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Ti atoms bond with Fe atoms and exchange their electron particles in the adjacent octahedral sites. This process produces the blue color on the blue sapphire. The Ti content is an important key to the alteration of the 3309 cm$^-$$^1$, 3232 cm$^-$$^1$, and 3185 cm$^-$$^1$ (3309 cm$^-$$^1$-series) peaks in infrared absorption (FTIR) spectra of blue sapphire samples. To study the effect of Fe and Ti oxidation state and the behavior of the Ti-related peaks in FTIR spectra during the heating process, the blue sapphire samples from Phrae and Kanchanaburi, Thailand were collected regarding their basaltic origins. The heating experiment was performed. The samples were step-heated at 800 °C, 1000 °C, 1200 °C, 1400 °C, and 1650 °C under an oxidizing atmosphere, with 1 hour soaking time at each temperature. The FTIR spectra and the X-ray absorption spectra (XAS) were measured before and after heating. Before heating, the FTIR spectra showed only the peak at 3309 cm$^-$$^1$ while the side peaks at 3232 cm$^-$$^1$ and 3185 cm$^-$$^1$ start to appear after heating at 800 ºC. The 3309 cm$^-$$^1$-series peaks were assigned as -Ti-OH stretching. The intensity of those peaks was slightly decreased after heat-treated. The XAS spectra revealed that the oxidation state of Fe is still Fe$^3$$^+$ while Ti is still Ti$^4$$^+$ in every heating temperature. The results pointed that the alteration of the 3309 cm$^-$$^1$-series peaks does not depend on the Fe and/or Ti oxidation state.
