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  • Articles  (4)
  • Best. von Lanthan, Cer, Neodym in Anorg. Material, Glas, Praseodymoxid, Aluminium  (1)
  • Campanian Ignimbrite  (1)
  • Chromosome mapping  (1)
  • Co-ion dependence  (1)
  • 2010-2014  (1)
  • 1995-1999  (1)
  • 1980-1984  (2)
Collection
  • Articles  (4)
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  • 2010-2014  (1)
  • 1995-1999  (1)
  • 1980-1984  (2)
  • 2005-2009  (1)
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  • 1
    Publication Date: 2021-06-16
    Description: The Campi Flegrei caldera collapsed 39 ka in the Neapolitan area (southern Italy) after the Campanian Ignimbrite eruption. This eruption, recognized as the largest and the most cataclysmic volcanic event in the Mediterranean area over the past 200 ka, extruded not less than 300 km3 of trachytic magma. Controversy exists over the timescales required to assemble a such large volume of silicic melt and thus whether large magmatic reservoirs can actually persist below active volcanic systems over prolonged periods of time. Uranium-series analyses have been performed on Campanian Ignimbrite whole-rocks, glass matrixes and separated minerals, and the obtained results have been interpreted in combination with data on Sr, Nd, Pb isotopes from literature. The compositionally most evolved sample which is most radiogenic with respect to Sr isotopes records a reference age of 71 ka. By contrast, U-Th internal isochrones of the three compositionally least evolved samples give identical initial Th isotope ratios and yield consistent ages predating the eruption by up to 6.4 ka. The highest Pb and Nd isotopic ratios and 230Th/232Th activity ratios together with the oldest reference age of the most evolved samples suggest the existence of a resident magma body possibly related to a magmatic system that is known to have fed earlier magmatic activity in the Campi Flegrei area. Conversely, the younger age of the least evolved and least radiogenic magma dates the crystallization/differentiation event of a chemically and isotopically new magma batch entering the reservoir of the resident magma some few thousand years before the cataclysmic eruption. Therefore, the time preceding this large caldera-forming eruption during which the large volume of Campanian Ignimbrite magma assembled and mixed is 6.4 ± 2.1 ka.
    Description: This study benefited from the financial support of the 5th Framework Programme of the European Union within the ERUPT project.
    Description: Published
    Description: 217-228
    Description: 3.5. Geologia e storia dei vulcani ed evoluzione dei magmi
    Description: JCR Journal
    Description: restricted
    Keywords: U-Th isotopes ; Campanian Ignimbrite ; 05. General::05.02. Data dissemination::05.02.01. Geochemical data
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    ISSN: 1432-1211
    Keywords: Key words Lipopolysaccharide binding protein ; Chromosome mapping ; Mouse ; Transcription ; Microsatellite
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine
    Type of Medium: Electronic Resource
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  • 3
    ISSN: 1612-1112
    Keywords: Chloride distribution coefficient ; Co-ion dependence ; Halide selectivity
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Notes: Summary The dependence of the chloride distribution coefficient on the co-ion of solutions of different alkali fluorides, MF, up to 11M is tested on the strongly basic anion-exchange resin AG1-X10. Under the same experimental conditions the distribution coefficient decreases in the following order for M+: Na+〉K+〉Rb+〉Cs+. This can be explained by the different co-ion-chloride interactions. The consequence of this interaction for a chromatographic separation of chloride is shown with 5M KF and CsF solutions, used as eluants. Depending on the fluoride concentration, the distribution coefficient passes through a minimum value to increase again at higher electrolyte concentration. The non-exchange electrolyte in the resin phase is responsible for this effect. In addition, the bromide and the iodide distribution coefficients up to 10M KF solutions are determined. One results is that the selectivity coefficient between halide ions increases at higher electrolyte concentrations.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Fresenius' Zeitschrift für analytische Chemie 310 (1982), S. 146-153 
    ISSN: 1618-2650
    Keywords: Best. von Lanthan, Cer, Neodym in Anorg. Material, Glas, Praseodymoxid, Aluminium ; Massenspektrometrie/Isotopenverdünnungstechnik ; Thermionisation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Zusammenfassung Die Spurenbestimmung von La, Ce und Nd durch massenspektrometrische Isotopenverdünnungsanalyse in Laborglas, Praseodymoxid und Aluminiumfolien, welche nach Dotierung mit einem Lanthanoidisotop im Kernreaktor bestrahlt wurden, wird beschrieben. Die gemeinsame Abtrennung der zu analysierenden Lanthanoide aus der Glas- und Aluminiummatrix bzw. ihre Anreicherung gegenüber Praseodym erfolgt über Anionenaustauschchromatographie. Die Ionisation der Proben im Massenspektrometer wird mit Hilfe der Zweiband-Thermionisationstechnik durchgeführt, wobei die Abhängigkeit des Atomionen/ Oxidionen-Verhältnisses von den Ionenquellenbedingungen ermittelt wird. Es können La, Ce und Nd-Gehalte im untersten μg/g-Bereich mit relativen Standardabweichungen zwischen 1–14% bestimmt werden. In den im Kernreaktor bestrahlten Aluminiumproben kann u.a. das 140Ce-Isotop neben einer über 400fach größeren Menge an 139La ermittelt werden. Wesentlicher Vorteil der massenspektrometrischen Isotopenverdünnungsanalyse ist, daß die erhaltenen Ergebnisse relativ richtig sein sollten und auch Isotope bestimmt werden können.
    Notes: Summary The trace determination of La, Ce and Nd by mass spectrometric isotope dilution analysis in laboratory glass, in praseodymium oxide and in aluminium foils which were irridiated in a nuclear reactor after adding a lanthanide isotope is described. The separation of the lanthanides to be analysed from the glass and the aluminium matrix as well as the enrichment from the praseodymium matrix was achieved by anionic exchange chromatography. Ionization of the samples in the mass spectrometer was carried out by double filament thermal ionization technique. The dependence of the atomic ions and lanthanide oxide ions on the ion source conditions was determined. La, Ce and Nd contents in the lower μg/g range could be determined with relative standard deviations of 1–14%. In one of the aluminium foils, the isotope 140Ce e.g. could be analysed in presence of a more than 400 times higher 139La amount. The essential advantage of mass spectrometric isotope dilution analysis is the accuracy of the results and the possibility to analyse isotopes as well as element contents.
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