0000000000520306

AUTHOR

Agnès Michel

showing 2 related works from this author

Geochemical mapping of magmatic gas–water–rock interactions in the aquifer of Mount Etna volcano

2001

Abstract Systematic analysis of major and minor elements in groundwaters from springs and wells on the slopes of Mt. Etna in 1995–1998 provides a detailed geochemical mapping of the aquifer of the volcano and of the interactions between magmatic gas, water bodies and their host rocks. Strong spatial correlations between the largest anomalies in pCO2 (pH and alkalinity) K, Rb, Mg, Ca and Sr suggest a dominating control by magmatic gas (CO2) and consequent basalt leaching by acidified waters of the shallow (meteoric) Etnean aquifer. Most groundwaters displaying this magmatic-type interaction discharge within active faulted zones on the S–SW and E lower flanks of the volcanic pile, but also in…

Basalt[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAlkalinityGeochemistryMineralogyAquifer010502 geochemistry & geophysics01 natural sciencesSalinityGeophysicsVolcano13. Climate actionGeochemistry and PetrologySedimentary rock[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentGeologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMud volcanoWater well
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Mobility and fluxes of major, minor and trace metals during basalt weathering and groundwater transport at Mt. Etna volcano (Sicily)

2000

Abstract The concentrations and fluxes of major, minor and trace metals were determined in 53 samples of groundwaters from around Mt Etna, in order to evaluate the conditions and extent of alkali basalt weathering by waters enriched in magma-derived CO 2 and the contribution of aqueous transport to the overall metal discharge of the volcano. We show that gaseous input of magmatic volatile metals into the Etnean aquifer is small or negligible, being limited by cooling of the rising fluids. Basalt leaching by weakly acidic, CO 2 -charged water is the overwhelming source of metals and appears to be more extensive in two sectors of the S-SW (Paterno) and E (Zafferana) volcano flanks, where out …

Basalt[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmospheregeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesAlkali basaltGeochemistryWeatheringAquifer010502 geochemistry & geophysics01 natural sciencesVolcano13. Climate actionGeochemistry and PetrologyLeaching (metallurgy)[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolatilesGroundwaterGeology0105 earth and related environmental sciences
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