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Hydroxyl and calcium ions diffusion from endodontic materials through roots of primary teeth - in vitro study

DOI: 10.1590/S1678-77572005000200018

Keywords: calcium hydroxide, atomic absorption spectrophotometer, primary teeth.

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Abstract:

the purpose of this research was to evaluate the diffusion of calcium (ca+2) and hydroxyl (oh-) ions from materials with a calcium hydroxide base - ca(oh)2 through the intact roots of deciduous teeth. this diffusion of ions is important for periapical healing. forty-six deciduous teeth were selected and instrumented to their working length with #40 files. the teeth were washed during cleaning and shaping with a 1% sodium hypochlorite (naocl) solution. the canals were dried with paper points. the teeth were divided into 4 groups based on the sealer type, with 10 specimens in each group. a fifth group of 6 teeth without sealer constituted the control group. the materials used as sealers were: ca(oh)2 paste associated to propylene glycol (cape) thickened at the proportion of 2:1 w/v; ufsc (federal university of santa catarina) paste - a mixture of 0.3g of zinc oxide with 0.3g of ca(oh)2 with 0.2ml of olive oil 1:1 w/w; vitapex? and sealapex?. the coronal access was sealed with a glass ionomer after the root had been filled with each sealer. a one-third apical surface and foramen was hard-pressed with araldite?. the teeth were stored individually in flasks containing saline solution at 37oc and 100% humidity. the oh- and ca+2 ions diffusion levels were determined using a ph meter and an atomic absorption spectrometer. data were collected at 48 hours and at intervals of 7, 30, 45 and 60 days. statistical analysis was performed using anova to compare groups. in the ph evaluation, the cape group presented the largest oh- ions diffusion, which peaked at sixty days (p=0.0309), when compared to the other groups (p<0.0001). in relation to amount of ca+2 ions released, the cape paste showed the best results, followed by the ufsc's paste. these results suggest that the cape paste was the material that allowed the highest diffusion of oh- and ca+2 ions.

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