Transport of fluid and solute in the intervertebral disc is studied in relation to the physicochemical properties of the tissue, in particular to its polyelectrolyte character which is conferred by the presence of glycosaminoglycans.
Solute partition and diffusion coefficients were determined in vitro, using experimental techniques which avoided leaching of glycosaminoglycans and swelling of the tissue. These in vitro measurements were found to apply to in vivo transport of (³⁵S) sulphate into dog discs. From the in vivo results it was estimated that about 40 percent of the endplate area was permeable to solutes. Since the profiles of (³⁵S) sulphate corresponded with those calculated using Ficks law, diffusion appears to be the main mechanism for solute transport into the disc.
Fluid transport was described in terms of a flow coefficient which depended on both the net swelling pressure in the tissue and on its hydraulic permeability. Experimental methods for the in vitro measurements of these parameters are described.