Search results for "mass [baryon]"

showing 10 items of 262 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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Towards Shorter-Lived Nuclides in ISOLTRAP Mass Measurements

2001

Recently, the applicability of Penning trap mass spectrometry has been extended to nuclides with a half-life of less than one second. The mass of 33Ar(T 1/2 = 174 ms) was measured using the ISOLTRAP spectrometer with an accuracy of 4.2 keV. This measurement provided a stringent test of the Isobaric Multiplet Mass Equation (IMME) at mass number A = 33 and isospin T = 3/2. The fast measurement cycle that shows the way to other measurements of very-short-lived nuclides is presented. Furthermore, the results of the IMME test are displayed.

Nuclear physicsMass numberChemistryNuclideIon trapAtomic physicsMass spectrometryPenning trapISOLTRAPAtomic massHybrid mass spectrometer
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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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Local suppression of collectivity in theN=80isotones at theZ=58subshell closure

2013

) transition strengths [1] and thenumber of nucleons in the valence shell. The global behaviorof these quantities between the major shells as a function ofthe nucleon number is well understood in the frameworks ofboth collective and microscopic models. One could expect thatthese general trends in the collective properties between themajorshellsaremodulated bythesubshellstructure.However,it is usually thought that the pairing correlations with anenergy scale of about 2 MeV, smear out and dissolve thesubshell structure as long as the separation energies betweenthe subshells are only about a few hundred keV.The recently observed evolution of the isovectorquadrupole-collective valence-shell exc…

Nuclear physicsMass numberPhysicsNuclear and High Energy PhysicsPairingNuclear TheoryPhysics::Atomic and Molecular ClustersClosure (topology)NucleonValence electronPhysical Review C
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Double-βtransformations in isobaric triplets with mass numbersA=124, 130, and 136

2012

The Q values of double-electron capture in ${}^{124}$Xe, ${}^{130}$Ba, and ${}^{136}$Ce and double-beta decay of ${}^{124}$Sn and ${}^{130}$Te have been determined with the Penning-trap mass spectrometer SHIPTRAP with a few hundred eV uncertainty. These nuclides are members of three isobaric triplets with common daughter nuclides. The main goal of this work was to investigate the existence of the resonant enhancement of the neutrinoless double-electron-capture rates in ${}^{124}$Xe and ${}^{130}$Ba in order to assess their suitability for the search for neutrinoless double-electron capture. Based on our results, in neither of these cases is the resonance condition fulfilled.

Nuclear physicsPhysicsMass numberSemileptonic decayNuclear and High Energy PhysicsMAJORANADouble beta decayOrder (ring theory)ResonanceNuclideAtomic physicsMuon capturePhysical Review C
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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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Smooth terminating bands inTe112: Particle-hole induced collectivity

2007

The Gammasphere spectrometer, in conjunction with the Microball charged-particle array, was used to investigate high-spin states in Te-112 via Ni-58(Ni-58, 4p gamma) reactions at 240 and 250 MeV. Several smooth terminating bands were established, and lifetime measurements were performed for the strongest one using the Doppler-shift attenuation method. Results obtained in the spin range 18-32h yield a transition quadrupole moment of 4.0 +/- 0.5eb, which corresponds to a quadrupole deformation epsilon(2)=0.26 +/- 0.03; this value is significantly larger than the ground-state deformation of tellurium isotopes. It was also possible to extract a transition quadrupole moment for the yrast band in…

Nuclear reactionMass numberPhysicsNuclear and High Energy PhysicsAngular momentumYrastNuclear TheoryQuadrupoleGammasphereDeformation (meteorology)Atomic physicsNuclear ExperimentSpin (physics)Physical Review C
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Gamow-Teller unit cross sections for (t,He3) and (He3,t) reactions

2011

The proportionality between differential cross sections at vanishing linear momentum transfer and Gamow-Teller transition strength, expressed in terms of the unit cross section (${\mathrm{\ensuremath{\sigma}\ifmmode \hat{}\else \^{}\fi{}}}_{\mathit{GT}}$), was studied as a function of target mass number for ($t$,$^{3}\mathrm{He}$) and ($^{3}\mathrm{He}$,$t$) reactions at $115A$ MeV and $140A$ MeV, respectively. Existing ($^{3}\mathrm{He}$,$t$) and ($t$,$^{3}\mathrm{He}$) data on targets with mass number $12\ensuremath{\leqslant}A\ensuremath{\leqslant}120$ were complemented with new and reevaluated ($t$,$^{3}\mathrm{He}$) data on proton, deuteron, $^{6}\mathrm{Li}$, and $^{12}\mathrm{C}$ tar…

Nuclear reactionPhysicsMass numberNuclear and High Energy PhysicsParticle physics010308 nuclear & particles physicsHadronCarbon-12Elementary particle01 natural sciencesIsospin0103 physical sciencesBorn approximationAtomic physics010306 general physicsNucleonPhysical Review C
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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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