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  • 1
    Electronic Resource
    Electronic Resource
    Woodbury, NY : American Institute of Physics (AIP)
    Applied Physics Letters 57 (1990), S. 2948-2950 
    ISSN: 1077-3118
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Powder-in-tube wires that contained Bi, Sr, Ca, and Cu in a 2:2:1:2 mole ratio were drawn then rolled flat before processing. The superconducting phase was aligned with its c axis perpendicular to the wide plane of the wire by sintering the wires just below the melting point and by melt processing. Melt processing with slow cooling of the melt yielded the most alignment. Gravity did not influence alignment during melt processing.
    Type of Medium: Electronic Resource
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  • 2
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: Samples of YBa2Cu3O7 have been prepared with rather sharp inductive transitions having in the best cases breadths of 7 K and midpoint Tc values of 88 K. The resistive Tc midpoints are 92–95 K with transition widths of ±1–2 K. Flux shielding at 4.2 K is normally 100% and flux expulsion at 4.2 K reaches 95%. However, even small fields of order 1 mT decouple some 15%–20% of the volume, allowing flux to enter the samples. Resistive Hc2 measurements suggest that Hc2(0) varies from 〈1 to 〉300 T, depending on the criterion chosen. ac susceptibility measurements suggest that Hc2(0) is ∼60 T. Magnetization current densities are relatively high (150–200 A/mm2 at 1–10 T at 4.2 K) but measured transport current densities are small (≤1 A/mm2). Magnetization current densities at 77 K are about two orders of magnitude lower. The samples were seen to be heavily twinned by light microscopy (scale of 1–5 μm) and by transmission electron microscopy (scale of ∼250 nm). It is concluded that these measurements are consistent with a model of superconducting regions of reduced dimensionality coupled by tunneling.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 118 (1994), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: A set of global Proudman functions, computed on a 2° finite-difference grid, is used to smooth raw tidal estimates previously derived by Cartwright and Ray from a two-year analysis of Geosat altimeter data. The least-squares problem provides an interesting application of ridge regression and Hansen's L-curve analysis. The final smoothed maps are found to agree more closely to a set of 80‘ground-truth’constants than did the original tidal models.
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 405 (2000), S. 775-778 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] How and where the ocean tides dissipate their energy are long-standing questions that have consequences ranging from the history of the Moon to the mixing of the oceans. Historically, the principal sink of tidal energy has been thought to be bottom friction in shallow seas. There has long ...
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 381 (1996), S. 595-597 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The Moon and Sun raise tides in the oceans, the atmosphere and the solid Earth. All three, but primarily the oceans, dissipate some amount of the imparted tidal energy; an accurate accounting of the tidal energy balance has been a long-sought goal12. The problem is of some importance, not only ...
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  • 6
    Electronic Resource
    Electronic Resource
    Springer
    Calcified tissue international 5 (1970), S. 236-246 
    ISSN: 1432-0827
    Keywords: Trabeculum ; Bone ; Vertebra ; Density ; Strength ; Osteoporosis
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Medicine , Physics
    Description / Table of Contents: Résumé L'objet de ce travail est de déterminer le rapport existant entre une force compressive et la densité osseuse des vertèbres humaines, ainsi que le rapport entre l'orientation des travées et la force de compression et enfin les effets du degré de charge sur la force compressive. Ce travail est effectué sur 71 échantillons prélevés au cours de 23 autopsies. Les densités sont déterminées et 2 types de densités sont calculées: 1. la densité apparente, en poids humide, divisée par le volume total de l'échantillon et 2. la densité réelle, en poids humide, divisée par le volume de la matrice osseuse, déterminé par le déplacement de l'eau. Des mesures de tests de compression sont effectuées sur des échantillons frais en utilisant une machine à tester les matériaux, de type Instron, sous des charges de déformation déterminées. Les résultats indiquent un rapport hautement significatif entre la densité apparente et la force de compression. Des rapports similaires sont trouvés entre le poids sec par volume total d'échantillon et le poids de cendre par volume total d'échantillon et la force compressive. Larsque la densité apparente augmente, la force compressive de l'échantillon diminue. Une régression négative entre la densité réelle et la force compressive est observée dans l'une des séries expérimentales de ce travail, où lorsque la densité de la matrice osseuse augmente, la force de compression de l'échantillon décroit. Ce rapport n'est pas significatif dans les deux autres séries expérimentales. La force de l'os vertébral est significativement plus élevée le long de l'axe supéro-inférieur ou axe vertical que le long des deux autres directions. Certains échantillons présentent une capacité significativement plus élevée de résistance à la compression, lorsque la charge de déformation est de 1 cm par minute, que lorsqu'elle est de 0,01 cm par minute.
    Abstract: Zusammenfassung Das Ziel dieser Untersuchung war, den Zusammenhang zwischen dem Widerstand gegen Kompression und der Dichte menschlicher Wirbel, den Zusammenhang zwischen der Anordnung der Trabekel und dem Kompressionswiderstand sowie die Auswirkung von der Belastung auf den Kompressionswiderstand festzustellen. Insgesamt wurden bei 23 Autopsien 71 Proben entnommen und untersucht. Es wurden Dichtebestimmungen vorgenommen und zwei verschiedene Dichten errechnet: 1. die scheinbare Dichte, bestimmt aus dem Naßgewicht dividiert durch das Gesamtprobenvolumen; 2. die effektive Dichte, bestimmt aus dem Naßgewicht dividiert durch das Volumen der Knochenmatrix, welches mittels Wasserverdrängung festgestellt werden konnte. An frischen Proben wurden Test-Druckmessungen bei verschiedenen bekannten Deformationsgraden mittels eines Instron-Materialprüfgerätes durchgeführt. Die Resultate ergaben eine hochsignifikante Beziehung zwischen der scheinbaren Dichte und dem Widerstand gegen Kompression. Gleiche Beziehungen fanden sich zwischen dem Kompressionswiderstand einerseits und dem Trockengewicht sowie Aschegewicht andererseits, beide auf das Gesamtprobenvolumen bezogen. Bei Zunahme der scheinbaren Dichte nahm der Kompressionswiderstand der Probe ab. Eine negative Regression zwischen effektiver Dichte und Kompressions-widerstand wurde in einer der Versuchsreihen dieser Experimente gefunden, wo bei zunehmender Dichte der Knochenmatrix der Kompressionswiderstand der Proben abnahm. Diese Beziehung war in den andern beiden Versuchsreihen nicht signifikant. Der Widerstand der Wirbelkörper war entlang der vertikalen Achse signifikant höher als in den andern beiden Richtungen. Bei einem Deformationsgrad von 1 cm/min zeigten die Proben eine signifikant höhere Widerstandskraft als bei einem solchen von 0,01 cm/min.
    Notes: Abstract The purpose of this investigation was to determine the relation between compressive strength and density of human vertebral bone, the relation between trabecular orientation and compressive strength, and the effects of the strain rate on compressive strength. A total of 71 samples obtained at 23 post mortem examinations were investigated. Density determinations were made and two different densities were calculated: (1) the apparent density as wet weight divided by the total sample volume; and (2) real density as wet weight divided by the volume of bone matrix determined by water displacement. Compression test measurements were made on the fresh samples using an Instron materials testing machine at controlled deformation rates. The results indicated a highly significant relation between apparent density and compressive strength. Similar relations were found between dry weight per total sample volume and ash weight per total sample volume and compressive strength. As the apparent density increased, the compressive strength of the sample decreased. A negative regression between real density and compressive strength was found in one of the experimental series of this investigation where, as the density of the bone matrix increased the compressive strength of the sample decreased. This relation was not significant in the other two experimental series. The strength of vertebral bone was significantly higher along the superior-inferior axis or vertical axis than along the two other directions. Samples showed a significantly greater ability to withstand compression when the deformation rate was 1 cm per minute than they did when the rate was 0.01 cm per minute.
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Journal of geodesy 71 (1997), S. 344-350 
    ISSN: 1432-1394
    Keywords: Key words. Tides ; Arctic Ocean tides ; Earth rotation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Architecture, Civil Engineering, Surveying
    Notes: Abstract. Oceanic tidal angular momentum (OTAM) is calculated for the four major tides of the Arctic Ocean, based on the tidal elevations and current velocities from a recent two-dimensional numerical hydrodynamic model. The presented OTAM tables are meant to be complementary to other modeling studies that use satellite altimetry (which cannot observe Arctic Ocean tides because of ice cover and limited satellite inclinations). Although the Arctic Ocean's influence on earth rotation is, as may be expected, relatively small, the rapid advancement of the subject now calls for such small contributions to be explicitly accounted for.
    Type of Medium: Electronic Resource
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  • 8
    Publication Date: 2020-09-29
    Print ISSN: 2169-9275
    Electronic ISSN: 2169-9291
    Topics: Geosciences , Physics
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  • 9
    Publication Date: 1990-12-31
    Print ISSN: 0003-6951
    Electronic ISSN: 1077-3118
    Topics: Physics
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  • 10
    Publication Date: 2013-02-15
    Description: Dickman argues that our model of the Mf ocean tide is unrealistic and that this invalidates conclusions regarding mantle anelasticity. His evidence is based on comparison with his own ocean modelling experiments and on his physical intuition regarding near-equilibrium tides. That evidence is unconvincing. Simple physical arguments alone are enough to rebut his main points. Furthermore, we test here his suggestion of increasing bottom-friction dissipation by a factor of 100 over our preferred solution, and we show that this results in unacceptable polar motion and poor agreement with independent tide-gauge data. In contrast, tests against independent data lend support to the realism of our Mf tide model and give confidence that our estimates of mantle anelasticity are reliable within stated error bounds.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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