Solubility of apatite is highly addressed in mineralogical and material studies.

Heating is one of the major processes in apatite industry. In this study, synthesized

hydroxylapatite (HAp), geological fluorapatite (FAp), and bone bioapatite (BAp) were heated

at various temperature (100-900 oC) for analyses. The mineralogy and solubility of the three

apatites were analyzed by XRD, ATR-IR, and ICP. Release of Ca and P in water for BAp

reach the maximum when heated at 200 oC, i.e., 0.215 mmol/L for Ca and 0.106 mmol/L for

P. The value is higher than the maximum values (heated at 900 oC) of solubility for HAp and

FAp. The heating temperature at 600 oC is a re-crystallization point for all the three types of

apatites. Especially, the crystallinity of BAp is significantly elevated at >600 oC. Phase of

geological FAp is relatively stable during heating up to 900 oC. Phase of =-TCP is present

when heating HAp at 800 to 900 oC. In addition, BAp is transformed to the resemblance of

HAp. However, no =-TCP was detected for BAp during heating between 800 to 900 oC,

which is probably due to its Ca-deficiency.

materials and fertilizer.

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