S. Kumaresan et al., Contribution of disc degeneration to osteophyte formation in the cervical spine: a biomechanical investigation, J ORTHOP R, 19(5), 2001, pp. 977-984
Cervical spine disorders such as spondylotic radiculopathy and myelopathy a
re often related to osteophyte formation. Bone remodeling experimental anal
ytical studies have correlated biomechanical responses such as stress and s
train energy density to the formation of bony outgrowth. Using these respon
ses of the spinal components, the present study was conducted to investigat
e the basis for the occurrence of disc-related pathological conditions. An
anatomically accurate and validated intact finite element model of the C4-C
5-C6 cervical spine was used to simulate progressive disc degeneration at t
he C5-C6 level. Slight degeneration included an alteration of material prop
erties of the nucleus pulposus representing the dehydration process. Modera
te degeneration included an alteration of fiber content and material proper
ties of the anulus fibrosus representing the disintegrated nature of the an
ulus in addition to dehydrated nucleus. Severe degeneration included decrea
se in the intervertebral disc height with dehydrated nucleus and disintegra
ted anulus, The intact and three degenerated models were exercised under co
mpression. and the overall force-displacement response, local segmental sti
ffness, anulus fiber strain, disc bulge, anulus stress, load shared by the
disc and facet joints, pressure in the disc, facet and uncovertebral joints
, and strain energy density and stress in the vertebral cortex were determi
ned. The overall stiffness (C4-C6) increased with the severity of degenerat
ion. The segmental stiffness at the degenerated level (C5-C6) increased wit
h the severity of degeneration. Intervertebral disc bulge and anulus stress
and strain decreased at the degenerated level. The strain energy density a
nd stress in vertebral cortex increased adjacent to the degenerated disc. S
pecifically. the anterior region of the cortex responded with a higher incr
ease in these responses. The increased strain energy density and stress in
the vertebral cortex over time may induce the remodeling process according
to Wolff's law, leading to the formation of osteophytes. (C) 2001 Orthopaed
ic Research Society. Published by Elsevier Science Ltd. All rights reserved
.