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  • Wiley  (117)
  • 2020-2022  (9)
  • 2015-2019  (55)
  • 1995-1999  (53)
  • 1960-1964
  • 1
    Publikationsdatum: 2020-02-22
    Print ISSN: 0011-183X
    Digitale ISSN: 1435-0653
    Thema: Land- und Forstwirtschaft, Gartenbau, Fischereiwirtschaft, Hauswirtschaft
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 1997-09-01
    Print ISSN: 0003-021X
    Digitale ISSN: 1558-9331
    Thema: Chemie und Pharmazie , Werkstoffwissenschaften, Fertigungsverfahren, Fertigung
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2016-07-14
    Beschreibung: Precursory aseismic slip lasting days to months prior to the initiation of earthquakes has been inferred from seismological observations. Similar precursory slip phenomena have also been observed in laboratory studies of shear rupture nucleation on frictional interfaces. However the mechanisms that govern rupture nucleation, even in idealized laboratory settings, have been widely debated. Here we show that a numerical model incorporating rate-and-state friction laws and elastic continuum can reproduce the behaviours of rupture nucleation seen in laboratory experiments. In particular, we find that both in laboratory experiments and simulations with a wide range of normal stresses, the nucleation consists of two distinct phases: initial slow propagation phase and faster acceleration phase, both of which are likely aseismic processes, followed by dynamic rupture propagation that radiates seismic waves. The distance at which the rupture transitions from the initial slow phase to the acceleration phase can be roughly predicted by a theoretical estimate of critical nucleation length. Our results further show that the critical nucleation length depends on the background loading rate. In addition, our analysis suggests that critical nucleation length and breakdown power derived from the Griffith-crack energy balance control the scaling of nucleating ruptures. Moreover, the background loading rate and loading configuration significantly affect the rupture propagation speed. Furthermore, if the same nucleation mechanism applies to natural faults, the migration speed of foreshocks triggered by the propagation of slow rupture within the nucleation zone would depend on the effective normal stress and hence fluid pressure in the fault zone.
    Print ISSN: 0148-0227
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2015-05-30
    Beschreibung: To investigate the relationships between the movement of an eddy and its interior structure and water properties, four profiling floats were deployed in an anticyclonic eddy in the western North Pacific in 2013 (April–October). Daily float profiles showed rapid changes in temperature and salinity corresponding to strong interactions between eddies north of the subtropical Kuroshio Extension. After the first interaction with a warm-core eddy in April, the isolation of the winter mixed layer from the surface was observed, forming a subsurface remnant layer. Another interaction with a cold fresh eddy at mid-depths in May resulted in the formation of a multilayer structure. The eddy then moved poleward along the Japan and Kuril–Kamchatka trenches, indicating changes in its propagation pattern coupled to its interior structure. The eddy then moved northward (June–July), stalled (July–August), and moved eastward (August–October). In addition to a general declining trend, the properties of the warm saline core changed over a short time period, coinciding with changes in propagation. A density anomaly at mid-depths of the eddy changed location during the stalled period; however, denser waters were continuously observed in the southeast part of the eddy during its northward and eastward movement. This unidirectional density anomaly pattern was consistent with the structure of the poleward-propagating eddy, which interacted with the western topographic boundary. Meridional exchanges of heat and material were potentially elevated by the eddy's advection and movement, as well as by water modifications in the eddy associated with exchanges along its perimeter. This article is protected by copyright. All rights reserved.
    Print ISSN: 0148-0227
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
    Publikationsdatum: 2015-10-14
    Beschreibung: Unloading induces bone loss and causes disuse osteoporosis. However, the mechanism underlying disuse osteoporosis is still incompletely understood. Here we examined the effects of cathepsin K (CatK) deficiency on disuse osteoporosis induced by using sciatic neurectomy (Nx) model. After four weeks of surgery, Cat-K KO and WT mice were sacrificed and subjected to analyses. For cancellous bone rich region, Nx reduced the bone mineral density (BMD) compared to the BMD in the sham operated side in wild type mice. In contrast, CatK deficiency suppressed such Nx-induced reduction of BMD in cancellous bone. Nx also reduced BMD in the mid shaft cortical bone compared to the BMD in the corresponding region on the sham operated side in wild type mice. In contrast, CatK deficiency suppressed such Nx-induced reduction of BMD in the mid shaft cortical bone. Bone volume (BV/TV) was reduced by Nx in WT mice. In contrast, Cat-K deficiency suppressed such reduction in bone volume. Interestingly, CatK deficiency suppressed osteoclast number and osteoclast surface in the Nx side compared to sham side. When bone marrow cells obtained from Nx side femur of CatK-KO mice were cultured, the levels of the calcified area in culture were increased. Further examination of gene expression indicated that Nx suppressed the expression of genes encoding osteoblast-phenotype-related molecules such as Runx2 and alkaline phosphatase in WT mice. In contrast, CatK deficiency suppressed such reduction. These data indicate that CatK is involved in the disuse-induced bone mass reduction. This article is protected by copyright. All rights reserved
    Digitale ISSN: 1097-4652
    Thema: Biologie , Medizin
    Publiziert von Wiley
    Standort Signatur Erwartet Verfügbarkeit
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  • 6
    Publikationsdatum: 2015-12-18
    Beschreibung: A novel acoustic tomographic measurement system capable of resolving sound travel time in extremely shallow rivers is introduced and the results of an extensive field measurements campaign are presented and further discussed. Acoustic pulses were transmitted over a wide frequency band of 20–35 kHz between eight transducers for about a week in a meandering reach of theBāsen River, Hiroshima, Japan. The purpose of the field experiment was validating the concept of acoustic tomography in rivers for visualizing current fields. The particular novelty of the experiment resides in its unusual tomographic features: subbasin scale (100 m × 270 m) and shallowness (0.5–3.0 m) of the physical domain, frequency of the transmitted acoustic signals (central frequency of 30 kHz), and the use of small sampling intervals (105 s). Inverse techniques with no a priori statistical information were used to estimate the depth-average current velocity components from differential travel times. Zeroth-order Tikhonov regularization, in conjunction with L-curve method deployed to stabilize the solution and to determine the weighting factor appearing in the inverse analysis. Concurrent direct environmental measurements were provided in the form of ADCP readings close to the right and left bank. Very good agreement found between along-channel velocities larger than 0.2 m/s obtained from the two techniques. Inverted quantities were, however, underestimated, perhaps due to vicinity of the ADCPs to the banks and strong effect of river geometry on the readings. In general, comparing the visualized currents with direct nodal measurements illustrate the plausibility of the tomographically reconstructed flow structures.
    Print ISSN: 0043-1397
    Digitale ISSN: 1944-7973
    Thema: Architektur, Bauingenieurwesen, Vermessung , Geographie
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 7
    Publikationsdatum: 2015-05-26
    Beschreibung: Temperature variations caused by a typhoon were measured in the northern part of Hiroshima Bay by four coastal acoustic tomography (CAT) systems. The horizontal distributions of depth-averaged temperature from 0 to 8 m were mapped at ten-minute intervals between the 11 th and the 25 th of September 2013. The horizontal distributions of a coastal upwelling and the associated diurnal internal tides were reconstructed well by regularized inversion based on the grid segmented method, using one-way travel time data along five successful sound transmission lines. Station-to-station ranges were corrected in such a way that sound speed (determined from one-way travel time data) was equal to sound speed calculated from a couple of CTD (conductivity-temperature-depth) datasets on each transmission line. In addition, all station positions were adjusted to make focal points at the geographical positions of the transducers. The corrections increased the accuracy of temperature measurements to make temperature errors as small as 0.073-0.079 o C. The high accuracy made it possible to map the temperature structure with a variation range of less than 0.5 o C. An upwelling grew from 16 to 17 Sept., due to a typhoon-derived northerly wind. The diurnal internal tide resonated with the semi-diurnal external tide, which was pronounced after the upwelling decayed (18 Sept.), around the time the spring tide occurred. The upwelling and mixing fractions were formulated. These fractions increased continuously as the upwelling grew. Complete mixing was observed during the upwelling's mature phase. This article is protected by copyright. All rights reserved.
    Print ISSN: 0148-0227
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Publikationsdatum: 2015-01-25
    Beschreibung: Interferometric Synthetic Aperture Radar (InSAR) data reveal surface slip on multiple faults triggered by the 2013 Mw 6.6 Lake Grassmere earthquake, New Zealand. Surface offsets of 1 - 2 cm occurred on previously inferred flexural-slip faults located ~4 km from the epicentre. We document dip slip on at least three different northeast-striking, northwest-dipping, flexural-slip faults located in the western limb of a syncline. The along-strike extent of the triggered slip is 1 - 1.5 km for each fault. Dislocation models suggest that triggered slip is confined to shallow depths (~800 m). Coulomb stress analysis indicates that slip was not triggered by the static stress change of the main shock but was likely caused by dynamic shaking during the passage of seismic waves. Our finding also provides an important clue on how some slip on shallow flexural-slip faults takes place.
    Print ISSN: 0094-8276
    Digitale ISSN: 1944-8007
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 9
    Publikationsdatum: 2017-09-15
    Beschreibung: A typhoon-driven upwelling event was observed with coastal acoustic tomography in Hiroshima Bay during September 2013. The tomography data were used to obtain state estimates from an ocean model, employing the ensemble Kalman filter (EnKF) for data assimilation. Hiroshima Bay was represented as a two-layer system with a fresh, near-surface layer overlaying a more saline, lower layer. Wind from the typhoon forced the surface layer southward, thus drawing the lower layer northward and causing upwelling. After the upwelling, these currents reversed for a period. During the upwelling, the total volume transports for the upper and lower layers were well balanced, showing continuity of the two layers. However, the total upper-layer volume transported northward during the reverse-flow period was significantly smaller than the total upper-layer volume transported southward during the upwelling, and significantly larger than the total lower-layer volume transported southward during the reverse-flow period. The downstream reductions of transported volume indicated mixing fractions of 24-30%, with water mixing at the interface of the upper and lower layers. Errors in state estimates were less than the changes in current and salinity associated with the upwelling.
    Print ISSN: 0148-0227
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2018-03-06
    Beschreibung: It is difficult to detect the signal of slow deformation in the 0.1–1.0 Hz frequency band between tectonic tremors and very low frequency events (VLFE), where microseism noise is dominant. Here we provide the first evidence of slow earthquakes in this microseism band, observed by the DONET1 ocean bottom seismometer network, after a Mw 5.8 earthquake off Kii Peninsula, Japan, on April 1 st , 2016. The signals in the microseism band were accompanied by signals from active tremors, VLFEs, and slow slip events that radiated from the shallow plate interface. We report the detection and locations of events across five frequency bands, including the microseism band. The locations and timing of the events estimated in the different frequency bands are similar, suggesting that these signals radiated from a common source. The observed variations in detectability for each band highlight the complexity of the slow earthquake process.
    Print ISSN: 0094-8276
    Digitale ISSN: 1944-8007
    Thema: Geologie und Paläontologie , Physik
    Publiziert von Wiley im Namen von American Geophysical Union (AGU).
    Standort Signatur Erwartet Verfügbarkeit
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