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  • 1
    Electronic Resource
    Electronic Resource
    γ-Ray-induced Formation of Gold Sol from Chloroauric Acid Solution (1962)
    [s.l.] : Nature Publishing Group
    Nature 196 (1962), S. 666-667 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] When an aqueous solution of chloroauric acid was irradiated with yravs from a cobalt-60 source, colloidal gold particles formed under the following-conditions: initial concentration of chloroauric acid, 4-9 x 10-4 M; bubbling with oxygen; radiation dose-rate of 9-3 x 103 r./min for 70 min (total ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/196666a0
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  • 2
    Electronic Resource
    Electronic Resource
    Process of the Tsushima Current formation revealed by ADCP measurements in summer (1996)
    Springer
    Journal of oceanography 52 (1996), S. 491-507 
    Details
    ISSN: 1573-868X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract In order to clarify detailed current structures over the continental shelf margin in the East China Sea, ADCP measurements were carried out in summers in 1991 and 1994 by the quadrireciprocal method (Katoh, 1988) for removing diurnal and semidiurnal tidal flows from observed flows, together with CTD measurements. We discussed the process of the Tsushima Current formation in the East China Sea. The Tsushima Current with a volume transport of 2 Sv (1 Sv=106 m3s−1) was found north of 31°N. A current with a volume transport of 0.4 Sv was clearly found along the 100 m isobath. Between the Kuroshio and the current along the 100 m isobath, southeastward component of velocity was dominant compared to northwestward one. Four eastward to southeastward currents were found over the sea bed shallower than 90 m depth. Total volume transport of these four currents was 1 Sv, and they seemed to be originated from the Taiwan Strait. Intrusion of offshore water into the inner shelf northwest of Amami Oshima was estimated to have a volume transport of 0.6 Sv. It is concluded that the Tsushima Current is the confluence of these currents over the continental shelf margin with the offshore water intruding northwest of Amami Oshima.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF02239051
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    Paper (German National Licenses)
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