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  • 1
    facet.materialart.
    Unbekannt
    Academic Press
    In:  Professional Paper, Open-File Rept., Advances in Geophysics, San Diego, Academic Press, vol. 22, no. 16, pp. 40-56, (ISBN 0080419208)
    Publikationsdatum: 2002
    Schlagwort(e): Seismicity ; Magnitude ; Statistical investigations ; ZMAP ; Gutenberg-Richter magnitude frequency b-value
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2015-08-29
    Beschreibung: We study the dynamics of two pinned droplets under the influence of an applied electric stress. We find that at a sufficiently strong field, this stress is sufficient to induce contact of the droplets. Interestingly, upon such contact, the dynamic behavior sensitively depends on the separation distance between the droplets. Besides the classical “coalescence” regime, we identify two other dynamic regimes: “fuse-and-split” and “periodic non-coalescence.” In the “fuse-and-split” regime, the droplets first fuse to form a jet, which subsequently breaks up into two droplets. In the “periodic non-coalescence” regime, the droplets contact and bounce away periodically without coalescence. Further analysis indicates that while the electric stress stretches the droplets into shapes that depend on the initial droplet separation, the surface tension stress dominates over the electric stress as soon as the droplets touch. We show that the shapes of the contacting droplets determine their subsequent dynamics. Our work provides a rationale for understanding the interplay between surface tension and electric stresses that govern the behavior of charged droplets and could inspire new methods for characterizing emulsion stability and surfactant performance.
    Print ISSN: 1070-6631
    Digitale ISSN: 1089-7666
    Thema: Physik
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Digitale Medien
    Digitale Medien
    College Park, Md. : American Institute of Physics (AIP)
    The Journal of Chemical Physics 111 (1999), S. 9280-9286 
    ISSN: 1089-7690
    Quelle: AIP Digital Archive
    Thema: Physik , Chemie und Pharmazie
    Notizen: The electronic absorption spectra of mono-hydrogenated carbon chain anions C2nH− (n=5–10) have been measured in the gas-phase and in 6 K neon matrices (n=8–12). The techniques of resonant two-color electron photodetachment in the gas-phase and absorption spectroscopy of mass-selected anions in neon matrix were used. A homologous series is observed, with band system origins shifting from 304 nm for C10H− to 590 nm for C20H−. In conjunction with ab initio calculations the band systems are attributed to a 1Σ+←X 1Σ+ transition of linear acetylenic anions. Another near lying electronic transition due to a second isomer is also apparent for C10H− up to C24H−. Comparison with tables of the known diffuse interstellar bands indicates possible matches for the origin bands of the C18H− and C20H− isomers. © 1999 American Institute of Physics.
    Materialart: Digitale Medien
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2004-04-01
    Print ISSN: 0037-1106
    Digitale ISSN: 1943-3573
    Thema: Geologie und Paläontologie , Physik
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2014-01-01
    Print ISSN: 0895-0695
    Digitale ISSN: 1938-2057
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2008-07-01
    Print ISSN: 0895-0695
    Digitale ISSN: 1938-2057
    Thema: Geologie und Paläontologie
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2000-10-01
    Beschreibung: We tested the hypothesis that, on the scale of a decade, earthquakes deeper than 60 km are produced at an approximately constant, that is, stationary Poissonian rate. We selected earthquakes with depths greater than 60 km to avoid the ubiquitous clusters present in shallow seismicity, without declustering the data set. Six of the 90 randomly positioned volumes contained obvious aftershock sequences and, thus, were excluded from the scoring. We showed that magnitude shifts of 0.2 to 0.4 units are present in some catalogs. Since we measure the seismicity rate above a minimum magnitude, these shifts introduce artificial fluctuations in the rate. Therefore, we modeled the influence of the magnitude shifts on the test. Measuring the goodness of fit to a stationary Poisson process model by the Chi (super 2) -test for samples of 500 earthquakes each, we found that the hypothesis cannot be rejected at the 95% confidence levels based on the data in the 84 volumes without obvious aftershock sequences. We propose that this constancy of production rate is due to the effect of a constant loading rate by tectonic plate motion on an asperity assembly with a uniform distribution of current loading stress. Although this result cannot be obtained for shallow seismicity because of the presence of numerous clusters, it seems reasonable to assume that the shallow background seismicity is also produced at a stationary Poissonian rate.
    Print ISSN: 0037-1106
    Digitale ISSN: 1943-3573
    Thema: Geologie und Paläontologie , Physik
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Publikationsdatum: 2006-04-01
    Beschreibung: The earthquake catalog in southern Iceland between 20.25 degrees W and 21.3 degrees W is complete down to approximately M (sub w) 0 and shows no evidence for magnitude shifts as a function of time since 1991. This means that 6902 earthquakes (M〉 or =-0.1, depth 〈 or =20 km) are available for studies of seismicity patterns preceding the two M (sub S) 6.6 mainshocks in 2000, in their source volumes and vicinity (20.25 degrees W and 20.9 degrees W). The power law of the frequency-magnitude relationship holds down to M (sub 0) . Detailed mapping (including 3D mapping) of the b-value of the frequency- magnitude distribution shows that variations from b = 0.6 to 1.4 exist over distances of about 2 km. This suggests that the tectonic fabric in southern Iceland is heterogeneous on a small scale. The hypocenters of the two M (sub S) 6.6 mainshocks and one additional M 4.5 mainshock are associated with low b-values (0.6-0.8), statistically significantly different from volumes in their vicinity. Therefore, one can expect future mainshocks in southern Iceland to also emanate from volumes characterized by low b-values. However, the small dimensions of these asperities may render it difficult to identify them before the mainshocks occur. Low values of estimated local recurrence times (500-2000 years) map the two fault zones that ruptured in 2000 against a background of local recurrence times longer than 5000 years. The first of the two M 6.6 mainshocks emanated from a volume of short estimated local recurrence time. This supports the hypothesis that asperities with short local recurrence times control locations of major ruptures. Mapping of b-values in cross sections shows anomalies of high b at the bottom of the seismogenic crust, correlating with the change of its thickness in the middle of the study area. These high b-value anomalies, and other pockets of such anomalies at shallower depths, are best interpreted as caused by high pore pressure because evidence of fluids under high pressure is ubiquitous in this area.
    Print ISSN: 0037-1106
    Digitale ISSN: 1943-3573
    Thema: Geologie und Paläontologie , Physik
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2011-05-29
    Beschreibung: For estimating fatalities and injured within minutes after an earthquake worldwide, we rely on real-time teleseismic determinations of epicenters. To estimate the teleseismic location errors, we computed the difference between the local epicenters of the dense seismograph networks of Japan, Italy, and Taiwan with those given by the PDE, those distributed in real time by the U.S. Geological Survey (USGS), and the European Mediterranean Seismological Center (EMSC). The average difference is 16 and 8 km between PDE teleseismic epicenters and those by the local networks for Japan/Taiwan and Italy, respectively. For EMSC epicenters, the average difference is 13 km for Italy. The average difference between real-time USGS parameters and those listed in the PDE is 12 km (median 9 km) for 30 earthquakes in Japan. Comparisons of real-time USGS epicenters and the Japan Meterological Agency (JMA) locations yield an average difference of 31 km (median 26 km). Estimates indicate that the epicenter errors in the local catalogs are typically 1 and 3 km for Japan/Italy and Taiwan, respectively. Assuming that the differences in earthquake locations are mostly due to teleseiseismic errors, we conclude that the mean errors in real-time epicenter solutions are in the range of 25 to 35 km. This implies that for earthquakes of M approximately 6.7 in the vicinity of a medium-sized city (80,000), the fatality estimates using QLARM in real time have to range from near 0 to 10,000 in the developing world and from 0 to 500 in an industrialized country. These results were verified by comparison with observed numbers of fatalities in the cases of the 2003 M 6.7 Bam, Iran, and the 2008 M 6.9 Iwate-Miyagi, Japan, earthquakes.
    Print ISSN: 0037-1106
    Digitale ISSN: 1943-3573
    Thema: Geologie und Paläontologie , Physik
    Standort Signatur Erwartet Verfügbarkeit
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