That sounds logical, but then some weird things occur in a certain (un)published dataset on olivine-melt trace element partitioning;
in a certain synthesized melt a MgO wt% measurement of 30,85% was measured, and a Mg wt% of 6,71%.. In another experiment a MgO wt% of 24,37 and Mg wt% of 5,30 was measured.
I don't get how these differences can be that large. I would expect a ratio of these wt% values of MgO and Mg respectively of 40,31/24,305 = 1,658.. But that does not seems to be the case.