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  • 21
    Electronic Resource
    Electronic Resource
    Springer
    Earth, moon and planets 66 (1994), S. 29-30 
    ISSN: 1573-0794
    Keywords: Comet Shoemaker-Levy 9 ; Jupiter ; albedo
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract The impact sites of the Comet Shoemaker-Levy 9 are observed with the 101-cm telescope at Bisei Astronomical Observatory until the end of August with B, V, R, I, and methane-band (0.89εm) filters. The outline of the observation is briefly described.
    Type of Medium: Electronic Resource
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  • 22
    Electronic Resource
    Electronic Resource
    Springer
    International journal of fracture 17 (1981), S. 111-119 
    ISSN: 1573-2673
    Source: Springer Online Journal Archives 1860-2000
    Topics: Mechanical Engineering, Materials Science, Production Engineering, Mining and Metallurgy, Traffic Engineering, Precision Mechanics
    Description / Table of Contents: Résumé Dans les aciers à faible ductilité et à haute résistance, le comportement à la fatigue au cours des premiers stades du phénomène est associé aux inclusions non métalliques et présente un caractère hautement localisé au voisinage de l'inclusion. Cependant, la nature du processus d'initiation d'une fissure de fatigue n'est pas claire. Dans ce mémoire, l'accent à été placé sur des différences que l'on peut rencontrer dans le mécanisme d'amorçage et dans le début de la croissance des fissures de fatigue entre un acier martensitique et des matériaux de ductilité normale. La faible liaison existant entre la matrice et une inclusion d'oxyde d'aluminium conduit à la formation d'une singularité associée à l'inclusion qui détermine une croissance de la contrainte. La fissure de fatigue prend naissance à la périphérie de cette singularité à un angle de 45° par rapport à la direction de la contrainte principale. Les observations métallurgiques et micro-fractographiques ont révélé que l'amorçage et le début de croissance des fissures de fatigue à partir d'inclusions métalliques relèvent du cisaillement plutôt que de la traction simple. On conclut donc que, bien que le processus de fatigue est entièrement localisé au voisinage d'une inclusion, le mécanisme d'amorçage et de début de croissance d'une fissure de fatigue est essentiellement le même que dans un matériau ductile. L'effet d'hétérogénéités métallurgiques dans la martensite, tel que les frontières du grain austénitique primaire, les empilements et les plaquettes, peuvent être considérés sur l'amorçage et le début de croissance des fissures de fatigue; ce point est également discuté au point de vue mécanique et métallurgique.
    Notes: Abstract In low ductility and high strength steels, the early stage fatigue behavior associated with non-metallic inclusions is a highly localized phenomenon near the inclusions. However, the nature of the fatigue crack initiation process is not clear. In this paper, a special emphasis is placed on the possible differences in the mechanism of initiation and the early growth of fatigue cracks between a martensitic steel and ordinary ductile materials. The poor adhesion between matrix and aluminum oxide inclusion leads to the formation of an inclusion pit which serves as a simple stress raiser. The fatigue crack originates at the periphery of this inclusion pit at an angle of 45 degrees to the principal stress direction. Metallurgical and micro-fractographical observations revealed that the initiation and early growth of fatigue cracks from non-metallic inclusion are of the shear rather than the tensile mode. Thus, it is concluded that, though the fatigue process is quite localized in the vicinity of inclusion, the mechanism for an initiation and early growth of fatigue cracks is essentially the same as that for ductile materials. The effects of metallurgical heterogeneities in the martensite, such as the prior austenite grain boundaries, packets, and plates on the initiation and early growth of the cracks, are also discussed from the mechanical-metallurgical viewpoint.
    Type of Medium: Electronic Resource
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  • 23
    ISSN: 1619-7089
    Keywords: Syndrome X ; Continuous ventricular function monitor ; Supine exercise ; VEST
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Abstract Left ventricular function during exercise and recovery was investigated in patients with angina pectoris, ST segment depression during exercise and angiographically normal coronary arteries (syndrome X) using a continuous left ventricular function monitor with cadmium telluride detector (CdTe-VEST). Fourteen patients with syndrome X and 14 patients with atypical chest pain without ST segment depression during exercise and normal coronary arteries (control group) performed supine ergometric exercise after administration of 740–925 MBq of technetium-99m labelled red blood cells, and left ventricular function was monitored every 20 s using CdTe-VEST. Left ventricular ejection fraction (EF) response was impaired (≤55% increase from rest to peak exercise) in 11 or 14 patients with syndrome X but in none of the control patients. Resting EF was similar in the two groups (62.1%±6.7% in patients with syndrome X, 61.9%±6.2% in controls); however, EF increase from rest to peak exercise was lower in syndrome X (−3.1±9.5% vs 14.7%±7.4%, P 〈0.001). After cessation of exercise, all patients showed rapid EF increase over baseline and this EF overshoot was lower (19.3%±8.3% vs 26.4%±7.3%, P 〈0.001) with the time to EF overshoot longer (114±43 s vs 74±43 s, P〈0.05) in patients with syndrome X. Thus, in patients with syndrome X, left ventricular dysfunction was frequently observed during exercise in spite of normal epicardial coronary arteries.
    Type of Medium: Electronic Resource
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  • 24
    ISSN: 1619-7089
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Type of Medium: Electronic Resource
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  • 25
    Electronic Resource
    Electronic Resource
    Springer
    Mineralogy and petrology 46 (1992), S. 155-161 
    ISSN: 1438-1168
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Zusammenfassung Potosiit and Incait wurden in Erzen der Hoei-Mine, Oita Präfektur, Japan, nachgewiesen. Potosiit kommt in plattigen Kristallen (3 cm x 2 cm) vor and ist mit Arsenkies, Magnetkies, Zinnkies, Jamesonit and Pyrit assoziiert. Incait kommt in polykristallinen Aggregaten, die Ränder um Bleiglanz bilden, oder als Haar-artige Massen in einer Matrix von Kutnahorite vor. Röntgendiffraktionsdaten zeigen, daß es sich hier um Potosiit and Incait handelt; Mikrosondenanalysen der beiden Minerale geben die allgemeine Formel (Pb, Sn)2+ 6+x(FeSb2 4+)2S4+x, with x 〈 2. Potosiit ist homogen, während Incait in Kontakt mit Bleiglanz inhomogen ist. Quantitative Reflexionsdaten für Potosiit zeigen, daß seine Bireflexion zu den niedrigsten bei opaken Mineralen mit Schichtgitter gehört.
    Notes: Summary Potosiite and incaite have been found at the Hoei mine, Oita Prefecture, Japan. Potosiite occurs as tabular crystals (3 cm x 2 cm in size), and is associated with arsenopyrite, pyrrhotite, stannite,jamesonite and pyrite, whereas incaite occurs as polycrystalline aggregates rimming galena or as hair-like masses in a matrix of kutnahorite. X-ray powder data reveal that these minerals are potosiite and incaite, respectively. Electron-microprobe analyses of potosiite and incaite gave the general formula (Pb, Sn)2+ 6+xFeSb2Sn4+ 2S14+x, with x 〈 2. Potosiite is homogeneous, whereas incaite, in contact with galena, is quite heterogeneous. Reflectance data for potosiite show that its bireflectance is one of the lowest among opaque minerals with a sheet-like structure.
    Type of Medium: Electronic Resource
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  • 26
    ISSN: 1432-8798
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Summary Antigenic variation of pseudorabies virus glycoprotein g II was demonstrated in field isolates by neutralizing monoclonal antibodies. Mutants capable of avoiding neutralization by the monoclonal antibodies specific for glycoproteins g II and g III could be obtained from the parent virus by mutagenesis.
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