The effects of temperature and pressure on the oxidation state of chromium in silicate melts.

The oxidation state of Cr, Cr²⁺/ΣCr (where ΣCr = Cr²⁺ + Cr³⁺ = 0.35 wt%), in Fe-free silicate glasses quenched from melts equilibrated as a function of pressure to 3.5 GPa at 1500 °C, and as a function of temperature to 1500 °C at atmospheric pressure, and at oxygen fugacities (fO₂, in log units relative to the quartz-fayalite-magnetite (QFM) buffer) between ∆QFM = − 1 and − 2, was determined by XANES spectroscopy. Increasing temperature stabilises Cr²⁺ and increasing pressure stabilises Cr³⁺. A general expression for Cr³⁺/Cr²⁺ in silicate melts was derived: log(Cr³⁺/Cr²⁺) = 1/4(∆QFM + 8.58 − 25,050/T + 940P/T − 0.02P) + 9770/T − 7.69 + 6.22Λ + (900P − 172P²)/T, where P is pressure in GPa, T is temperature in K, and Λ is the optical basicity of the composition. This equation reproduces 213 Cr²⁺/ΣCr values reported here and in the literature with an average ΔCr²⁺/ΣCr of 0.02. A MORB melt at 1400 °C and QFM is predicted to have Cr²⁺/ΣCr ~ 0.35 at the surface but Cr²⁺/ΣCr ~ 0 at a depth of ~ 60 km. Although Cr²⁺ is an important oxidation state in silicate melts it is not preserved at low temperatures due to an electron exchange reaction with Fe³⁺. [ABSTRACT FROM AUTHOR]