Search results for "Volcano-hydrothermal system"

showing 2 items of 2 documents

Geochemical processes assessed by Rare Earth Elements fractionation at "Laguna Verde" acidic-sulphate crater lake (Azufral volcano, Colombia)

2017

Abstract The geochemical behaviour of major elements, Fe, Al, Mn, and Rare Earth Elements (REE) was investigated in the “Laguna Verde” acidic crater lake of Azufral volcano (Colombia). The cold lake water (T close to 10 °C) is sulphate-dominated, due to absorption and oxidation of H2S (pH 2.1–2.7, Eh 196–260 mV), and Na-enriched (Total Dissolved Solids 0.79 g L−1). The total amount of REE dissolved in the lake ranges from 3.3 to 9.1 ppb. The REE patterns normalized to the local rocks show a Light Rare Earth Elements (LREE) depletion quite constant in the 15 samples. Similar patterns were already found in the acidic sulphate springs of Nevado del Ruiz volcano-hydrothermal system, caused by t…

Alunite precipitation010504 meteorology & atmospheric sciencesGeochemistryMineralogyengineering.material010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationRare Earth ElementVolcano-hydrothermal systemImpact craterGeochemistry and PetrologyCrater lakeJarositeEnvironmental ChemistryPrecipitation0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryAcidic crater lakeAlunitePollutionVolcanoLight Rare Earth Elements depletionengineeringSeawaterGeology
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The role of the aquifer in soil CO2 degassing in volcanic peripheral areas: A case study of Stromboli Island (Italy)

2017

Abstract The peripheral area of Stromboli Island, Italy, named “Scari”, was continuously studied between January 2009 and December 2010. Data on soil CO 2 flux and the partial pressure of CO 2 (pCO 2 ) in equilibrium with the thermal aquifer linked to the magmatic system are presented. Soil CO 2 fluxes range from 20 to 370 g m − 2  d − 1 and have been strongly affected by soil temperature variations. Soil CO 2 flux data were filtered with respect to the soil temperature and the calculated values, called “residuals”, were considered to detect changes induced by the magmatic system. The pCO 2 values change in a wide range from 0.03 to 0.6 (atm), showing rapid variations. The results of this s…

Hydrologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciences2GeologySoil scienceAquiferin waterPartial pressure010502 geochemistry & geophysics01 natural sciencesfluxVolcano-hydrothermal systemSoil temperatureFlux (metallurgy)VolcanoGeochemistry and PetrologypCOMagmaSoil COGeologyGas-water interaction0105 earth and related environmental sciencesChemical Geology
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