Stability of α′′-Fe16N2 in hydrogenous atmospheres
2014
We revealed the inherent instability of α′′-Fe16N2 in hydrogenous atmospheres due to the denitrification toward α-Fe by forming NH3 at the particle surface. Coating the particle surface with SiO2 to suppress the formation of NH3 has proven to be a simple yet powerful method to enhance the stability of α′′-Fe16N2 in hydrogenous atmospheres.
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