Koeller W, Meier W, Hartmann F
Spine (Phila Pa 1976). 1984 Oct;9(7):725-33. doi: 10.1097/00007632-198410000-00013.
This investigation revealed biomechanical properties and some morphological parameters of isolated intervertebral discs at various disc levels. One hundred twenty-three specimens were subjected to axial dynamic compressive loads. The duration of testing was 5 minutes, the loads Fd1 = 650 N +/- 400 N (discs from T5-6 to L1-2) and Fd2 = 950 N +/- 540 N (discs from T9-10 to L5-S1). Down the spine, the mean disc heights and cross-sectional areas increased; the water content seemed to be nearly constant. Axial deformation and ventral bulging increased down the spine as well, which is mainly due to the increasing disc height. Creep showed different characteristics. It was smallest within the region T10-11 to L1-2 and increased above and below this level. The increase below L1-2 is mainly due to the increasing disc height; the increase above T10-11 occurs because the thoracic discs behave in a more viscous manner than the lumbar discs.
本研究揭示了不同椎间盘节段孤立椎间盘的生物力学特性和一些形态学参数。123个标本承受轴向动态压缩载荷。测试持续时间为5分钟,载荷Fd1 = 650 N +/- 400 N(T5 - 6至L1 - 2节段的椎间盘)和Fd2 = 950 N +/- 540 N(T9 - 10至L5 - S1节段的椎间盘)。沿脊柱向下,椎间盘的平均高度和横截面积增加;含水量似乎几乎恒定。轴向变形和腹侧膨出也沿脊柱向下增加,这主要是由于椎间盘高度增加所致。蠕变表现出不同的特征。它在T10 - 11至L1 - 2区域内最小,并在该水平以上和以下增加。L1 - 2以下的增加主要是由于椎间盘高度增加;T10 - 11以上的增加是因为胸段椎间盘比腰段椎间盘表现出更粘滞的特性。