The intervertebral disc faces high compressive forces during daily activities. Axial compression induces creeping fluid loss and reduction in disc height. With degeneration, disc fluids and height are progressively lost, altering biomechanics. It is assumed that this loss of fluids is caused by a drop in osmolality in the disc due to proteoglycan depletion. Here we investigate the isolated effect of a reduction in osmosis on the biomechanical properties of the intervertebral disc. Continuous diurnal loading was applied to healthy caprine intervertebral discs in a loaded disc culture system for a total of 6 days. We increased testing bath osmolality with two doses of polyethylene-glycol (PEG), thereby reducing the osmotic gradient between the disc and the surrounding fluid. This way we could study the isolated effect of reduced osmosis on axial creep, without damaging the disc. We evaluated: daily creep and recovery, recovery time-constants and compressive stiffness. Additionally, we investigated water content. There was a strong dose-dependent effect of PEG concentration on water content and axial creep behaviour: disc height, amplitude and rate of creep and recovery were all significantly reduced. Axial compressive stiffness of the disc was not affected. Reduction of water content and amplitude of creep and recovery showed similarity to degenerative disc biomechanics. However, the time-constants increased, indicating that the hydraulic permeability was reduced, in contrast to what happens with degeneration. This suggests that besides the osmotic gradient, the permeability of the tissues determines healthy intervertebral disc biomechanics.

Intervertebral disc degeneration is a common cause of low-back pain, the musculoskeletal disorder with the largest impact world-wide. The complex disease is however not yet well understood, and no treatment is available. This is somewhat in contrast with osteoarthritis, a subject of more extensive research. Intervertebral disc degeneration may though be a type of osteoarthritis, as other vertebrates have a diarthrodial joint instead of an intervertebral disc. We describe the parallel in view of the anatomy, composition and degeneration of the intervertebral disc and articular joint. Not only different embryonic origin and anatomy suggest significant differences between the intervertebral disc and the synovial joint, but their biomechanical properties also partly differ, as articulation is one of the key properties of a synovial joint and does not occur in the intervertebral disc. However, both tissues provide flexibility and are able to endure compressive loads, and both cell behavior and extracellular matrix appear much the same, mainly existing of chondrocytes, proteoglycans and collagen type II, suggesting that the environment of the cell is more important to its behavior than embryonic origin. Moreover, great similarities are found in the inflammatory cytokines, which are mainly IL-1β and TNF-α, and matrix-degrading factors (i.e. MMPs and ADAMTSs) involved in the cascade of degeneration, resulting in overlapping clinical and radiological features such as loss of joint space, subchondral sclerosis, and the formation of osteophytes, causing pain and morning stiffness. Therefore, we state that disc degeneration can result in the osteoarthritic intervertebral disc. This point of view may enhance the synergy between both fields of research, and potentially provide new regenerative strategies for intervertebral disc degeneration.