矿化、骨形成、类骨质组织和骨吸收情况。从OA中成骨细胞的外观判断,硬化改变主要是局灶性的,成骨相对较少。在硬化区域未见破骨细胞。矿化软骨分解后,会形成囊肿,囊肿内有高度细胞化的结缔组织,具有高成骨细胞活性和破骨细胞活性。类骨质组织相对稀疏。RA中的改变更弥漫,成骨细胞活性更高,类骨质组织广泛存在,同时有破骨细胞吸收。似乎OA中85Sr摄取增加更多地取决于相对惰性的骨硬化的发生,而非骨组织的快速更新。