A significant biochemical change that takes place in intervertebral disc degeneration is the loss of proteoglycans in the nucleus pulposus. Proteoglycans attract fluid, which works to reduce mechanical stresses in the solid matrix of the nucleus and provide a hydrostatic pressure to the annulus fibrosus, whose fibrous nature accommodates this stress. Our goals are to develop an osmoporoelastic finite element model to study the relationship between proteoglycan content and the stress distribution within the disc and to analyze the effects of degeneration on the disc's diurnal mechanical response. Stress in the annulus increased with degeneration from $0.2 to 0.4 MPa, and an increase occurred in the center of the nucleus from 1.2 to 1.6 MPa. The osmotic pressure in the central nucleus region decreased the most with degeneration, from $0.42 to $0.1 MPa in a severely dehydrated disc. A 3% decrease in diurnal fluid lost with degeneration equated to $21% decrease in fluid exchange, and hence a decrease in nutrients that require convection to enter the disc. We quantified the increases in internal stresses in the nucleus and annulus throughout the various stages of degeneration, suggesting that these changes lead to further remodeling of the tissue. Keywords: intervertebral disc; degeneration; osmotic pressure; diurnal cycle; finite element During a diurnal cycle, the intervertebral disc experiences $16 h of functional loading (e.g., standing and sitting), followed by 8 h of recovery (lying prone). As the disc is compressed and fluid is exuded, the density of the fixed charges within the nucleus is increased, creating an osmotic gradient with the interstitial fluids surrounding the disc; this osmotic potential aids in drawing fluid back into the disc.
1The intervertebral disc changes with age and degeneration.2-4 Alterations in its major biochemical constituents coincide with aging and disc degeneration, and can subsequently alter its ability to support load. A significant change is the loss of proteoglycans in the central region, the nucleus. Proteoglycans attract and bind fluid, working to resist mechanical stresses in the solid matrix of the nucleus and, through hydration of the molecules, provide a hydrostatic pressure to the outer layers of the disc, the annulus, whose fibers function in tension to support these additional stresses.5 In a dehydrated disc, the function of the nucleus to transfer load to the annulus through creation of intradiscal pressure no longer occurs at a normal level. However, the effects of these changes on the internal stresses and strains are not well understood. Also, since proteoglycans govern fluid content in the disc, their loss with degeneration affects fluid flow into and out of the disc throughout a diurnal cycle.Poroelastic theory does not account for the effects of swelling due to osmotic pressure on the mechanical behavior of the disc. Fixed negative charges from the proteoglycans help draw fluid back into the disc after loading (and work to retain the fluid during load...