Bone mineral density of the thoracolumbar spine in relation to burst fractures: a quantitative computed tomography study.

The most common pattern among thoracolumbar burst fractures involves failure of the superior vertebra end-plate. There have been many biomechanical studies of thoracolumbar burst fractures, but the biomechanics related to the internal architecture of thoracolumbar vertebrae has been rarely documented. The objective of this study was to test the hypotheses that distribution of the bone mineral density (BMD) of the thoracolumbar spine is related to the stress concentration in this region and therefore, supports the pattern of burst fractures that occur most commonly. We measured spinal BMD of the first lumbar vertebra in 22 individuals using quantitative computed tomography (QCT) in three levels. At each level, the BMD for the trabecular compartment was determined from each of six sites and from one site within each pedicle. Thus the trabecular density was measured at a total of 20 sites for each person. The highest average QCT BMD was in the pedicle (sites 13 and 14), whereas the BMD was abruptly decreased at the posterior part of the vertebral body near the pedicles. The results of the study indicate that stress concentration of the spine related to the regional variation in vertebral bone density may be implicated in the biomechanical mechanism underlying thoracolumbar burst fractures. This finding may be correlated with the injury mechanism of thoracolumbar burst fractures and of clinical significance.