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  • 1965-1969  (3)
  • 1950-1954  (3)
Material
Years
Year
  • 1
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Analytical chemistry 22 (1950), S. 185-188 
    ISSN: 1520-6882
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Industrial and engineering chemistry 7 (1968), S. 565-572 
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 205 (1965), S. 110-110 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Many of the examples have used measurements of continuous or quantitative traits such as body-weights, observations on cell heights and mouse reflex times. The sensitivity of a specific experiment involving a quantitative trait can be measured by the 'F value'. It represents the ratio of the ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Meteorology and atmospheric physics 6 (1954), S. 417-439 
    ISSN: 1436-5065
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geography , Physics
    Description / Table of Contents: Summary Occurrence of predominantly horizontal linear air currents in the ionosphere could be verified by direct and indirect electrical observations. The maximum of frequency of the measured wind velocities lies, within the range of 80 and 120 km altitude, at 60 m/sec and within theF-layer (200 to 350 km altitude) at 100 m/sec. The measured wind velocities do not show a uniform pattern. The standard deviation of the observations reaching several 100 per cent makes it probable that wind direction and speed depend on the hour of day and the season as well as on the geographical latitude and altitude. Considering particularly theF-layer the velocity of propagation of the deviation centers was found to be proportional to the earth-magnetic characteristic number. The extention of these deviation centers, however, does not depend on the intensity of the earth-magnetic disturbance and is nearly constant also in other respects. These more or less linear air currents are combined with a more or less turbulent movement. The direct and indirect observations verify this for the range between 80 and 100 km altitude; knowledge on the respective conditions in theF-layer, however, could not be obtained by them. The root of the average velocity square of all velocity components in the direction of the observations amounts to approximately 2 m/sec. The occurrence of solar and lunar tides in the range of theE-layer with a velocity amplitude of 35 and 25 m/sec respectively can be considered as a indisputable fact, whereas for theF-layer there exist too few investigations as yet.
    Abstract: Résumé La présence de courants d'air essentiellement horizontaux dans l'ionosphère a été prouvée par des observations visuelles directes et électriques indirectes. Le maximum de fréquence des vitesses de vent mesurées se trouve dans la couche comprise entre 80 et 120 km, où elles atteignent 60 m/s, ainsi qu'au niveau de la coucheF (200–350 km) avec 100 m/s. Les directions observées ne fournissent pas d'image simple; la dispersion des mesures conduit à penser que les azimuts et les vitesses dépendent du moment du jour et de la saison, comme de la latitude et de l'altitude. En ce qui concerne la coucheF en particulier, il apparaît que la vitesse de déplacement des centres de dispersion est proportionnelle au nombre caractéristique géomagnétique. La grandeur de ces centres est toutefois indépendante de l'intensité de la perturbation géomagnétique et reste à peu près constante. A ces courants ionosphériques plus ou moins linéaires se superpose un courant d'air plus ou moins turbulent; les observations directes et indirectes vérifient ce fait pour la couche comprise entre 80 et 120 km, mais elles ne peuvent rien dire à ce sujet en ce qui concerne la coucheF. La racine carrée du carré moyen des vitesses de toutes les composantes de vitesse dans la direction d'observation est égale à 2 m/s environ. L'existence de marées solaires et lunaires dans la coucheE avec une amplitude des vitesses de respectivement 35 et 25 m/s peut être considérée comme assurée; les recherches analogues concernant la coucheF sont encore trop peu nombreuses.
    Notes: Zusammenfassung Siehe Abschnitt IV.
    Type of Medium: Electronic Resource
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  • 5
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    Unknown
    Chicago, Ill. : Periodicals Archive Online (PAO)
    The University of Chicago Law Review. 18 (1950/1951) 394 
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  • 6
    Electronic Resource
    Electronic Resource
    Hoboken, NJ : Wiley-Blackwell
    AIChE Journal 13 (1967), S. 1155-1159 
    ISSN: 0001-1541
    Keywords: Chemistry ; Chemical Engineering
    Source: Wiley InterScience Backfile Collection 1832-2000
    Topics: Chemistry and Pharmacology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: The pressure drop of water was measured when water flowed through a bed of stainless steel ball bearings packed in an ordered rhombohedral geometry. Experiments were carried out with eleven different packed beds, encompassing the entire range of the square-base array, in the same 10.85 by 10.85 by 30-in. rectangular test column in a forced circulation loop at modified Reynolds numbers up to 17,000. The test variables included water velocity, bed voidage, spacing between adjacent balls, ball diameter, and bed height. Curves of friction factor vs. Reynolds number are presented. An increase in the relative horizontal spacing between balls was found to have a more important effect than an increase in voidage in decreasing the pressure drop. A general correlation relating the mutual effects of bed voidage and ball spacing on pressure drop that would bring all the data points together, especially in the transition flow region, could not be found. As a result, the system appears to consist of two distinct parts separated at the minimum packing density. A correlation was found only for the first, but from a practical point of view more important, region. Data may be corrected for bed voidage, but only for small variations in ball spacing, by the ratios of (1 - ε)/ε3 at the two voidages. No entrance and exit effects could be measured beyond the first seven ball layers.
    Additional Material: 7 Ill.
    Type of Medium: Electronic Resource
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