Volcanic degassing of bromine and iodine: experimental fluid/melt partitioning data and applications to stratospheric chemistry

In order to understand the degassing behavior of heavy halogens in Volcanic processes, we experimentally studied the distribution of Cl, Br, and I bet ween albite melt and hydrous fluids containing 0.01-2 wt% of NaCl, NaBr, or NaI, respectively. All experiments were carried out at 2 kbar and 900 degr eesC in rapid-quench cold-seal autoclaves with a run duration of 7 days. Th e major element compositions and CI contents of the glassy run products wer e measured by electron microprobe. Bromine and iodine were measured by prot on-induced X-ray emission. Fluid compositions were obtained by mass balance . All halogens investigated were found to partition strongly into the fluid phase. Over the range of concentrations studied, the halogen contents in t he melt are proportional to the concentrations in the fluid. The fluid/melt partition coefficients, D-f/m, are 8.1 +/- 0.2 for CI, 17.5 +/- 0.6 for Br , and 104 +/- 7 for I. The logarithm of D-f/m is linearly correlated with t he ionic radius of the halogenide ion. On the basis of our experimental dat a, we estimate the amount of bromine injected into the stratosphere by majo r volcanic explosions. For the 1991 Mount Pinatubo eruption, we obtain Br y ields of 11-25 kt as minimum estimates. These numbers are comparable to the total annual influx of bromine into the stratosphere from all other natura l and anthropogenic sources (about 100 kt/year). Since bromine is much more efficient in destroying stratospheric ozone than chlorine, it could at lea st be partially responsible for the massive ozone depletion observed after the 1991 Mount Pinatubo eruption. (C) 2000 Elsevier Science B.V. All rights reserved.