Deviation from stoichiometric composition of ferrous-sulfide Fe
1−δS and solid solution sulfides (Fe, Cr)
1−δS containing Cr up to 0.3 cation fraction was measured as functions of sulfide composition ξ, sulfur pressures (1∼10
−5 Pa) and temperatures (973∼1173 K) using a thermogravimetric technique.
Nonstoichiometry δ increased with increasing Cr content in the (Fe, Cr)
1−δS and sulfur pressures, while it decreased with increasing temperature at a constant composition and sulfur pressure. Cation vacancy is a predominant lattice defect in the (Fe, Cr)
1−δS sulfide, and from the Libowitz model nonstichiometry δ and sulfur activity
aS could be expressed by the following relation:
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\
oindentwhere μ
MeS is a free energy change for formation of a sulfide with stoichiometric composition as well as
qVMe and σ
VMe are the formation and interaction energies of cation vacancies. It was observed that the values of σ
VMe were positive, ranging from 50 to 70 kJ/mol, independent of sulfide compositions, and the values of
qVMe decreased from 56 to 17 kJ/mol with increasing sulfide composition.
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