Estimation of fOX2 based on Fe-Mg exchange in olivine-orthopyroxene in magnetite buffered assemblages

This is based on the following equilibrium (see classic paper of Frost 1982, JPet)

6FeX2SiOX4+OX2=3FeX2SiX2OX6+2FeX3OX4 (1)

Oxygen fugacity can be expressed as follows

log⁡fOX2=3log⁡aFeX2SiX2OX6opx+2log⁡aFeX3OX4mt−6log⁡aFeX2SiOX4ol+ΔG°1/(ln⁡(10)·RT) [Eq. 1]

In order to derive this expression, let's start as

ΔGo+RTln⁡K=0

where

K=(aFeX2SiX2OX6opx)3+(aFeX3OX4mt)2(aFeX2SiOX4ol)6+aOX2fl

and

RTln⁡K=3RTln⁡aFeX2SiX2OX6opx+2RTln⁡aFeX3OX4mt−6RTln⁡aFeX2SiOX4ol−RTln⁡aOX2

the activity of OX2 is

ln⁡aOX2=3ln⁡aFeX2SiX2OX6opx+2ln⁡aFeX3OX4mt−6ln⁡aFeX2SiOX4ol+ΔG°1/RT

but we want log10 units instead so,

log⁡fOX2=3log⁡aFeX2SiX2OX6opx+2log⁡aFeX3OX4mt−6log⁡aFeX2SiOX4ol+ΔG°1/(ln⁡(10)·RT) [Eq. 1]

Formal derivation

The above treatment is obscure in the definition of ΔG°1 because it is calculated at the P,T conditions for all endmembers except for OX2 that is computed at 1 bar. The derivation is as follows

6FeX2SiOX4+OX2=3FeX2SiX2OX6+2FeX3OX4 (1)

for this reaction in solid solution we have

3gfso+2gmto−6gfao−μOX2o+RTln⁡K=0

Which is strictly

ΔGo+RTln⁡K=0

then

3gfso+2gmto−6gfao−μOX2o+3RTln⁡aFeX2SiX2OX6opx+2RTln⁡aFeX3OX4mt−6RTln⁡aFeX2SiOX4ol−RTln⁡aOX2

but noting that

μOX2=μOX2o+RTln⁡aOX2

that simplifies to

3gfso+2gmto−6gfao−μOX2+3RTln⁡aFeX2SiX2OX6opx+2RTln⁡aFeX3OX4mt−6RTln⁡aFeX2SiOX4ol

then

μOX2=3gfso+2gmto−6gfao+3RTln⁡aFeX2SiX2OX6opx+2RTln⁡aFeX3OX4mt−6RTln⁡aFeX2SiOX4ol

we normally report this value as fOX2, that by definition is

fOX2=exp⁡(μOX2−μOX21barRT)

fOX2=exp⁡(3gfso+2gmto−6gfao−μOX21bar+3RTln⁡aFeX2SiX2OX6opx+2RTln⁡aFeX3OX4mt−6RTln⁡aFeX2SiOX4olRT)

 

fOX2=exp⁡(3gfso+2gmto−6gfao−μOX21barRT)+3aFeX2SiX2OX6opx+2aFeX3OX4mt−6aFeX2SiOX4ol

or in ln units

ln⁡fOX2=3gfso+2gmto−6gfao−μOX21barRT+3ln⁡aFeX2SiX2OX6opx+2ln⁡aFeX3OX4mt−6ln⁡aFeX2SiOX4ol

and more frequently (ln⁡x=log10xln⁡(10))

log10⁡fOX2ln⁡(10)=3gfso+2gmto−6gfao−μOX21barRT+3ln⁡aFeX2SiX2OX6opx+2ln⁡aFeX3OX4mt−6ln⁡aFeX2SiOX4ol

log10⁡fOX2=3gfso+2gmto−6gfao−μOX21barln⁡(10)RT+3log⁡aFeX2SiX2OX6opx+2log⁡aFeX3OX4mt−6log⁡aFeX2SiOX4ol

which is Eq.1