{"title":"CHARACTERIZATION AND HYDRATION REACTIVITY OF α–TRICAICIUM PHOSPHATE PREPARED BY HEATING WITH GYPSUM","authors":"H. Monma, Y. Moriyoshi, H. Ogata, T. Okura","doi":"10.3363/PRB.27.1","DOIUrl":null,"url":null,"abstract":"Beta tricalcium phosphate (β-Ca3(PO4)2, β-TCP) mixed with gypsum (CaSO4・2H2O) was heated at 1300°C and 1400°C. The resulting products were characterized by DTA, XRD, FTIR, EDX and hydration reactivity. An inhibition effect on the transition of the low temperature form β to high temperature form α was observed with increasing the amount of gypsum. The substitution of SO4 for PO4 was suggested from increases of the β→α transition temperature and hydration reactivity. However both the substitution and the presence of S were not recognized by XRD, EDX and FTIR. Increasing the amount of gypsum resulted in the formation of hydroxyapatite (Ca5(OH)(PO4)3) at 1300°C and tetracalcium phosphate (Ca4(PO4)2O) at 1400°C. The hydration reactivity was in the order, pure α-TCP << α-TCP heated with gypsum. (Received Oct. 6, 2011; Accepted March 17, 2012)","PeriodicalId":20022,"journal":{"name":"Phosphorus Research Bulletin","volume":"32 1","pages":"1-5"},"PeriodicalIF":0.0000,"publicationDate":"2012-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Phosphorus Research Bulletin","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3363/PRB.27.1","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
Beta tricalcium phosphate (β-Ca3(PO4)2, β-TCP) mixed with gypsum (CaSO4・2H2O) was heated at 1300°C and 1400°C. The resulting products were characterized by DTA, XRD, FTIR, EDX and hydration reactivity. An inhibition effect on the transition of the low temperature form β to high temperature form α was observed with increasing the amount of gypsum. The substitution of SO4 for PO4 was suggested from increases of the β→α transition temperature and hydration reactivity. However both the substitution and the presence of S were not recognized by XRD, EDX and FTIR. Increasing the amount of gypsum resulted in the formation of hydroxyapatite (Ca5(OH)(PO4)3) at 1300°C and tetracalcium phosphate (Ca4(PO4)2O) at 1400°C. The hydration reactivity was in the order, pure α-TCP << α-TCP heated with gypsum. (Received Oct. 6, 2011; Accepted March 17, 2012)