Decompression experiments were performed on corn syrup-water solutions in o
rder to investigate the effect of viscosity on processes of vesiculation an
d degassing at low to moderate degrees of volatile supersaturation. Repeat
experiments demonstrated similar long term vesiculation behavior at moderat
e decompression rates despite highly variable initial nucleation styles, Re
sults suggest that magmas may not necessarily achieve chemical equilibrium
by vapor exsolution and may require viscosity-dependent critical supersatur
ations in order to vesiculate. Vesiculation also increased the ambient pres
sure and decreased supersaturations, resulting in unsteady degassing.