Published experimental data were used in a new calibration of the dependence of the Ti4+/Ti3+ ratio in silicate melts on temperature, oxygen fugacity, and melt composition. The standard error in determining log {{{{X{ₓ₈{{{O}₂}}}}} / {{{{X{{ₓ₈{{{O}₂}}}}} ({{{X{ₓ₈{{{O}{₁{. 5}}}}}}}) }}}. -0em} ({{{X{ₓ₈{{{O}{₁{. 5}}}}}}}) }}} by the proposed equation log {{{{X{ₓ₈{{{O}₂}}}}} / {{{{X{{ₓ₈{{{O}₂}}}}} ({{{X{ₓ₈{{{O}{₁{. 5}}}}}}}) }}}. -0em} ({{{X{ₓ₈{{{O}{₁{. 5}}}}}}}) }}} = 0. 216log fO2 – 0. 280 {X{{ₓ₈{{{O}₂}}}^2} / {{X{{ₓ₈{{{₎₂}}}^2} X{{ₒ₈{{{O}₂}}}^{}}}}. -0em} X{{ₒ₈{{{O}₂}}}^{}}} – 2. 885 {{{X{₀{{{l}₂}{{O}₃}}}}} / {{{{X{{₀{{{l}₂}{{O}₃}}}}} {{X{ₒ₈{{{O}₂}}}}}}}. -0em} {{X{ₒ₈{{{O}₂}}}}}} – 5. 727XMgO/ {X{ₒ₈{{{O}₂}}}} – 5. 997XCaO/ {X{ₒ₈{{{O}₂}}}} – 3. 864 {{{X{₍{{{a}₂}O}}}} / {{{{X{{₍{{{a}₂}O}}}} {{X{ₒ₈{{{O}₂}}}}}}}. -0em} {{X{ₒ₈{{{O}₂}}}}}} + 12 433 (XMgO + XCaO + {X{₍{{{a}₂}O}}}) / ({X{ₒ₈{{{O}₂}}}} T (K) ) + 2. 490 (where Xi is the mole fraction of component i in the melt) is 0. 065, which is equivalent to an error of 0. 24 in determining log fO2. It has been shown that in melts corresponding to the compositions of lunar glasses (Delano, 1986), the Ti3+/Titot ratio at 1300°C and oxygen fugacity at the iron–wüstite (IW) buffer level is only 0. 03 on average. Even this small Ti3+ content should be mostly oxidized to Ti4+ during melt cooling/quenching into glass as a result of redox exchange with Fe3+.
А. A. Борисов (Mon,) studied this question.