Abstract
The metastable β-phase Zn2SiO4:Mn2+ phosphor was successfully reproducible only under the following critical conditions: SiO2-rich stoichiometry, melting, and rapid cooling. The metastability of the β-phase was demonstrated through the phase transformation of the as-grown β-phase into the α-phase polymorph by reannealing and then slowly cooling. The β-phase showed yellow emission with a quantum efficiency of 65 %. The β-phase has less crystalline structure caged into amorphous SiO2 phase and the more widely diffused larger grain sizes like a hexagonal shape of a snowflake. It showed the less thermal quenching behavior due to its lower lattice vibration, as well as the longer decay time due to less Mn2+ pairs.
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