Search results for "Planet"

showing 10 items of 5662 documents

Impact of acidic volcanic emissions on ash leaching and on the bioavailability and mobility of trace metals in soils of Mt Etna

2021

We report on original geochemical data, which combine the rainfall trace metal contents from three different areas of Mt. Etna, variably fumigated by the volcanic plume, and those from soils, collected over the whole volcano. Trace element contents in rainfall appear mostly related to acidic ash leaching, while only for the most volatile elements (Cu, Zn, Cd, Pb, As, Sb, Tl, Se) we suggest a derivation from magmatic degassing. We analyzed separately the labile fraction of soil samples, considered the fraction bioavailable to plants and soil organisms living in. The complexing medium used to extract the bioavailable fraction simulates the growth environment of plant roots.The contents of tra…

Soil testTrace elementGeologySoil carbon010502 geochemistry & geophysics01 natural sciencesSoil pHEnvironmental chemistrySoil waterGeneral Earth and Planetary SciencesEnvironmental scienceTrace metalLeaching (metallurgy)Mt. Etna Rainwater Soil Trace elementsVolatiles0105 earth and related environmental sciences
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Wildland fire ash: Production, composition and eco-hydro-geomorphic effects

2014

Abstract: Fire transforms fuels (i.e. biomass, necromass, soil organic matter) into materials with different chemical and physical properties. One of these materials is ash, which is the particulate residue remaining or deposited on the ground that consists of mineral materials and charred organic components. The quantity and characteristics of ash produced during a wildland fire depend mainly on (1) the total burned fuel (i.e. fuel load), (2) fuel type and (3) its combustion completeness. For a given fuel load and type, a higher combustion completeness will reduce the ash organic carbon content, increasing the relative mineral content, and hence reducing total mass of ash produced. The hom…

Soil texturePhysicsSoil organic matterSoil scienceSoil typeHydraulic conductivitySoil pHEnvironmental chemistryGeneral Earth and Planetary SciencesEnvironmental scienceSoil horizonWater qualitySurface runoffBiology
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OSSOS. IX. Two objects in Neptune's 9:1 resonance: implications for resonance sticking in the scattering population

2018

We discuss the detection in the Outer Solar System Origins Survey (OSSOS) of two objects in Neptune's distant 9:1 mean motion resonance at semimajor axis $a\approx~130$~au. Both objects are securely resonant on 10~Myr timescales, with one securely in the 9:1 resonance's leading asymmetric libration island and the other in either the symmetric or trailing asymmetric island. These objects are the largest semimajor axis objects with secure resonant classifications, and their detection in a carefully characterized survey allows for the first robust resonance population estimate beyond 100~au. The detection of these objects implies a 9:1 resonance population of $1.1\times10^4$ objects with $H_r&…

Solar System010504 meteorology & atmospheric sciencesPopulationFOS: Physical sciencesSpace (mathematics)01 natural sciencesResonance (particle physics)Neptune0103 physical sciences/dk/atira/pure/subjectarea/asjc/1900/1912education010303 astronomy & astrophysicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesPhysicsEarth and Planetary Astrophysics (astro-ph.EP)education.field_of_studyScatteringAstronomygeneral [Kuiper belt]Astronomy and AstrophysicsSpace and Planetary Science/dk/atira/pure/subjectarea/asjc/3100/3103Astrophysics::Earth and Planetary Astrophysics[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]Astrophysics - Earth and Planetary Astrophysics
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Mean Interplanetary Magnetic Field Measurement Using the ARGO-YBJ Experiment

2011

The sun blocks cosmic ray particles from outside the solar system, forming a detectable shadow in the sky map of cosmic rays detected by the ARGO-YBJ experiment in Tibet. Because the cosmic ray particles are positive charged, the magnetic field between the sun and the earth deflects them from straight trajectories and results in a shift of the shadow from the true location of the sun. Here we show that the shift measures the intensity of the field which is transported by the solar wind from the sun to the earth.

Solar SystemField (physics)media_common.quotation_subjectAstrophysics::High Energy Astrophysical PhenomenaFOS: Physical sciencesmagnetic fieldCosmic rayHigh Energy Physics - ExperimentHigh Energy Physics - Experiment (hep-ex)Settore FIS/05 - Astronomia E AstrofisicaShadowAstrophysics::Solar and Stellar AstrophysicsInterplanetary magnetic fieldcosmic raySolar and Stellar Astrophysics (astro-ph.SR)media_commonPhysicsHigh Energy Astrophysical Phenomena (astro-ph.HE)Settore FIS/01 - Fisica SperimentaleAstrophysics::Instrumentation and Methods for AstrophysicsAstronomyAstronomy and AstrophysicsCosmic Rays Gamma Sources Extended Air Showers Solar windMagnetic fieldSolar windAstrophysics - Solar and Stellar Astrophysicssolar windSpace and Planetary ScienceSkyPhysics::Space PhysicsAstrophysics::Earth and Planetary AstrophysicsAstrophysics - High Energy Astrophysical Phenomena
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Are high-temperature fractionations in the solar nebula preserved in highly siderophile element systematics of the Earth's mantle?

2004

The relative abundances of the highly siderophile elements (HSE) Os, Ir, Ru, Pt, Rh, and Pd in relatively pristine lherzolites differ from solar abundance ratios and are several orders of magnitude higher than predicted for equilibrium distribution between metal/silicate (core-mantle). The samples are characterized by a mean Ca/Al ratio of 1.18 ± 0.09 σM and a mean Ca/Si ratio of 0.10 ± 0.01 σM, overlapping with a mean Ca/Al of 1.069 ±  0.044 σM and a mean Ca/Si of 0.081 ± 0.023 σM found in chondrites (Wasson and Kallemeyn 1988). Interestingly, the CI-normalized abundance pattern shows decreasing solar system normalized abundances with increasing condensation temperatures. The abundance of …

Solar SystemGeochemistryAnalytical chemistryengineering.materialSilicatechemistry.chemical_compoundGeophysicschemistrySpace and Planetary ScienceAbundance (ecology)ChondriteEnstatiteengineeringFormation and evolution of the Solar SystemGeologyEarth (classical element)Refractory (planetary science)Meteoritics & Planetary Science
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Water and Geodynamics

2006

Hydrogen is the most abundant element (Fig. 1⇓) in the galaxy and our solar system (Lodders 2003). Therefore it is not astonishing that hydrogen is a key player in the geodynamic evolution of planets. Its fate in the early Earth, after condensation of the solar nebula, the accretion of our planet and hydrogen reprocessing through early asteroidal and cometary bombardment (Dauphas et al. 2000) and segregation of a proto-Earth into iron core and silicate mantle is described elsewhere in this volume (Marty and Yokochi 2006). Figure 1. Abundance of elements in the solar system in numbers of atoms per 106 atoms of silicon (Lodders 2003). This chapter concerns itself with the geodynamics of the m…

Solar SystemHydrogenchemistryGeochemistry and PetrologyPlanetchemistry.chemical_elementGeodynamicsFormation and evolution of the Solar SystemEarly EarthGeologyMantle (geology)Abundance of the chemical elementsAstrobiologyReviews in Mineralogy and Geochemistry
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The Search Starts

2010

The previous chapter has shown us that life on Earth arose surprisingly fast and easy, as soon as the conditions were right for liquid water to be sustained on the surface. We saw that there is evidence of the presence of this valuable substance in at least two other bodies in the Solar System, and these are encouraging indications that life in the Solar System might not be limited to Earth. Also, we saw that planetary systems are not rarities of nature but seem to abound across the universe, and that life is much more resistant than was once believed, which extends the limits of what can be considered a habitable world. All these facts, despite our own ignorance about many things, make num…

Solar SystemLiquid watermedia_common.quotation_subjectIgnoranceEarth (chemistry)Planetary systemGalaxyGeologymedia_commonAstrobiology
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Looking for the origin of life in cosmochemistry : asteroids and their carbon-rich meteorites

2015

Carbonaceous chondrite meteorites are carbon-containing fragments of primitive asteroids that have offered the only samples available to date giving insights into chemical evolution in laboratory analyses. Their study has revealed that abundant organic chemistry came to be in the Solar System ahead of terrestrial life and, by the input of these meteorites and comets, might have aided in the origin of our planet’s biochemistry.

Solar SystemMultidisciplinarychemistry.chemical_elementAstrobiologyCosmochemistryHistory and Philosophy of SciencechemistryMeteoriteAsteroidPlanetAbiogenesisCarbonaceous chondriteCarbonGeology
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Small solar system bodies as granular systems

2017

Asteroids and other Small Solar System Bodies (SSSBs) are currently of great scientific and even industrial interest. Asteroids exist as the permanent record of the formation of the Solar System and therefore hold many clues to its understanding as a whole, as well as insights into the formation of planetary bodies. Additionally, SSSBs are being investigated in the context of impact risks for the Earth, space situational awareness and their possible industrial exploitation (asteroid mining). In all these aspects, the knowledge of the geophysical characteristics of SSSB surface and internal structure are of great importance. Given their size, constitution, and the evidence that many SSSBs ar…

Solar SystemSituation awareness[PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]Computer sciencePhysicsQC1-999Small solar system bodiesContext (language use)Granular systems01 natural sciencesCelestial mechanicsAstrobiologyTheoretical physics13. Climate actionAsteroidFísica Aplicada0103 physical sciencesFormation and evolution of the Solar System[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]010306 general physics010303 astronomy & astrophysicsComputingMilieux_MISCELLANEOUSSoil mechanicsAsteroid miningEPJ Web of Conferences
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The polarimetric and helioseismic imager on solar orbiter

2020

This paper describes the Polarimetric and Helioseismic Imager on the Solar Orbiter mission (SO/PHI), the first magnetograph and helioseismology instrument to observe the Sun from outside the Sun-Earth line. It is the key instrument meant to address the top-level science question: How does the solar dynamo work and drive connections between the Sun and the heliosphere? SO/PHI will also play an important role in answering the other top-level science questions of Solar Orbiter, as well as hosting the potential of a rich return in further science. SO/PHI measures the Zeeman effect and the Doppler shift in the FeI 617.3nm spectral line. To this end, the instrument carries out narrow-band imaging…

Solar Telescope010504 meteorology & atmospheric sciencesphotosphere [Sun]FiltegramsHighly elliptical orbitFOS: Physical sciencesAstrophysics01 natural scienceslaw.inventionTelescopeOrbiterPhotospherelaw0103 physical sciencesAstrophysics::Solar and Stellar AstrophysicsHelioseismologySolar dynamo010303 astronomy & astrophysicsSun: magnetic fieldsInstrumentation and Methods for Astrophysics (astro-ph.IM)0105 earth and related environmental sciencesSun: helioseismologyPhysics[PHYS]Physics [physics]PhotosphereEllipsometrypolarimeters [Instrumentation]Spacecraftbusiness.industryAstrophysics::Instrumentation and Methods for AstrophysicsAstronomyinstrumentation: polarimetersSun: photosphereHeliosismologiaAstronomy and AstrophysicsAstrophysics - Astrophysics of Galaxiestechniques: polarimetricmagnetic fields [Sun]Space and Planetary Sciencetechniques: imaging spectroscopyAstrophysics of Galaxies (astro-ph.GA)Physics::Space PhysicsHelioseismologyAstrophysics::Earth and Planetary AstrophysicsbusinessAstrophysics - Instrumentation and Methods for Astrophysics[PHYS.ASTR]Physics [physics]/Astrophysics [astro-ph]HeliosphereEl·lipsometria
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