Wu J J, Eyre D R
Department of Orthopaedics, University of Washington, Seattle 98195.
Calcif Tissue Int. 1988 Apr;42(4):243-7. doi: 10.1007/BF02553750.
The method of heat-denaturation and trypsin digestion was used to dissect bone biochemically into mineral-protected and mineral-unprotected pools of collagenous matrix. It was found that varying the particle size of the bone powder had a profound effect on the results. Using mature bovine cortical bone, the observed pool of "unmineralized" (mineral-unprotected) collagen could be varied from 2% to more than 60% of the total bone collagen simply by decreasing the particle size of the bone sample from greater than 1 mm to less than 38 micron. No major differences were seen in the contents of hydroxypyridinium cross-links between the collagens of the trypsin-soluble and trypsin-insoluble pools from the fine powders, contrary to earlier reports. A trend to a higher content of these cross-links was evident, however, in the very small collagen pool extracted from the coarsest bone particles. Similar extraction differences were noted using bacterial collagenase to probe for mineral-protected vs. mineral-unprotected domains of bone collagen. In summary, the biochemical dissection results appear largely to be an artifact of the powdering technique, the shear energies of which presumably destroy the intimate physical relationship between the mineral crystallites and the collagen fibrils at the fractured surfaces of the bone particles. As the fractured surface area increases with decreasing particle size so the fraction of protease degradable collagen increases. Since powdering is routinely adopted for many structural studies on both the mineral and organic phases of bone, the findings on finely powdered bone should be interpreted cautiously.
采用热变性和胰蛋白酶消化法将骨进行生化剖析,分为矿物保护的和未受矿物保护的胶原基质池。结果发现,改变骨粉的颗粒大小对结果有深远影响。使用成年牛皮质骨,仅通过将骨样品的颗粒大小从大于1毫米减小到小于38微米,观察到的“未矿化”(未受矿物保护)胶原池可占总骨胶原的2%至60%以上。与早期报道相反,细粉中胰蛋白酶可溶池和胰蛋白酶不溶池的胶原之间,羟基吡啶交联的含量未见重大差异。然而,从最粗的骨颗粒中提取的非常小的胶原池中,这些交联的含量有升高趋势。使用细菌胶原酶探测骨胶原的矿物保护与未受矿物保护区域时,也注意到了类似的提取差异。总之,生化剖析结果在很大程度上似乎是粉碎技术的假象,粉碎的剪切能量可能破坏了骨颗粒断裂表面上矿物微晶与胶原纤维之间的紧密物理关系。随着颗粒大小减小,断裂表面积增加,因此蛋白酶可降解胶原的比例增加。由于在对骨的矿物相和有机相进行的许多结构研究中都常规采用粉碎方法,因此对细粉化骨的研究结果应谨慎解释。