z-logo
open-access-imgOpen Access
Mercury and halogen emissions from Masaya and Telica volcanoes, Nicaragua
Author(s) -
Witt M. L. I.,
Mather T. A.,
Pyle D. M.,
Aiuppa A.,
Bagnato E.,
Tsanev V. I.
Publication year - 2008
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2007jb005401
Subject(s) - mercury (programming language) , fumarole , halogen , volcano , chemistry , plume , analytical chemistry (journal) , mercure , environmental chemistry , mineralogy , radiochemistry , geology , meteorology , alkyl , physics , organic chemistry , seismology , computer science , programming language
We report measurements of Hg, SO 2 , and halogens (HCl, HBr, HI) in volcanic gases from Masaya volcano, Nicaragua, and gaseous SO 2 and halogens from Telica volcano, Nicaragua. Mercury measurements were made with a Lumex 915+ portable mercury vapor analyzer and gold traps, while halogens, CO 2 and S species were monitored with a portable multi gas sensor and filter packs. Lumex Hg concentrations in the plume were consistently above background and ranged up to 350 ng m −3 . Hg/SO 2 mass ratios measured with the real‐time instruments ranged from 1.1 × 10 −7 to 3.5 × 10 −5 (mean 2 × 10 −5 ). Total gaseous mercury (TGM) concentrations measured by gold trap ranged from 100 to 225 ng m −3 . Reactive gaseous mercury accounted for 1% of TGM, while particulate mercury was 5% of the TGM. Field measurements of Masaya's SO 2 flux, combined with the Hg/SO 2 ratio, indicate a Hg flux from Masaya of 7.2 Mg a −1 . At Masaya's low temperature fumaroles, Hg/CO 2 mass ratios were consistently around 2 × 10 −8 , lower than observed in the main vent (Hg/CO 2 ∼ 10 −7 ). Low‐temperature fumarole Hg fluxes from Masaya are insignificant (∼150 g a −1 ). Ratios of S, C and halogen species were also measured at Masaya and Telica volcanoes. CO 2 /SO 2 ratios at Masaya ranged from 2.8 to 3.9, comparable to previously published values. At Masaya molar Br/SO 2 was 3 × 10 −4 and I/SO 2 was 2 × 10 −5 , suggesting fluxes of 0.2–0.5 Mg HBr d −1 and 0.02–0.05 Mg HI d −1 . At Telica the Br/SO 2 ratio was also 3 × 10 −4 and the I/SO 2 ratio was 5.8 × 10 −5 , with corresponding fluxes of 0.2 Mg HBr d −1 and 0.06 Mg HI d −1 . Gases at both volcanoes are enriched in I relative to Br and Cl, compared to gases from volcanoes elsewhere.

The content you want is available to Zendy users.

Already have an account? Click here to sign in.
Having issues? You can contact us here