6533b821fe1ef96bd127aff5

RESEARCH PRODUCT

Sulphur-gas concentrations in volcanic and geothermal areas in Italy and Greece: Characterising potential human exposures and risks

Walter D'alessandroSergio CalabreseAlessandro AiuppaAlessandro AiuppaManfredi LongoKonstantinos KyriakopoulosLorenzo BruscaMarcello LiottaSergio Bellomo

subject

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesHydrogen sulphide010502 geochemistry & geophysics01 natural sciencesVolcanic riskFumaroleSettore GEO/08 - Geochimica E VulcanologiaSulphur dioxide Hydrogen sulphide Volcanic risksGas hazardVolcano13. Climate actionGeochemistry and PetrologyEconomic GeologyPhysical geographyGeothermal gradientGeologySeismology0105 earth and related environmental sciences

description

Abstract Passive samplers were used to measure the atmospheric concentrations of SO 2 naturally emitted at three volcanoes in Italy (Etna, Vulcano and Stromboli) and of H 2 S naturally emitted at three volcanic/geothermal areas in Greece (Milos, Santorini and Nisyros). The measured concentrations and dispersion patterns varied with the strength of the source (open conduits or fumaroles), the meteorological conditions and the area topography. At Etna, Vulcano and Stromboli, SO 2 concentrations reach values that are dangerous to people affected by bronchial asthma or lung diseases (> 1000 μg m − 3 ). H 2 S values measured at Nisyros also exceed the limit considered safe for the same group of people (> 3000 μg m − 3 ). The data obtained using passive samplers represent time-averaged values over periods from a few days up to 1 month, and hence concentrations probably reached much higher peak values that were potentially also dangerous to healthy people. The present study provides evidence of a peculiar volcanic risk associated with tourist exploitation of active volcanic areas. This risk is particularly high at Mt. Etna, where the elderly and people in less-than-perfect health can easily reach areas with dangerous SO 2 concentrations via a cableway and off-road vehicles.

10.1016/j.gexplo.2012.08.015http://hdl.handle.net/10447/72277