Abstract

The pores (tubules) of human dentine in 0.02-cm planoparallel sections of newly extracted permanent teeth were investigated. By the conventional scanning electron microscopy these pores appear empty, but by the newly developed scanning-probe microscopy the presence of a complex matrix could be established. By measuring the transport of neutral myoglobin by diffusion alone and diffusion + bulk flow, the area of dentine occupied by the matrix was calculated to be 1.9 ± 0.9% and 2.3 ± 0.5%, respectively. The hydraulic conductivity was surprisingly small, 1.35 ± 0.55 × 10 −7 ml/(s·cm 2 dentine) at a pressure difference of 0.1 kPa across a 1-cm thick section. This suggests a hydrogel with a relatively dense network, the width of meshes estimated at 2 × 30 nm. In line with this concept, enzymatic degradation of the organic matter increased the hydraulic conductivity 3000 times. By studying the transport of negatively charged myoglobin, the matrix was calculated to carry 18 mEq/1 of positive charges. Due to the consequent attraction of small, negative ions and thence of water, the pressure within the matrix would be about 1.33 kPa, a force which will act to immobilize the water in the channels. The concept of a hydrogel in the dentine tubules was also supported by the finding that shielding the charges with bathing media of high ionic strength reduced the hydraulic conductivity.

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