Formation of Fluorapatite in the Equilibrium System CaO–P<sub>2</sub>O<sub>5</sub>–HF–H<sub>2</sub>O at 298 K in a Nitrogen Atmosphere

Formation of Fluorapatite in the Equilibrium System CaO–P<sub>2</sub>O<sub>5</sub>–HF–H<sub>2</sub>O at 298 K in a Nitrogen Atmosphere

The process of biomineralization of apatite in nature has been studied by scientists from various fields of science for more than a century. Unlike the volcanogenic, hydrothermal, and other types of igneous apatites, the genesis of which is entirely clear, the formation of phosphate ores of marine s...

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Bibliographic Details
Main Authors: Marina V. Chaikina, Natalia V. Bulina, Igor Yu. Prosanov, Arcady V. Ishchenko
Format: Article
Language:English
Published: MDPI AG 2023-08-01
Series:Crystals
Subjects:
fluorapatite
formation
water system
low concentration
equilibrium
isotherm
Online Access:https://www.mdpi.com/2073-4352/13/8/1264

Internet

https://www.mdpi.com/2073-4352/13/8/1264

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