In-situ Raman spectroscopy of amorphous calcium phosphate to crystalline hydroxyapatite transformation

被引:111
|
作者
Stammeier, Jessica A. [1 ]
Purgstaller, Bettina [1 ]
Hippler, Dorothee [1 ]
Mavromatis, Vasileios [1 ,2 ]
Dietzel, Martin [1 ]
机构
[1] Graz Univ Technol, Inst Appl Geosci, Rechbauerstr 12, A-8010 Graz, Austria
[2] CNRS, UMR 5563, Observ Midi Pyrenees, GET, 14 Av E Belin, F-31400 Toulouse, France
关键词
Amorphous calcium phosphate; In-situ monitoring; Raman spectroscopy; Intermediate phase; Apatite;
D O I
10.1016/j.mex.2018.09.015
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Amorphous calcium phosphate (Ca-3(PO4)(2)xnH(2)O; n=3-4.5; ACP) is a precursor phase of the mineral hydroxyapatite (Ca-5(PO4)(3)(OH); HAP) that in natural settings occurs during both authigenic and biogenic mineral formation. In aqueous solutions ACP transforms rapidly to the crystalline phase. The transformation rate is highly dependent on the prevailing physico-chemical conditions, most likely on: Ca & PO4 concentration, pH and temperature. In this study, we conducted a calcium phosphate precipitation experiment at 20 degrees C and pH 9.2, in order to study the temporal evolution of the phosphate mineralogy. We monitored and assessed the transformation process of ACP to crystalline HAP using highly time-resolved in-situ Raman spectroscopy at 100 spectra per hour, in combination with solution chemistry and XRD data. Transformation of ACP to crystalline HAP occurred within 18 h, as it is illustrated in a clear peak shift in Raman spectra from 950 cm (1) to 960 cm (1) as well as in a sharpening of the 960 cm (1) peak. The advantages of this method are: In-situ Raman spectroscopy facilitates quasi - continuous monitoring of phase transitions. It is an easy to handle and non-invasive method. (C) 2018 The Authors. Published by Elsevier B.V.
引用
收藏
页码:1241 / 1250
页数:10
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