0000000000323108

AUTHOR

Roberto M. R. Di Martino

showing 3 related works from this author

Asynchronous changes of CO2, H2, and He concentrations in soil gases: A theoretical model and experimental results

2016

010504 meteorology & atmospheric sciencesHydrogenchemistry.chemical_elementSoil science010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundGeophysicschemistrySpace and Planetary ScienceGeochemistry and PetrologyAsynchronous communicationCarbon dioxideEarth and Planetary Sciences (miscellaneous)GeologyHelium0105 earth and related environmental sciencesJournal of Geophysical Research: Solid Earth
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Seismic moment tensors and regional stress in the area of the December 2013–January 2014, Matese earthquake sequence (Italy)

2014

Abstract The main goal of this study is to provide moment tensor solutions for small and moderate earthquakes of the Matese seismic sequence in southern Italy for the period of December 2013–January 2014. We estimate the focal mechanisms of 31 earthquakes with local magnitudes related to the Matese earthquake seismic sequence (December 2013–January 2014) in Southern-Central Italy which are recorded by the broadband stations of the Italian National Seismic Network and the Mediterranean Very Broadband Seismographic Network (MedNet) run by the Istituto Nazionale di Geofisica e Vulcanologia (INGV). The solutions show that normal faulting is the prevailing style of seismic deformation in agreeme…

Stress (mechanics)TectonicsSequence (geology)GeophysicsDeformation (mechanics)Moment tensorSeismic momentStress inversionSeismologyGeologyEarth-Surface ProcessesJournal of Geodynamics
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Continuous monitoring of hydrogen and carbon dioxide at Mt Etna

2013

article i nfo This study assessed the use of an H2 fuel cell as an H2-selective sensor for volcano monitoring. The resolution, repeatability, and cross-sensitivity of the sensor were investigated and evaluated under known laboratory conditions. A tailor-made device was developed and used for continuously monitoring H2 and CO2 at Mt Etna throughout 2009 and 2010. The temporal variations of both parameters were strongly correlated with the evolution of the volcanic activity during the monitoring period. In particular, the CO2 flux exhibited long-term variations, while H2 exhibited pulses immediately before the explosive activity that occurred at Mt Etna during 2010.

geographygeography.geographical_feature_categoryHydrogenContinuous monitoringCo2 fluxchemistry.chemical_elementSoil CO2 fluxH2 monitoringH2 fuel cell Mt EtnaGeologyRepeatabilityAtmospheric sciencesSettore GEO/08 - Geochimica E VulcanologiaSoil co2 fluxchemistry.chemical_compoundVolcanochemistryGeochemistry and PetrologyCarbon dioxideFuel cellsSeismologyGeologyChemical Geology
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