Title: Valence state partitioning of V between pyroxene‐melt: Effects of pyroxene and melt composition, and direct determination of V valence states by XANES. Application to Martian basalt QUE 94201 composition
Abstract: Abstract— Experiments on a Martian basalt composition show that D v augite/melt is greater than D v pigeonite/melt in samples equilibrated under the same f O 2 conditions. This increase is due to the increased availability of elements for coupled substitution with the V 3+ or V 4+ ions, namely A1 and Na. For this bulk composition, both A1 and Na are higher in concentration in augite compared with pigeonite; therefore more V can enter augite than pigeonite. Direct valence state determination by XANES shows that the V 3+ and V 4+ are the main V species in the melt at f O 2 conditions of IW‐1 to IW+3.5, whereas pyroxene grains at IW‐1, IW, and IW+1 contain mostly V 3+ . This confirms the idea that V 3+ is more compatible in pyroxene than V 4+ . The XANES data also indicates that a small percentage of V 2+ may exist in melt and pyroxene at IW‐1. The similar valence of V in glass and pyroxene at IW‐1 suggests that V 2+ and V 3+ may have similar compatibilities in pyroxene.