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Department of Geology, University of Toronto, 22 Russell Street, Toronto, Ontario, Canada M5S 3B1
Corresponding author: e-mail,brenan{at}zircon.geology.utoronto.ca
The effects of transition metal content and the fugacities of oxygen (fO2)
and sulfur (fS2)
on the wetting behavior of molten sulfide against forsteritic olivine have been
investigated in this study. Wetting behavior, or the mobility of a liquid phase
within a coexisting solid matrix, is quantified by the dihedral angle, 
,
which is a function of the relative solid-solid and solid-liquid surface
energies. In order to determine sulfide wetting behavior, experiments were
performed at 1,300°C
using a vertical tube furnace employing C-O-S gas mixtures to control fO2
and fS2.
Samples consisted of mixtures of San Carlos olivine and Fe + (Ni, Cu, Co; 0–30
wt 
) + S melts equilibrated for 24 to 168 hr. Experimental conditions ranged
from fO2
= 10–8
to 10–10
and fS2
from 10–1.2
to 10–4
in accordance with values appropriate for basalt petrogenesis. Results of our
experiments revealed that dihedral angles exhibited a marked increase with
decreasing fO2,
and variable dependence on melt metal composition. At fO2
= 10–8,
all sulfide melt compositions were found to be wetting (i.e.,
< 60°),
whereas only those with <~15 wt percent added Cu, Co, or Ni were wetting at fO2
= 10–9,
and no wetting compositions were encountered at fO2
= 10–10.
In agreement with the results of other investigators, we found that values of
decreased as the mole fraction of oxygen in the melt increased, suggesting that
metal oxide species in the melt are more likely to be surface-active with
respect to olivine.
In light of our experimental data, it is expected that the wetting behavior of natural sulfide liquids will depend on both the identity and quantity of nonferrous metal and the abundance of dissolved oxygen. Because of this latter effect, the prevailing conditions of both fO2 and fS2 are therefore likely to dictate sulfide melt mobility. In terms of the potential for sulfide melt metasomatism in the upper mantle, consideration of the range of fO2 reflected by natural sulfide liquids, mafic lavas, and upper mantle source regions reveals that conditions for sulfide melt mobility encompass much of this spectrum, even for many Ni- and Cu-rich natural liquid compositions. Thus, such liquids may be potent agents for redistributing siderophile and chalcophile elements in the upper mantle.
Sulfide melt wetting behavior will also play a role in the final sulfide distribution on solidification of mafic-ultramafic magmas that achieve saturation in an immiscible sulfide liquid. Efficient sulfide segregation may occur in reduced magmas only by early sulfide settling through a largely liquid medium, inasmuch as late-formed sulfide liquid will become trapped in the solid silicate matrix. For the case of relatively oxidized magmas, the wettability of sulfide liquid at these conditions, combined with a low viscosity and high density, suggests that efficient compaction-driven sulfide segregation is possible, even over the relatively short cooling intervals likely for high level mafic intrusions.
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