Julius Wolff Institut Charité - Universitätsmedizin Berlin, Berlin, Germany.
École Polytechnique, Montréal, Canada.
J Mech Behav Biomed Mater. 2018 Mar;79:309-313. doi: 10.1016/j.jmbbm.2018.01.012. Epub 2018 Jan 11.
Experimental and computational studies often presume that nuclei pulposi of non-degenerated human lumbar discs function as fluid-filled cavities with single hydrostatic pressures throughout that vary neither with time nor location and orientation. Recent simultaneous measurements of the pressure at multiple locations within disc nuclei have however shown time-dependent and nonhomogeneous pressure distributions. This combined in vitro and in silico study aims to re-examine the temporal and spatial variations of the pressure within disc nuclei with special focus on the effect of tissue hydration. After 20h of free swelling, effects of two preload magnitudes (0.06 and 0.28MPa) on nucleus pressure were investigated under 8h of constant preloads followed by 10 cycles of high-low loads each lasting 15min using 6 disc-bone bovine specimens. Changes in pressure at 3 different nucleus locations were recorded as surrogate measures of fluid flow within the discs. To identify the likely mechanisms observed in vitro, a finite element model of a human disc (L4-L5) was employed while simulating foregoing plus additional loading protocols. In vitro and computed results show a clear and substantial pressure gradient within the nucleus, especially early after the load application under higher loads and in more hydrated discs. The pressure reaches its maximum in the nucleus center reducing axially toward endplates and radially toward the nucleus-annulus interface. These cause pressure gradients that substantially diminish with time and at lower hydration levels. With time and as the pore pressure drops, the contribution of the nucleus bulk increases till it reaches equilibrium. The relative share of the annulus bulk in supporting the applied loads markedly increases not only with time but at higher loads and lower hydrations. The hydration state of the disc is hence crucial in the disc pressure distribution and internal response under various static-dynamic loads in vitro and in the replication of in vivo conditions.
实验和计算研究通常假定未退变的人类腰椎间盘的髓核作为充满液体的腔室发挥作用,其静水压力在整个髓核中既不随时间变化也不随位置和方向变化。然而,最近对椎间盘核内多个位置的压力进行的同步测量显示出时间依赖性和非均匀的压力分布。这项结合了体外和计算机模拟的研究旨在重新检查椎间盘核内压力的时间和空间变化,特别关注组织水合作用的影响。在自由水合 20 小时后,在 8 小时的恒载后,研究了两种预载大小(0.06 和 0.28MPa)对核压的影响,然后进行了 10 个高低载循环,每个循环持续 15 分钟,使用 6 个椎间盘-骨牛标本。作为椎间盘内流体流动的替代测量,记录了 3 个不同核位置的压力变化。为了确定体外观察到的可能机制,采用了人椎间盘(L4-L5)的有限元模型,同时模拟了上述外加额外的加载方案。体外和计算结果显示,在较高载荷和更水合的椎间盘中,尤其是在载荷施加后的早期,核内存在明显且显著的压力梯度。压力在核中心达到最大值,轴向向终板降低,径向向核-环界面降低。这些压力梯度随着时间的推移和水合水平的降低而显著减小。随着时间的推移,随着孔隙压力的下降,核体的贡献增加,直到达到平衡。在各种静态-动态载荷下,环体的相对份额不仅随着时间的推移而增加,而且在较高的载荷和较低的水合水平下也会增加。因此,在体外和体内条件的复制中,椎间盘的水合状态对椎间盘压力分布和内部响应至关重要。