The influence of Fe Ti oxide microlites on bubble nucleation in rhyolitic melts

We conducted a set of high-temperature decompression experiments to constrain the mechanisms of heterogeneous bubble nucleation in high-silica rhyolitic melt that contained 4.6–4.8 wt% H 2 O. The melt was seeded with two different size fractions of magnetite crystals: 1–2 μm crystals and large crystals of 32–135 μm (long axis). The number density of bubbles (BND) that nucleated on the small crystals was found to increase from 10 6.5 to 10 8.7 cm −3 as H 2 O increasingly supersaturated (ΔP) in the melt from 3 to 23 MPa. At ΔP >23 MPs, however, the number of bubbles nucleated equals the number of small magnetite and no more nucleated with increased ΔP. At the same conditions, the number of bubbles that nucleated on the large crystals increases, from <1 bubble per crystal at ΔP = 3 MPa to 14 ± 4 bubbles per crystal at 58 MPa. We thus find that ΔP has a significant influence on the mechanisms of heterogenous nucleation, but the observed increases in BND are much greater than would be predicted solely from the increase in ΔP. The discrepancy can be reconciled if there are different sites on the crystals that become activated at greater ΔP, leading to greater numbers of bubbles nucleating. The cumulative BND nucleated on small crystals, however, is capped by the number of crystals present. The BND values generated at ΔP >23 MPa in our experiments overlap with those found in ~80 % of naturally occurring pumice. Assuming our experiments are representative of natural pumice, this suggests that explosively erupted magmas either become significantly volatile supersaturated before heterogeneously nucleating bubbles, or that the number of nucleation sites in natural magmas greatly exceed 10 9 cm −3 . • The number of bubbles that nucleate is controlled by the amount of decompression. • The number of available nucleation sites increases with increasing decompression. • Modeling should account for nucleation on different size fractions of crystals. • Modeling should account for different nucleation sites available. • Magmas may become highly supersaturated prior to eruption.