A proposal on the hard tissue remineralization in osteoarthritis of the knee joint investigated by FT-IR spectrometry.

An investigation was performed on hard tissues of the affected area in the cases of osteoarthritis of the knee joint by using Fourier transform infrared spectroscopy (FT-IR) to obtain the information on components and characteristics of the compounds in the hard tissues at the molecular level. Biological specimens used were: normal cortical bone, normal cancellous bone, sclerotic area of the affected site (subchondral bone), osteophyte and cartilage of the affected joint. FT-IR spectra of these specimens were measured and spectroscopic characteristics of various types of hard tissues were quantified. As the result of the analysis, signal ratio of PO4(3-) to amide I (PO4(3-)/amide I) was 0 in cartilage, and the ratio was at the highest in normal cortical bone of the ulna, being as high as 1.82. The signal ratio of the sclerotic area of the affected site was 1.69, and this was higher than the values in osteophyte (1.44) or cancellous bone of the tibia (1.61). It is inferred from these data that the degree of remineralization was considerably higher in osteoarthritis of the knee joint. On the other hand, in the osteophyte, which is frequently seen in the radiography of osteoarthritis, it was 1.44 for the attached osteophyte and 1.37 for the detached osteophyte, and these values were lower compared with the values in the sclerotic area of the affected site (1.69). From these results, it appears that remineralization of mineral components is very likely to occur under the acidic conditions in the articular region in this disease. We propose that the mechanism of hard tissue formation in the knee joint of osteoarthritis is a form of remineralization.