Search results for "Sal"

showing 10 items of 15931 documents

Secondary minerals from salt caves in the Atacama Desert (Chile): a hyperarid and hypersaline environment with potential analogies to the Martian sub…

2017

Over the past 15 years several expeditions by French, American and especially Italian cavers have unveiled over 50 caves in the Cordillera de la Sal (Atacama Desert, Northern Chile). Many of these caves contain a variety of speleothems and minerals, some of which have rarely been observed within karst systems. Most of the secondary deposits in these caves are composed of halite, but also other halide, carbonate, sulphate, nitrate, phosphate, and silicate minerals have been found. Among the sixteen cave mineral species recognized, atacamite, darapskite, blödite, leonite, anhydrite, and especially antarcticite are worth mentioning. In one of the samples an unknown Ca-Sr-bearing chloride miner…

010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaEarth scienceSalt (chemistry)martian010502 geochemistry & geophysics01 natural sciencesAstrobiologyatacamaCaveminerogenesisMinerogenesiBiology (General)Hyperaridity0105 earth and related environmental sciencesEarth-Surface Processescave mineralschemistry.chemical_classificationMartianQE1-996.5Settore GEO/06 - Mineralogiageographygeography.geographical_feature_categoryDesert (philosophy)Mars analoguesMars analogueCave mineralGeologysalt cavescave minerals atacama martianchemistrySalt cavecave minerals salt caves hyperaridity minerogenesis Mars analoguesGeologyInternational Journal of Speleology
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Late Quaternary Variations in the South American Monsoon System as Inferred by Speleothems—New Perspectives using the SISAL Database

2019

Here we present an overview of speleothem δ18O records from South America, most of which are available in the Speleothem Isotopes Synthesis and Analysis (SISAL_v1) database. South American tropical and subtropical speleothem δ18O time series are primarily interpreted to reflect changes in precipitation amount, the amount effect, and consequently history of convection intensity variability of convergence zones such as the Intertropical Convergence Zone (ITCZ) and the South America Monsoon System (SAMS). We investigate past hydroclimate scenarios in South America related to the South American Monsoon System in three different time periods: Late Pleistocene, Holocene, and the last tw…

010504 meteorology & atmospheric sciencesSAMSSpeleothemlcsh:GN281-289SubtropicsSouth American Monsoon System010502 geochemistry & geophysicscomputer.software_genreMonsoon01 natural scienceslcsh:StratigraphyEarth and Planetary Sciences (miscellaneous)PrecipitationSISALHolocenelcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesgeographyquaternarygeography.geographical_feature_categoryDatabasespeleothemsIntertropical Convergence ZoneMUDANÇA CLIMÁTICAlcsh:Human evolutionSouth Atlantic Convergence ZoneQuaternarycomputerGeologyQuaternary
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Scale: The Universal Laws of Growth, Innovation, Sustainability, and the Pace of Life in Organisms, Cities, Economies, and Companies

2020

National audience

010504 meteorology & atmospheric sciencesScale (ratio)Geography Planning and Development0211 other engineering and technologies021107 urban & regional planning02 engineering and technologyUniversal law01 natural sciences[SDE]Environmental Sciences11. SustainabilitySustainabilityEconomic geographyBusinessComputingMilieux_MISCELLANEOUSPace of life0105 earth and related environmental sciencesPlanning Theory
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Applying the USLE Family of Models at the Sparacia (South Italy) Experimental Site

2016

Soil erosion is a key process to understand the land degradation, and modelling of soil erosion will help to understand the process and to foresee its impacts. The applicability of the Universal Soil Loss Equation (USLE) at event scale is affected by the fact that USLE rainfall erosivity factor does not take into account runoff explicitly. USLE-M and USLE-MM, including the effect of runoff in the event rainfall– runoff erosivity factor, are characterized by a better capacity to predict event soil loss. The specific objectives of this paper were (i) to determine the suitable parameterization of USLE, USLE-M and USLE-MM by using the dataseries of Sparacia experimental site and (ii) to evaluat…

010504 meteorology & atmospheric sciencesScale (ratio)Soil ScienceSoil scienceDevelopment01 natural sciencesDeposition (geology)Soil lossplot soil loUSLE-MMSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-ForestaliEnvironmental Chemistry0105 earth and related environmental sciencesGeneral Environmental ScienceEvent (probability theory)Hydrologysoil erosionSediment04 agricultural and veterinary sciencesUniversal Soil Loss Equation040103 agronomy & agricultureLand degradationUSLE-M0401 agriculture forestry and fisheriesEnvironmental scienceSurface runoffEvent scaleLand Degradation & Development
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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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Predicting plot soil loss by empirical and process-oriented approaches. A review

2018

Soil erosion directly affects the quality of the soil, its agricultural productivity and its biological diversity. Many mathematical models have been developed to estimate plot soil erosion at different temporal scales. At present, empirical soil loss equations and process-oriented models are considered as constituting a complementary suite of models to be chosen to meet the specific user need. In this paper, the Universal Soil Loss Equation and its revised versions are first reviewed. Selected methodologies developed to estimate the factors of the model with the aim to improve the soil loss estimate are described. Then the Water Erosion Prediction Project which represents a process-oriente…

010504 meteorology & atmospheric sciencesSoil erosion; Soil loss measurements; Universal soil loss equation; Water erosion prediction project; Bioengineering; Mechanical Engineering; Industrial and Manufacturing EngineeringBioengineeringSoil science01 natural sciencesIndustrial and Manufacturing EngineeringPlot (graphics)lcsh:Agriculturewater erosion prediction project.Soil loss measurementSettore AGR/08 - Idraulica Agraria E Sistemazioni Idraulico-Forestalilcsh:Agriculture (General)Temporal scalesReliability (statistics)0105 earth and related environmental sciencesgeographysoil loss measurementsgeography.geographical_feature_categoryPhysical modelMathematical modelMechanical EngineeringWater erosion prediction projectlcsh:S04 agricultural and veterinary sciencesUniversal Soil Loss Equationlcsh:S1-972RillUniversal Soil Loss EquationSoil erosion040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSpatial variability
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The geological roots of South America: 4.1 Ga and 3.7 Ga zircon crystals discovered in N.E. Brazil and N.W. Argentina

2015

International audience; We present new LA-ICP-MS in situ geochronological results for seven Eoarchean zircons dated at 3.7 Ga coming from Cretaceous ash layers of NW Argentina and one Hadean single crystal sampled within the São Francisco Craton in NE Brazil. This zircon comprises a zoned magmatic core dated at 4.1 Ga surrounded by a 1.9 Ga overgrowth related to Paleoproterozoic reworking. This Hadean age is consistent with previously published Nd model ages on orthogneisses from the same domain. These two results represent among the oldest geological witnesses discovered to date in South America, which demonstrates the occurrence of a primitive crust. The contrasting age patterns recorded …

010504 meteorology & atmospheric sciencesU–Pb zircon datingLaser ablation ICP-MSHadeanGeochemistryAge patternsGeologyCrustHadean010502 geochemistry & geophysics[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry01 natural sciencesCretaceousSao Francisco Craton BrazilSalta rift ArgentinaGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryPrimitive crustSão Francisco CratonGeology0105 earth and related environmental sciencesZircon
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Soil erosion processes in European vineyards: A qualitative comparison of rainfall simulation measurements in Germany, Spain and France

2016

Small portable rainfall simulators are considered a useful tool to analyze soil erosion processes in cultivated lands. European research groups in Spain (Valencia, Málaga, Lleida, Madrid and La Rioja), France (Reims) and Germany (Trier) have used different rainfall simulators (varying in drop size distribution and fall velocities, kinetic energy, plot forms and sizes, and field of application) to study soil loss, surface flow, runoff and infiltration coefficients in different experimental plots (Valencia, Montes de Málaga, Penedès, Campo Real and La Rioja in Spain, Champagne in France and Mosel-Ruwer valley in Germany). The measurements and experiments developed by these research teams give…

010504 meteorology & atmospheric sciencesWater en Landgebruiksoil hydrologyOceanography01 natural sciencesRUISSELLEMENTSoilvineyardsBodemSoil Water and Land UseQualitative comparisonlcsh:ScienceWaste Management and DisposalWater Science and Technology2. Zero hungerSoil classification04 agricultural and veterinary sciencesqualitative comparisonPE&RCInfiltration (hydrology)INFILTRATIONERODIBILITE DU SOLPRECIPITATIONErosionWEPPSIMULATION DE PLUIESoil hydrologyEAU DU SOLSoil scienceVIGNESoil lossETUDE COMPARATIVE[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology0105 earth and related environmental sciencesEarth-Surface ProcessesTerroirHydrologysoil erosionWater and Land UseTERRE CULTIVABLEECOULEMENT DE SURFACErainfall simulation15. Life on landBodemfysica en LandbeheerVineyardsRainfall simulationBodem Water en LandgebruikSoil Physics and Land Managementrainfall simulation; soil erosion; soil hydrology; qualitative comparison; vineyardsrainfall simulation soil erosion soil hydrology qualitative comparison vineyards040103 agronomy & agricultureRainfall simulationSoil erosion0401 agriculture forestry and fisheriesEnvironmental sciencelcsh:QSurface runoffMETHODOLOGIE
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The Early-Cambrian Boho volcano of the El Graara massif, Morocco: Petrology, geodynamic setting and coeval sedimentation

2006

15 pages; International audience; A major volcanic episode is recorded across the Neoproterozoic-Cambrian transition in the Moroccan Anti-Atlas. Several volcanic cones are still preserved in the El Graara massif, laterally correlatable with volcanic flows dated as Early Cambrian (U/Pb date of 534 ± 10 Ma). Volcanic ashes and flows are interbedded with the uppermost part of the Adoudou dolostones, whereas the best-preserved volcano (the Boho Jbel) is onlapped by the overlying Lie-de-vin strata. Available petro-geochemical data from the Boho volcano suggest an alkaline magmatism probably derived from low-grade melting of a garnet–lherzolite mantle source, followed by fractional crystallizatio…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesGeochemistrySlope apron[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/Volcanology010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphySyenites01 natural sciencesDiagenesisLower CambrianBreccia[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyAlkaline basaltsPetrologySlope aponComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyBasaltgeographygeography.geographical_feature_categoryTerrigenous sedimentGeologyMassifDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangesMoroccoVolcano13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphySubaerial[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyVolcanic coneGeology
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Chlorine Partitioning Between a Basaltic Melt and H2O-CO2 Fluids at Mount Etna

2009

Partitioning experiments between a basaltic melt from Mt. Etna and a low-density hydrous fluid or vapor containing H(2)O or H(2)O-CO(2) were performed at 1200-1260 degrees C, at pressures between 1 and 200 MPa, either near the nickel-nickel oxide (NNO) buffer or at two log units above it (NNO + 2), and with different chloride concentrations. Most of the experiments were done at chloride-brine-undersaturated conditions, although at the highest Cl concentrations explored brine saturation might have been reached. The average partition coefficients (D(Cl)(fluid/melt)) over the range of Cl concentrations were derived on a weight basis by plotting the calculated concentrations of Cl in the fluid …

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesOxideAnalytical chemistrychemistry.chemical_elementMineralogyBasaltic melt010502 geochemistry & geophysics01 natural sciencesChloridechemistry.chemical_compoundGeochemistry and PetrologyCl solubilityChlorinemedicine[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyFugacity0105 earth and related environmental sciencesBasalthalogen degassingGeologySilicateSettore GEO/08 - Geochimica E VulcanologiaPartition coefficientBrinechemistry13. Climate actionFluid/melt partitioningMount EtnaChlorineGeologymedicine.drug
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