Search results for "mass [target]"

showing 10 items of 514 documents

Proton decay of 108I and its significance for the termination of the astrophysical rp-process

2019

Abstract Employing the Argonne Fragment Mass Analyzer and the implantation-decay-decay correlation technique, a weak 0.50(21)% proton decay branch was identified in 108I for the first time. The 108I proton-decay width is consistent with a hindered l = 2 emission, suggesting a d 5 2 origin. Using the extracted 108I proton-decay Q value of 597(13) keV, and the Q α values of the 108I and 107Te isotopes, a proton-decay Q value of 510(20) keV for 104Sb was deduced. Similarly to the 112,113Cs proton-emitter pair, the Q p ( I 108 ) value is lower than that for the less-exotic neighbor 109I, possibly due to enhanced proton-neutron interactions in N ≈ Z nuclei. In contrast, the present Q p ( Sb 104 …

Nuclear and High Energy Physicsalpha decayProton decayQ valueastrofysiikkaNuclear Theory104Sb01 natural sciencesastrophysical rp process108I0103 physical sciencesMass analyzer107Te010306 general physicsNuclear ExperimentPhysicsIsotopeta114010308 nuclear & particles physicsInteraction energyrp-processlcsh:QC1-999proton decayHigh Energy Physics::ExperimentAtomic physicsydinfysiikkalcsh:PhysicsPhysics Letters B
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Selective ultra trace isotope determination in environmental and biomedical studies by high-resolution resonance ionization mass spectrometry

2002

The precise determination of relative abundances of ultra trace isotopes in the range below 10 -9 is of importance for a wide spectrum of applications in fields like environmental protection, cosmo-chemistry, bio-medical tracer studies or geological and geo-chronological investigations. The necessary high isotopic selectivity, rather complete isobaric suppression and good overall efficiency for these investigations is provided by high-resolution resonance ionization mass spectrometry. Multi-step continuous wave laser excitation and ionization using diode lasers at a compact quadrupole mass spectrometer has been optimized to become a powerful and reliable experimental method, which is just b…

Nuclear magnetic resonanceSpectrometerIsotopelawIonizationAnalytical chemistryPhysics::Atomic PhysicsThermal ionization mass spectrometryMass spectrometryLaserQuadrupole mass analyzerAccelerator mass spectrometrylaw.inventionSPIE Proceedings
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Direct mass measurements above uranium bridge the gap to the island of stability

2010

The mass of an atom incorporates all its constituents and their interactions. The difference between the mass of an atom and the sum of its building blocks (the binding energy) is a manifestation of Einstein's famous relation E = mc(2). The binding energy determines the energy available for nuclear reactions and decays (and thus the creation of elements by stellar nucleosynthesis), and holds the key to the fundamental question of how heavy the elements can be. Superheavy elements have been observed in challenging production experiments, but our present knowledge of the binding energy of these nuclides is based only on the detection of their decay products. The reconstruction from extended d…

Nuclear physicsMass numberMultidisciplinaryMass excessAtomic mass constantIsotopeChemistryNuclideAtomic physicsNuclear ExperimentAtomic massBeta-decay stable isobarsSpontaneous fission
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Study of excited states of [sup 31]S through beta-decay of [sup 31]Cl for nucleosynthesis in ONe novae

2011

We have produced an intense and pure beam of 31Cl with the MARS Separator at the Texas A&M University and studied β‐decay of 31Cl by implanting the beam into a novel detector setup, capable of measuring β‐delayed protons and γ‐rays simultaneously. From our data, we have established decay scheme of 31Cl, found resonance energies with 1 keV precision, have measured its half‐life with under 1% accuracy, found its Isobar Analog State decay and by using the IMME obtained an improved mass excess for its ground state. In this contribution, a description of the used method along with selected preliminary experimental results are given and their relevance for novae nucleosynthesis discussed.

Nuclear physicsPhysicsDecay schemeMass excessta114NucleosynthesisExcited stateIsobarResonanceAtomic physicsGround stateBeta decayAIP Conference Proceedings
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The new neutron-rich isotope228Rn

1989

2 pages, 1 table, 2 figures.-- PACS nrs.: 23.90.+w; 27.90.+b.-- Section: Short Notes.

Nuclear physicsPhysicsNuclear and High Energy PhysicsIsotopeNuclear fusionNeutronSpallation[PACS] Other topics in radioactive decay and in-beam spectroscopy[PACS] Properties of specific nuclei listed by mass ranges: A ≥ 220SpectroscopyA ≥ 220 [[PACS] Properties of specific nuclei listed by mass ranges]Zeitschrift f�r Physik A Atomic Nuclei
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Manifestation of fine structures in the fission fragment mass-energy distribution of the reaction

2002

Methods of identifying structure peculiarities in two-dimensional distributions of experimental observables are discussed. Structures different from that produced by proton odd-even staggering were revealed for the first time in the mass-energy distribution of fission fragments in the 233 Uðnth; fÞ reaction. The new structures could presumably be linked with fission modes and collective vibrations of the fissioning system. r 2002 Elsevier Science B.V. All rights reserved.

Nuclear physicsPhysicsNuclear and High Energy PhysicsMass energyDistribution (mathematics)ProtonFragment (logic)FissionObservableNuclear ExperimentInstrumentationNuclear Instruments and Methods in Physics Research Section A: Accelerators, Spectrometers, Detectors and Associated Equipment
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Variable masses in fission and heavy-ion collisions

1972

With the use of the cranking formula, the coordinate-dependent mass parameters of the kinetic-energy operator in fission processes and heavy-ion collisions are calculated in the two-center oscillator model. It is shown that the reduced mass and also the classical moment of inertia are obtained for large separations of the fragments. For small separations, however, the mass parameter for the motion of the centers of mass of the fragments is larger than the reduced mass by an order of magnitude.

Nuclear reactionPhysicsMass excessFissionOperator (physics)General Physics and AstronomyReduced massMoment of inertiaKinetic energyUranium-236Nuclear physicsddc:530Atomic physicsNuclear Experiment
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A method for the calculation of the heat transfer coefficient in potato drying

1993

A method for the determination of the heat transfer coefficient was proposed for the first falling drying period of potato cubes. During this period, heat and mass transfer were considered as coupled phenomena. Temperature calculation inside the sample was performed using the macroscopic heat transfer balance. The heat transfer coefficient was computed by means of parametric identification, using the Gauss–Newton method. The figure obtained for the heat transfer coefficient shows good agreement with other sources.

Nutrition and DieteticsNTU methodChemistryMass transferHeat transferFilm temperatureHeat transfer coefficientMechanicsParametric identificationAgronomy and Crop ScienceChurchill–Bernstein equationFood ScienceBiotechnologyJournal of the Science of Food and Agriculture
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Seawater carbonate chemistry and biogenic habitat shifts under long-term ocean acidification

2023

Experiments have shown that increasing dissolved CO2 concentrations (i.e. Ocean Acidification, OA) in marine ecosystems may act as nutrient for primary producers (e.g. fleshy algae) or a stressor for calcifying species (e.g., coralline algae, corals, molluscs). For the first time, rapid habitat dominance shifts and altered competitive replacement from a reef-forming to a non-reef-forming biogenic habitat were documented over one-year exposure to low pH/high CO2 through a transplant experiment off Vulcano Island CO2 seeps (NE Sicily, Italy). Ocean acidification decreased vermetid reefs complexity via a reduction in the reef-building species density, boosted canopy macroalgae and led to chang…

Ocean Acidification International Coordination Centre (OA-ICC)IdentificationSalinityTemperateCommunity composition and diversityinorganicAlkalinityDensityType of studyExperimentTemperature waterCarbon inorganic dissolvedAbundanceCalculated using seacarb after Nisumaa et al 2010Aragonite saturation stateAlkalinity totalSalinity standard errortotalCO2 ventpHTemperaturePartial pressure of carbon dioxide (water) at sea surface temperature (wet air) standard errordissolvedCarbonate ionPartial pressure of carbon dioxide (water) at sea surface temperature (wet air)Field experimentstandard errorEarth System ResearchPotentiometric titrationCalcite saturation stateCoveragePotentiometricwaterSiteRocky-shore communityAlkalinity total standard errorBenthosReplicateMediterranean SeaOcean Acidification International Coordination Centre OA ICCBicarbonate ionTemperature water standard errorCalculated using seacarb after Nisumaa et al. (2010)pH standard errorCalculated using CO2SYSCarbonate system computation flagComplexityFugacity of carbon dioxide (water) at sea surface temperature (wet air)CarbonBiomass/Abundance/Elemental compositionAragonite saturation state standard errorPartial pressure of carbon dioxide water at sea surface temperature wet airCarbon dioxideEntire communityRocky shore communityFugacity of carbon dioxide water at sea surface temperature wet airBiomass Abundance Elemental compositionCoast and continental shelfSpecies richness
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Seaweed fails to prevent ocean acidification impact on foraminifera along a shallow-water CO2 gradient

2015

Ocean acidification causes biodiversity loss, alters ecosystems, and may impact food security, as shells of small organisms dissolve easily in corrosive waters. There is a suggestion that photosynthetic organisms could mitigate ocean acidification on a local scale, through seagrass protection or seaweed cultivation, as net ecosystem organic production raises the saturation state of calcium carbonate making seawater less corrosive. Here, we used a natural gradient in calcium carbonate saturation, caused by shallow-water CO2 seeps in the Mediterranean Sea, to assess whether seaweed that is resistant to acidification (Padina pavonica) could prevent adverse effects of acidification on epiphytic…

Ocean Acidification International Coordination Centre (OA-ICC)TemperateIdentificationSalinityCommunity composition and diversityTriloculinella dilatatainorganicAlkalinityElphidium spMiliolinella sp.Miliolinella subrotundaQuinqueloculina sp.Daitrona spTemperature waterCarbon inorganic dissolvedCalculated using seacarb after Nisumaa et al 2010Adelosina longirostraPercentageAragonite saturation stateMiliolinella spRosalina globularisAlkalinity totaltotalElphidium sp.Elphidium crispumCO2 ventElphidium advenumpHTemperaturedissolvedPseudotriloculina spCarbonate ionPartial pressure of carbon dioxide (water) at sea surface temperature (wet air)Rosalina spQuinqueloculina annectensEarth System ResearchHaynesina depressulaField observationElphidium margaritaceumPotentiometric titrationCalcite saturation statePotentiometricwaterMassilina gualtierianaRocky-shore communitySpiroloculina ornataQuinqueloculina auberianaBenthosDaitrona sp.Pileolina patelliformisOcean Acidification International Coordination Centre OA ICCMediterranean SeaBicarbonate ionCalculated using seacarb after Nisumaa et al. (2010)SpeciesVertebralina striataAffinetrina gualtierianaElphidium macellumCalculated using CO2SYSIndividualsCarbonate system computation flagFugacity of carbon dioxide (water) at sea surface temperature (wet air)Rosalina sp.CarbonBiomass/Abundance/Elemental compositionBolivina pseudoplicataPartial pressure of carbon dioxide water at sea surface temperature wet airCarbon dioxideQuinqueloculina stelligeraQuinqueloculina spPeneroplis pertususRocky shore communityEntire communityPeneroplis planatusFugacity of carbon dioxide water at sea surface temperature wet airCornuspira involvensBiomass Abundance Elemental compositionCoast and continental shelfLobatula lobatulaQuinqueloculina boscianaPseudotriloculina sp.
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