Search results for "Environmental Science"

showing 10 items of 15856 documents

Selenium mobilization in soils due to volcanic derived acid rain: An example from Mt Etna volcano, Sicily

2011

International audience; The significant amounts of selenium (Se) emitted by volcanoes may have important impact on human health due to the narrow range between nutrition requirement and toxic effects for living organisms upon Se exposure. Although soils play a key role in determining the level in food and water and thereby human health, little is known about the behaviour of Se in volcanic soils. In this work we evaluated the Se release during rainwater–soil interaction under controlled conditions using soils collected on the flanks of Etna volcano and synthetic rain. Selenium concentrations in soil leachate solutions displayed a spatial distribution, which cannot be explained by plume depo…

010504 meteorology & atmospheric sciencesSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; GroundwaterSelenium; Volcanic soils; Geogenic; Volcanoes; Contamination; Groundwaterchemistry.chemical_element[SDU.STU]Sciences of the Universe [physics]/Earth SciencesVolcanoe010502 geochemistry & geophysics01 natural sciencesSelenateVolcanic soilchemistry.chemical_compoundSeleniumContaminationGeochemistry and PetrologySelenium acid rain soilsGeogenicChemical compositionGroundwater0105 earth and related environmental sciencesgeographyGroundwaterSeleniumgeography.geographical_feature_categoryGeologySettore GEO/08 - Geochimica E VulcanologiaDeposition (aerosol physics)chemistryVolcano13. Climate action[SDU]Sciences of the Universe [physics]Environmental chemistrySoil waterAcid rainGeologyGroundwaterSelenium
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Stage–Discharge Relationship for an Upstream Inclined Grid with Transversal Bars

2016

AbstractCheck dams with grids upgrading upstream are often used in mountain rivers, where intense sediment transport and steep slopes occur. In some cases, sloping grids are used in the construction of debris flow breakers. In this paper, the outflow process of an upstream-inclined grid with transversal bars is studied by using the dimensional analysis and the incomplete self-similarity theory. Next, the theoretical analysis shows that a power equation can be used for establishing the stage-discharge equation. The coefficient of the power equation depends on both the slope angle and the void ratio, whereas the exponent depends only on the slope angle. Finally, this deduced stage–discharge r…

010504 meteorology & atmospheric sciencesSelf-similarity0208 environmental biotechnologyGeometryAstrophysics::Cosmology and Extragalactic Astrophysics02 engineering and technologyGrid01 natural sciencesAgricultural and Biological Sciences (miscellaneous)020801 environmental engineeringDebris flowTransversal (combinatorics)Upstream (networking)OutflowGeotechnical engineeringStage (hydrology)Sediment transportGeology0105 earth and related environmental sciencesWater Science and TechnologyCivil and Structural EngineeringJournal of Irrigation and Drainage Engineering
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Comparison of cloud-reconstruction methods for time series of composite NDVI data

2010

Land cover change can be assessed from ground measurements or remotely sensed data. As regards remotely sensed data, such as NDVI (Normalized Difference Vegetation Index) parameter, the presence of atmospherically contaminated data in the time series introduces some noise that may blur the change analysis. Several methods have already been developed to reconstruct NDVI time series, although most methods have been dedicated to reconstruction of acquired time series, while publicly available databases are usually composited over time. This paper presents the IDR (iterative Interpolation for Data Reconstruction) method, a new method designed to approximate the upper envelope of the NDVI time s…

010504 meteorology & atmospheric sciencesSeries (mathematics)0211 other engineering and technologiesSoil ScienceGeology02 engineering and technologyLand cover15. Life on land01 natural sciencesNormalized Difference Vegetation IndexBruit13. Climate actionCompositingmedicineEnvironmental scienceSatellite imageryNoise (video)Computers in Earth Sciencesmedicine.symptom021101 geological & geomatics engineering0105 earth and related environmental sciencesInterpolationRemote sensingRemote Sensing of Environment
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Mountain building in NW Sicily from the superimposition of subsequent thrusting and folding events during Neogene: structural setting and tectonic ev…

2017

We present a 1:25.000 scale geological map of the Kumeta-Pizzuta ridge in north-western Sicily (Italy), achieved by integrating stratigraphic, structural and geophysical data. In this area, the tectonic edifice results from the piling-up of deep-water-, carbonate platform- and pelagic platform-derived tectonic units (Imerese and Sicilide, Panormide and Trapanese domains, respectively) resulting from deformations of the former southern Tethyan continental margin. The structural setting shows interference of tectonic events, different types of structural styles and different scales of deformational patterns. Early overthrust of the Imerese on the Trapanese units (since the late Serravallian) …

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformGeography Planning and Development010502 geochemistry & geophysicsNeogene01 natural sciencesgeological mapContinental marginlcsh:G3180-9980Sicily; Kumeta ridge; backthrust; geological mapEarth and Planetary Sciences (miscellaneous)SuperimpositionSicily0105 earth and related environmental scienceslcsh:Mapsgeographygeography.geographical_feature_categoryKumeta ridgeGeologic mapTectonicsMountain formationRidgeSeismologyGeologybackthrust
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An Integrated Multiscale Method for the Characterisation of Active Faults in Offshore Areas. The Case of Sant’Eufemia Gulf (Offshore Calabria, Italy)

2021

Diagnostic morphological features (e.g., rectilinear seafloor scarps) and lateral offsets of the Upper Quaternary deposits are used to infer active faults in offshore areas. Although they deform a significant seafloor region, the active faults are not necessarily capable of producing large earthquakes as they correspond to shallow structures formed in response to local stresses. We present a multiscale approach to reconstruct the structural pattern in offshore areas and distinguish between shallow, non-seismogenic, active faults, and deep blind faults, potentially associated with large seismic moment release. The approach is based on the interpretation of marine seismic reflection data and …

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaScienceSettore GEO/03 - Geologia StrutturaleInversion (geology)Active faultSlab-tear faultLate MioceneCalabrian arc (Italy)010502 geochemistry & geophysicsFault scarp01 natural sciencesPaleontologymorphotectonic analysiMorphotectonic analysisHigh-resolution seismic dataBathymetry0105 earth and related environmental sciencesActive tectonicsactive tectonicQAnticlineSeafloor spreadingTectonicsGeneral Earth and Planetary SciencesGeologySouthern tyrrhenian sea
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The Graham Bank (Sicily Channel, central Mediterranean Sea). Seafloor signatures of volcanic and tectonic controls

2018

Abstract Graham Bank is a dominant physiographic element of the NW Sicily Channel (central Mediterranean Sea), affected in the last 100 years by numerous well-documented volcanic eruptions. We present the first results of a geomorphological study where the Graham Bank region in the depth interval 7–350 m was mapped for the first time with multi-beam echosounder and high-resolution seismic and multi-channel seismic reflection profiles. We describe in high resolution the detailed geomorphological features of Graham Bank, and how the superficial expression of different process and dynamics occurring in the sub-seafloor evidence volcanic and tectonic controls on seafloor morphology across a rel…

010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSeamount010502 geochemistry & geophysics01 natural sciencesFluid seepagePaleontologyMediterranean seaEcho soundingSlope instability14. Life underwater0105 earth and related environmental sciencesEarth-Surface ProcessesgeographyFluid seepage; Graham Bank; Slope instability; Volcanic seamountgeography.geographical_feature_categoryVolcanic seamountFluid seepage Slope instability Volcanic seamount Graham BankGraham BankSeafloor spreadingTectonicsVolcanoSedimentary rockChannel (geography)Geology
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How Offshore Groundwater Shapes the Seafloor

2018

The MARCAN project, launched last January, is working to fill a gap in our knowledge of how freshwater flowing underground shapes and alters the continental margins.

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologia010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingOceanographyContinental margin13. Climate actioncontinental marginGeneral Earth and Planetary SciencesSubmarine pipelineGroundwaterGroundwaterGeology0105 earth and related environmental sciencesEos
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Historical analysis of rainfall-triggered rockfalls: the case study of the disaster of the ancient hydrothermal Sclafani Spa (Madonie Mts, northern-c…

2017

Abstract. In 1851, the region of Sicily experienced many rainstorm-induced landslides. On 13 March 1851, a rainstorm brought about a severe rockfall disaster near the small town of Sclafani (Madonie Mountains, northern-central Sicily, Italy). Rocks detached from the carbonate crest of Mt Sclafani (813 m above sea level) and fell downslope, causing the collapse of the ancient hydrothermal spa (about 430 m above sea level) and burying it. Fortunately, there were no injuries or victims. Given its geological, geomorphological and tectonic features, the calcareous–dolomitic and carbonate–siliciclastic relief of Mt Sclafani is extremely prone to landsliding. This study combines the findings of de…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaClimate change010502 geochemistry & geophysics01 natural scienceslcsh:TD1-1066Extreme weatherRockfalllcsh:Environmental technology. Sanitary engineeringNatural disasterlcsh:Environmental sciencesSea level0105 earth and related environmental scienceslcsh:GE1-350geographygeography.geographical_feature_categorylcsh:QE1-996.5Global warminglcsh:Geography. Anthropology. RecreationLandslideLandslide rainfall rockfall thermal spring Sicilylcsh:GeologyTectonicslcsh:GGeneral Earth and Planetary SciencesPhysical geographyGeologyNatural Hazards and Earth System Sciences
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Disambiguating the soils of Mars

2020

Abstract Anticipated human missions to Mars require a methodical understanding of the unconsolidated bulk sediment that mantles its surface, given its role as an accessible resource for water and as a probable substrate for food production. However, classifying martian sediment as soil has been pursued in an ad hoc fashion, despite emerging evidence from in situ missions for current and paleo-pedological processes. Here we find that in situ sediment at Gusev, Meridiani and Gale are consistent with pedogenesis related to comminuted basalts mixing with older phyllosilicates – perhaps of pluvial origin – and sulfates. Furthermore, a notable presence of hydrated amorphous phases indicates signi…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceWeatheringMartian soilRegolith01 natural sciences0103 physical sciencesWorld Reference Base for Soil ResourcesCryosol010303 astronomy & astrophysics0105 earth and related environmental sciencesUSDA soil taxonomyMartianSoil TaxonomyGelisolAstronomy and AstrophysicsSoil classificationMineral weatheringPedogenesisSettore AGR/14 - PedologiaSpace and Planetary ScienceSoil waterEnvironmental scienceWRBSettore M-GGR/01 - GeografiaPlanetary and Space Science
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Geomorphological evolution of western Sicily, Italy

2017

Abstract This paper proposes a morphoevolutionary model for western Sicily. Sicily is a chain–foredeep–foreland system still being built, with tectonic activity involving uplift which tends to create new relief. To reconstruct the morphoevolutionary model, geological, and geomorphological studies were done on the basis of field survey and aerial photographic interpretation. The collected data show large areas characterized by specific geological, geomorphological, and topographical settings with rocks, landforms, and landscapes progressively older from south to north Sicily. The achieved results display: (1) gradual emersion of new areas due to uplift, its interaction with the Quaternary gl…

010504 meteorology & atmospheric sciencesSettore GEO/04 - Geografia Fisica E Geomorfologialcsh:QE1-996.5GeologySicily geomorphological evolution Quaternary uplift extensional tectonics down-cutting processes differential erosion.010502 geochemistry & geophysicsextensional tectonics01 natural sciencesdown-cutting processesQuaternarylcsh:GeologyPaleontologyupliftExtensional tectonicsdifferentialerosionQuaternarySicilyGeologygeomorphological evolution0105 earth and related environmental sciences
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