We reported previously that dentinal fluid flow caused by intrapulpal pressure has inhibitory effects on root demineralization. However, its role in the comprehensive caries process including remineralization is not known. This study was conducted to examine the effects of dentinal fluid flow on remineralization of root caries lesion in vitro. The pulpal cavities of demineralized root samples were filled with a pulpal fluid-based mineral solution (0.65 mM CaCl
2, 0.94 mM KH
2PO
4, 20 mM HEPES buffer, pH7) under various intrapulpal pressure conditions (20,30 or 40 mmHg) for 8 d. It was confirmed using a confocal laser scanning microscopy that the dentinal fluid containing a fluorescent dye reached to root surfaces within a few minutes at 20 mmHg. Separately, demineralized root samples were immersed in a saliva-based mineral solution (1.5 mM CaCl
2, 0.9 mM KH
2PO
4, 20 mM HEPES buffer, pH 7, 0 or 2 ppm F
-) or a pulpal fluid-based mineral solution to investigate the effects of outer solutions on remineralization. After treatment, the lesions in the root surfaces were observed under a polarized microscope, and the mineral distributions were assessed microradiographically with the aid of computer assisted videodensitometry (CAV). The lesion depth l
d and mineral loss values ΔZ decreased with elevations in the pulpal pressure. Compared with the 20-mmHg group, the l
d values in the 40-mmHg group were lower by 55% with significant differences (p<0.01). In addition, it was found that the 40-mmHg group and samples remineralized by the saliva-based outer solution with 2 ppm F
- had no significant differences in the mineral parameter values (l
d and ΔZ), indicating equality of remineralization. In conclusion, it was suggested that dentinal fluid flow may play an important role in the remineralization of root caries, especially in the lesion bottom, as a physiological defense mechanism.
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