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T Aoba

Publications and source records attributed to T Aoba.

At least 73 records · Page 4Linked to original sources

Effects of acid-dissolution on thin ground sections of enamel caries studied by microradiography and x-ray microbeam diffraction.

In order to obtain information about the chemical reactivity of localized areas within natural enamel caries, thin ground sections prepared from white spot lesions were subjected to HCl solutions with 0.01, 0.05, and 0.1 N concentrations. Microradiographic examination combined by densitometric analysis demonstrated that the surface layer covering demineralized lesions remained relatively stable against acid attacks and that, despite the original lower degree of mineralization, its microradiographic density became higher than that of the underlying normal enamel during acid-dissolution. Another interesting finding was that in the experiment using the most diluted HCl solution, a radiopaque zone became noticeable at the advancing front of the lesions in the course of dissolution. X-ray microbeam diffraction analysis of these sections showed that no apparent alterations occurred in mineral structure of enamel with acid dissolution, except for the decrease in crystallinity of enamel apatite. Based on the results obtained here, one can expect that the surface layer and the interior part of natural carious lesions possess a high degree of resistance to acid attacks, relative to the underlying normal enamel.

Dental Caries↗

Crystallographic and structural alterations in the mineral phase of human enamel with carious attacks.

The present study aims to obtain further information about the crystallographic and structural alterations in the mineral phase of enamel with the onset of caries. For this purpose, X-ray microbeam diffraction analysis was carried out on ground sections prepared from natural white spot lesions. Electron spin resonance (ESR) analysis was also performed on block samples cut from white spot lesions and from undamaged enamel of the same teeth. The results of crystallinity measurements showed that enamel apatite in demineralized lesions was lower in crystallinity than the apatite in the surface layer and surrounding sound enamel. This X-ray diffraction study also revealed the presence of two non-apatitic minerals in the demineralized lesions. One type of the mineral is whitlockite, giving spotty rings. The nature of the other mineral, giving a single ring-like reflection, remains to be elucidated. A comparison of ESR spectra taken from the caries-attacked and undamaged enamel provided evidence that the former samples have a lower degree of alignment of apatite microcrystals. The occurrence of non-apatitic mineral phases and the observed difference in microcrystalline alignment may be the results of a remineralization process.

Apatites↗

Carbonate apatites from aqueous and non-aqueous media studied by ESR, IR, and X-ray diffraction: effect of NH4+ ions on crystallographic parameters.

Carbonate-containing apatites prepared from aqueous and non-aqueous media were investigated by ESR, IR, and X-ray diffraction. A typical asymmetric signal at g = 2.0, which many workers have observed in irradiated calcified tissues, is interpreted in terms of CO3(3)- and Co-2 and the trapped electron center, The CO3(3)- and CO2- ions originated from the carbonate which substitutes for the phosphate ion in the apatite crystalline structure. From the comparison of the data between the carbonate apatites prepared under the presence of Na+ and NH4+ ions, it is suggested that NH4+ ions contribute to the crystallographic parameters, either by substituting in the structure or by suppressing the CO3 incorporation into the structure, or by both. The production of the CO2- radical ion could be accounted for based on the concept of hydrogen bond between the oxygen atom of CO2(3)- and the hydrogen atom of NH4+.

Apatites↗

ESR on the hydroxyl ion vacancies in the apatites.

Heating biological apatites and synthetic apatites in the stream of inert gas saturated with heavy water vapor, introduces OD ions which substitute for the hydroxyl (OH) ions and partially for the OH vacancies, depending on the heating time and the gas flow rate. This has been verified by ESR and partially by IR. Deuteration gives no serious alterations of the a-axis dimension or of the PO4 bands in the IR spectra. These findings have been interpreted as suggesting that the OH ions diffuse out and the OD ions diffuse in through specific pathways, and the diffusing ions interact permanently with none of the other ions in the apatite structure. Heating in dry inert gas results in the formation of hydroxyl ion vacancies. The ESR spectra of these samples in the g = 2.06 region have been interpreted in terms of O-2 and O-. The shortening of the a-axis dimension in this case has been accounted for based on the loss of structurally incorporated H2O and the loss of the OH ions on the hexad axis.

Bone and Bones↗

Electron spin resonance study of sound and carious enamel.

The present electron spin resonance (ESR) study aimed to investigate chemical alterations in enamel apatite associated with carious attacks. Enamel blocks were cut from sound areas and natural white spot lesions of human molar teeth and then X-irradiated at room temperature in air. Q-band ESR analysis of these samples showed the presence of two stable signals in the spectra recorded at room temperature. One of them has been identified at CO3-(3) centers, which originate from the carbonate ion substituting in the apatite lattice. The other signal is tentatively identified as O- defects in the hexad axis of apatite lattice. A comparison of the spectra between sound and carious samples demonstrated that the intensity ratios between the O- and the g parallel component of CO3-(3), R = O-/CO3-(3) (g parallel), are significantly higher in the carious samples than in the sound ones. This suggests that enamel apatite in the white spot lesions may have less carbonate ions in the crystal lattice, or have a higher producibility of the O- defects in its hexad axis. The observed alterations in enamel apatite may well be accounted for by remineralization playing a major role in the formation of white spot lesions, because this acid-dissolution study using irradiated enamel blocks showed that the R values do not increase but decrease in a simple process of demineralization.

Dental Caries↗

Cementifying fibroma of the maxilla. Report of a case.

A case of cementifying fibroma growing into the right maxillary sinus is reported. Clinical and histopathological findings are presented. The differentiation from central fibro-osseous lesions in jaw bones is discussed.

Humans↗

The intact surface layer in natural enamel caries and acid-dissolved hydroxyapatite pellets. An X-ray diffraction study.

The crystallographic features of various histological sites found in enamel carious lesions were studied by means of X-ray microbeam diffraction. The most interesting finding was the crystallinity of apatite crystals in the intact surface layer covering the demineralized lesions was higher than that of the crystals in the subsurface lesions or unaffected areas. Acid-dissolution experiments using synthetic hydroxyapatite pellets showed that a well mineralized layer was produced on the pellet surface under the condition that no Ca and PO4 ions were added to the initial acidic solution. Furthermore, X-ray diffraction analysis revealed that half-line breadth values of 004, 222, and 310 reflections of apatite pellets decreased, and their integrated peak intensities increased with dissolution time. These findings are in agreement with the results obtained in the study of enamel carious lesions, leading to the conclusion that the intact surface layer is formed by deposition of the mineral ions from dissolving subsurface lesions, and that this process is accompanied by the improvement in crystallinity of apatite crystals, possibly due to growth of the crystals.

Crystallography↗

The laser-Raman spectroscopic studies on human enamel and precipitated carbonate-containing apatites.

Laser-Raman spectra of synthetic apatites containing from zero to 12.4 wt% carbonate ions and enamel apatite are reported. Special attention is paid to the correlation between the intensities of the carbonate, phosphate, and hydroxyl modes and the carbonate content in the apatites. The data presented here indicate that most of the CO2-3 incorporated in the apatite lattice substitutes for PO3-4 and suggest that a small amount of CO2-3 might be located in the OH- position.

Apatites↗

Solubility and crystallinity in relation to fluoride content of fluoridated hydroxyapatites.

Fluoridated hydroxyapatites were synthesized at 80 degrees C (pH 7.4) to study their crystallinity and solubility in relation to fluoride content. The crystallinity of fluoridated hydroxyapatities increased initially, then decreased, and finally increased again with the degree of fluoridation, whereas the decrease in relative solubility of fluoridated hydroxyapatites at 25 degrees C (pH 4.0) was proportional to the logarithm of the fluoride content.

Crystallography↗

High-voltage electron microscopy of radiation damages in octacalcium phosphate.

The present high-voltage electron microscopic study showed two types of radiation damages in OCP. The first type commenced with the formation of voids, which later grew and coalesced along the c-axis. The second type was characterized by the appearance of paired and concentric strain fields and the subsequent formation of dislocations. The origin of the strain fields is attributed tentatively to a precipitation of a second phase in the crystal.

Calcium Phosphates↗

Organic-bound chromium in enamel, dentin, and bone studied by electron spin resonance.

The present ESR investigation shows clearly that chromium is potentially present in the calcified tissues. With the use of the hydrazine-deproteinated procedure, it is suggested that chromium is associated with the organic constituent of the calcified tissues. The fact that the unheated tissues disclosed no chromium signal indicates either that the potentially present chromium is not paramagnetic, or that it is still paramagnetic, but the chromium signal cannot be detected because of a short relaxation time due to strong interaction with the organic materials.

Animals↗

Dissolution rate behavior of fluoridated apatite pellets.

The dissolution rate of synthetic fluoridated apatite pellets with various fluoride content was measured in acetate buffer solution at pH 4.0. The dissolution rate decreased with degree of fluoridation. The rate decreased greatly at low fluoride levels. The experimental data were analyzed by means of a diffusion-controlled model and compared with the solubility data. This model showed that the initial dissolution rate is greatly affected by both the solubility and the overall mass transfer resistance. Overall mass transfer resistance is affected by fluoride content.

Apatites↗