In ancient times, glass products were not only practical goods but also prized as trading goods for their beauty and rarity. Ancient glassmakers produced colorful glasses using various materials around them. The authors have developed portable X-ray fluorescence spectrometers for on-site scientific investigation of cultural heritage and applied them to nondestructive chemical composition analysis of ancient glass products to discuss their production and trade from a scientific point of view. The present review outlines scientific analytical research of ancient glass and introduces the authors’ recent investigation of precious glass products designated as national treasures in Japan.
Due to iron impurities in the raw materials, it is typically difficult to produce industrial glass free of iron. Iron absorbs light in soda-lime glass over a broad wavelength range from ultraviolet to infrared. However, there are few reports on the relationship between the optical absorption and structure of the surrounding ions.
Herein, the structure of the surrounding iron ions in simplified soda silicate glass with MgO or CaO is examined in detail. Glasses composed of Na2O, SiO2 , and alkaline earth oxides (MgO or CaO) doped with FeO were strongly reduced to focus on the investigation of Fe2+. The surrounding structure of Fe2+ was examined using light, X-ray absorption spectroscopy, and molecular dynamics simulation. The results suggest that Fe2+ ions in Na2O-CaO-SiO2 glass show longer Fe-O bond length and higher degree of distortion of FeO6 octahedra compared with those in Na2O-MgO-SiO2 glass.
Low thermal expansion glass-ceramics including β-quartz s.s. as the main precipitated crystal have been applied widely, such as in electronic and optical devices, production equipment, and home and cooking appliances. The coloration mechanisms of Fe and V ions in glass-ceramics have been investigated because appearance is important in applications of fire-rated windows and top plates for cookers. It was revealed that the coloration occurs by a coexistence of Ti ion and the ions in residual glass-matrix phases through crystallization processes.