“…For conducting such experiments, the method proposed here provides an alternative to experimentation in IHPV equipped with a Shaw membrane, a technique that is being applied only in a few laboratories worldwide (e.g., Schmidt et al, 1997;Scaillet and Evans, 1999;Gaillard et al, 2001;Botcharnikov et al, 2005;Klimm et al, 2012a;Pichavant et al, 2016). An additional application area where flexible f O 2 control is critically important is the investigation of the solubility of metals in silicate melts and magmatic fluids because these will always be f O 2 dependent as most dissolution reactions involve the oxidation of the metal (Bell et al, 2011;Brenan et al, 2016;Guo et al, 2018;Sullivan et al, 2018;Zajacz et al, 2010Zajacz et al, , 2011Zajacz et al, , 2012aZajacz et al, , 2013. Sulfur is a constituent of important ligands that form complexes with ore-forming metals, and it goes through a very sharp redox transition from S 2− to S 6+ oxidation state exactly in the characteristic f O 2 range of arc magmas (Jugo et al, 2005(Jugo et al, , 2010Klimm et al, 2012b;Richards, 2014).…”