“…Divalent iron has the highest electronegativity value, 1.65 (Fyfe, 1964), among all the major network-modifier cations (Mg, Ca, Fe, Na, and K) in silicate melts and the empty d orbitals of divalent iron favor its bonding to S 2À more readily than other ions lacking d orbitals, or with filled d orbitals (Fyfe, 1964). However, the activity of divalent iron is affected by the other components in the silicate melt, and the possible formation of melt species involving sulfur and cations other than iron cannot be eliminated (Eissa et al, 1996;O'Neill and Mavrogenes, 2002). Therefore, concentrations of all cations in the melt influence sulfur solubility, rather than only that of Fe.…”