EFFECTS OF FLUORIDE ON THE HYDROLYSIS OF CALCITE IN POTASSIUM DIHYDROGEN PHOSPHATE SOLUTION

  • Matsuya Shigeki
    Department of Biomaterials Faculty of Dental Science, Kyushu University
  • Udoh Koh-ichi
    Department of Biomaterials Faculty of Dental Science, Kyushu University
  • Nakagawa Masaharu
    Department of Biomaterials Faculty of Dental Science, Kyushu University
  • Ishikawa Kunio
    Department of Biomaterials Faculty of Dental Science, Kyushu University

抄録

Hydrolysis of calcite was investigated in 0.1M KH2PO4 solution containing potassium fluoride (0 and 1005 ppm as F) at 37°C by means of solution analyses (pH, Ca, P and F concentrations), X-ray diffraction, 31P magic angle spinning nuclear magnetic spectroscopy (MAS NMR), Fourier-transformed infrared spectroscopy (FT-IR) and scanning electron microscopy (SEM). With the non-fluoride solution, octacalcium phosphate (OCP) was a main product of the hydrolysis for 10 days though some amount of calcite still remained. With increasing in fluoride concentration in the solution, OCP formed less and apatite phase formed instead. Remaining calcite was also decreased with fluoride concentration. Fluoride in the solution was completely absorbed in the product after hydrolysis for 10 days except for the highest fluoride concentration of 1000 ppm. FT-IR analysis showed that the apatite phase formed was fluoridated B-type carbonated apatite, in which CO32- ion substituted for PO43- ion. Fluoride ion was found to promote fluoridated carbonated apatite formation directly and/or through OCP transformation.

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詳細情報 詳細情報について

  • CRID
    1390282680440438528
  • NII論文ID
    130004992468
  • DOI
    10.3363/prb1992.17.0_153
  • COI
    1:CAS:528:DC%2BD28XotlKkt74%3D
  • ISSN
    09184783
  • 本文言語コード
    en
  • データソース種別
    • JaLC
    • Crossref
    • CiNii Articles
  • 抄録ライセンスフラグ
    使用不可

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