Hernandez C J
Musculoskeletal Mechanics and Materials Laboratory, Case Western Reserve University, Cleveland, OH, USA.
Bone. 2008 Jun;42(6):1014-20. doi: 10.1016/j.bone.2008.02.001. Epub 2008 Feb 20.
The amount of bone turnover in the skeleton has been identified as a predictor of fracture risk independent of areal bone mineral density (aBMD) and is increasingly cited as an explanation for discrepancies between areal bone mineral density and fracture risk. A number of mechanisms have been proposed to explain how bone turnover influences bone biomechanics, including regulation of tissue degree of mineralization, the disconnection or fenestration of individual trabeculae by remodeling cavities, and the ability of cavities formed during the remodeling process to act as stress risers. While these mechanisms can influence bone biomechanics, they also modify bone mass. If bone turnover is to explain any of the observed discrepancies between fracture risk and areal bone mineral density, however, it must not only modify bone strength, but must also modify bone strength in excess of what would be expected from the associated change in bone mass. This article summarizes biomechanical studies of how tissue mineralization, trabecular disconnection, and the presence of remodeling cavities might have an effect on cancellous bone strength independent of bone mass. Existing data support the idea that all of these factors may have a disproportionate effect on bone stiffness and/or strength, with the exception of average tissue degree of mineralization, which may not affect bone strength independent of aBMD. Disproportionate effects of mineral content on bone biomechanics may instead come from variation in tissue degree of mineralization at the micro-structural level. The biomechanical explanation for the relationship between bone turnover and fracture incidence remains to be determined, but must be examined not in terms of bone biomechanics, but in terms of bone biomechanics relative to bone mass.
骨骼中的骨转换量已被确定为独立于骨面积密度(aBMD)的骨折风险预测指标,并且越来越多地被引用来解释骨面积密度与骨折风险之间的差异。人们提出了多种机制来解释骨转换如何影响骨生物力学,包括组织矿化程度的调节、重塑腔对单个小梁的断开或开窗,以及重塑过程中形成的腔作为应力集中器的能力。虽然这些机制可以影响骨生物力学,但它们也会改变骨量。然而,如果骨转换要解释骨折风险与骨面积密度之间观察到的任何差异,它不仅必须改变骨强度,而且还必须改变骨强度,且改变程度要超过骨量相关变化所预期的程度。本文总结了关于组织矿化、小梁断开和重塑腔的存在如何可能独立于骨量影响松质骨强度的生物力学研究。现有数据支持这样一种观点,即所有这些因素可能对骨刚度和/或强度产生不成比例的影响,但平均组织矿化程度除外,它可能不会独立于aBMD影响骨强度。矿物质含量对骨生物力学的不成比例影响可能反而来自微观结构水平上组织矿化程度的变化。骨转换与骨折发生率之间关系的生物力学解释仍有待确定,但必须从相对于骨量的骨生物力学角度进行研究,而不是仅从骨生物力学角度进行研究。