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  • Inorganic Chemistry  (1)
  • Scholte waves  (1)
  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Marine geophysical researches 20 (1998), S. 239-247 
    ISSN: 1573-0581
    Keywords: bottom shots ; implosive sources ; P-waves ; Scholte waves ; seismic velocities
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Bottom shots have been used for a number of years in seismic studies on the ocean floor. Most experiments utilized explosives as the energy source, though researchers have recognized the usefulness of collapsing water voids to produce seismoacoustic signals. Implosive sources, however, suffered generally from a lack of control of source depth. We present a new experimental tool, called SEEBOSEIS, to carry out seismic experiments on the seafloor utilizing hollow glass spheres as controlled implosive sources. The source is a 10-inch BENTHOS float with penetrator. Inside the sphere we place a small explosive charge (two detonators) to destabilize the glass wall. The time of detonation is controlled by an external shooting device. Test measurements on the Ninetyeast Ridge, Indian Ocean, show that the implosive sources can be used in seismic refraction experiments to image the subbottom P-wave velocity structure in detail beyond that possible with traditional marine seismic techniques. Additionally, the implosions permit the efficient generation of dispersed Scholte waves, revealing upper crustal S-wave velocities. The frequency band of seismic energy ranges from less than 1 Hz for Scholte modes up to 1000 Hz for diving P-waves. Therefore, broadband recording units with sampling rates 〉2000 Hz are recommended to sample the entire wave field radiated by implosive sources.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 0044-2313
    Keywords: Chemistry ; Inorganic Chemistry
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology
    Description / Table of Contents: Studies on Oxide Catalysts. XXV. Catalytic Activity and Aging Properties of Modified Mordenites in the Cracking of n-OctaneMeH-mordenites (Me = Li, K, Mg, Ca, Ba) were prepared by ion exchange starting with H-mordenite (SiO2/Al2O3 mole ratio = 14). To characterize these samples the cracking of n-octane was used as catalytic test reaction. Surface OH groups and the adsorption of NH3 on these samples were investigated by i. r. spectroscopy. Unaffected by the kind of the exchanged cation the Brönsted acidity of the H-mordenite decreases monotonously with increasing content of the incorporated cation. The catalytic activity and (to a much higher degree) the rate of deactivation by coking during the reaction decrease as the Brönsted acidity decreases. The strong dependence of the Brönsted acidity on the deactivation rate points to a multi-site mechanism of the coking process.
    Notes: MeH-Mordenite (Me = Li, K, Mg, Ca, Ba) wurden ausgehend von einem H-Mordenit (Molverhältnis SiO2/Al2O3 = 14) durch Ionenaustausch hergestellt. Als Testreaktion zur Katalytischen Charakterisierung diente die n-Octanspaltung. IR-spektroskopisch wurden die OH-Oberflächengruppen und die Adsorption von NH3 an den Proben untersucht. Unabhängig von der Art des eingetauschten Kations sinkt die Brönsted-Acidität des H-Mordenits monoton mit steigendem Gehalt an den eingetauschten Kationen. Die katalytische Aktivität und (im weit Stärkeren Maße) die Desaktivierungsgeschwindigkeit (infolge „Verkokens“ während der Reaktion) sinken symbat mit der Brönsted-Acidität. Die starke Abhängigkeit der Geschwindigkeit der Desaktivierung von der Brönsted-Acidität weist auf einen Mehrzentrenmechanismus für die Verkokung hin.
    Additional Material: 5 Ill.
    Type of Medium: Electronic Resource
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