Jh. Kinney et al., MINERAL DISTRIBUTION AND DIMENSIONAL CHANGES IN HUMAN DENTIN DURING DEMINERALIZATION, Journal of dental research, 74(5), 1995, pp. 1179-1184
Many bonding agents require the dentin surface to be acid-etched prior
to being bonded. Understanding the stability and morphology of the et
ched dentin surface is important for improving bond strength and relia
bility in these systems. In this study, the atomic force microscope wa
s used to quantify dimensional changes that occur to fully hydrated de
ntin during demineralization with a pH 4.0 lactic acid gel. A high-res
olution microtomography instrument, the x-ray tomographic microscope,
was also used to quantify the mineral density distribution in the dent
in as a function of etching time. The intertubular dentin surface shra
nk by less than 0.5 Fun during etching, while the peritubular dentin r
eceded at an initially rapid linear rate. The dentin surface retained
its initial morphology, although it was more porous with the removal o
f the peritubular dentin. Beneath the etched surface, there were three
major zones characterized by mineral density differences. The first z
one was a fully demineralized collagen layer, subjacent to which was a
partially demineralized zone of roughly constant mineral density. Imm
ediately following the partially mineralized layer was normal dentin.
The presence of the partially mineralized layer could be explained in
terms of different transport rates in the peritubular and intertubular
dentin.