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- Matsuya Shigeki
- Department of Biomaterials, Faculty of Dental Science, Kyushu University
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- Udoh Koh-ichi
- Department of Biomaterials, Faculty of Dental Science, Kyushu University
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- Nakagawa Masaharu
- Department of Biomaterials, Faculty of Dental Science, Kyushu University
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- Ishikawa Kunio
- Department of Biomaterials, Faculty of Dental Science, Kyushu University
抄録
Hydrolysis of calcite was investigated in 0.1 mol/L KH2PO4/KB2PO4 solutions with various pHs between 4.5 and 8.5 at 60°C by means of solution analyses (pH, Ca and P concentrations), X-ray diffraction, Fourier-transformed infrared spectroscopy and scanning electron microscopy. Calcite was mostly hydrolyzed within several days and the final product was octacalcium phosphate (OCP) or apatite phase depending on their initial pHs. OCP was initially formed in the solution with lower pH and it was transformed into apatite phase with increasing in pH. Calcite was directly transformed into apatite in 0.1 mol/L K2HPO4 solution with the highest initial pH. These phenomena were probably related to solubility of apatite, OCP and calcite at pH during hydrolysis. FT-IR analysis showed that the apatite phase formed was B-type carbonated apatite, in which CO32- ion substituted for PO43- ion.
収録刊行物
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- Phosphorus Research Bulletin
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Phosphorus Research Bulletin 17 (0), 159-164, 2004
Japanese Association of Inorganic Phosphorus Chemistry
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詳細情報 詳細情報について
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- CRID
- 1390282680440439936
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- NII論文ID
- 130004992469
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- COI
- 1:CAS:528:DC%2BD28XotlKkt7w%3D
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- ISSN
- 09184783
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可