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  • 2010-2014  (6)
Materialart
Verlag/Herausgeber
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Erscheinungszeitraum
  • 2010-2014  (6)
Jahr
  • 1
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2010
    In:  Nuclear Engineering and Design Vol. 240, No. 2 ( 2010-2), p. 266-274
    In: Nuclear Engineering and Design, Elsevier BV, Vol. 240, No. 2 ( 2010-2), p. 266-274
    Materialart: Online-Ressource
    ISSN: 0029-5493
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2010
    ZDB Id: 2001319-X
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Online-Ressource
    Online-Ressource
    Hindawi Limited ; 2012
    In:  Science and Technology of Nuclear Installations Vol. 2012 ( 2012), p. 1-9
    In: Science and Technology of Nuclear Installations, Hindawi Limited, Vol. 2012 ( 2012), p. 1-9
    Kurzfassung: The subcooled decompression under temperature gradient experiment performed by Takeda and Toda in 1979 has been reproduced using the in-house code WAHA version 3. The sudden blowdown of a pressurized water pipe under temperature gradient generates a travelling pressure wave that changes from decompression to compression, and vice versa, every time it reaches the two-phase region near the orifice break. The pressure wave amplitude and frequency are obtained at different locations of the pipe's length. The value of the wave period during the first 20 ms of the experiment seems to be correct but the pressure amplitude is overpredicted. The main three parameters that contribute to the pressure wave behavior are: the break orifice (critical flow model), the ambient pressure at the outlet, and the number of volumes used for the calculation. Recent studies using RELAP5 code have reproduced the early pressure wave (transient) of the same experiment reducing the discharge coefficient and the bubble diameter. In the present paper, the long-term pipe pressure, that is, 2 seconds after rupture, is used to estimate the break orifice that originates the pressure wave. The numerical stability of the WAHA code is clearly proven with the results using different Courant numbers.
    Materialart: Online-Ressource
    ISSN: 1687-6075 , 1687-6083
    Sprache: Englisch
    Verlag: Hindawi Limited
    Publikationsdatum: 2012
    ZDB Id: 2397941-0
    SSG: 3,6
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2010
    In:  Nuclear Engineering and Design Vol. 240, No. 2 ( 2010-2), p. 275-283
    In: Nuclear Engineering and Design, Elsevier BV, Vol. 240, No. 2 ( 2010-2), p. 275-283
    Materialart: Online-Ressource
    ISSN: 0029-5493
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2010
    ZDB Id: 2001319-X
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2012
    In:  Nuclear Engineering and Design Vol. 253 ( 2012-12), p. 153-160
    In: Nuclear Engineering and Design, Elsevier BV, Vol. 253 ( 2012-12), p. 153-160
    Materialart: Online-Ressource
    ISSN: 0029-5493
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2012
    ZDB Id: 2001319-X
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
    Online-Ressource
    Online-Ressource
    AIP Publishing ; 2014
    In:  Physics of Fluids Vol. 26, No. 12 ( 2014-12-01)
    In: Physics of Fluids, AIP Publishing, Vol. 26, No. 12 ( 2014-12-01)
    Kurzfassung: Channel flow DNS (Direct Numerical Simulation) at friction Reynolds number 180 and with passive scalars of Prandtl numbers 1 and 0.01 was performed in various computational domains. The “normal” size domain was ∼2300 wall units long and ∼750 wall units wide; size taken from the similar DNS of Moser et al. The “large” computational domain, which is supposed to be sufficient to describe the largest structures of the turbulent flows was 3 times longer and 3 times wider than the “normal” domain. The “very large” domain was 6 times longer and 6 times wider than the “normal” domain. All simulations were performed with the same spatial and temporal resolution. Comparison of the standard and large computational domains shows the velocity field statistics (mean velocity, root-mean-square (RMS) fluctuations, and turbulent Reynolds stresses) that are within 1%-2%. Similar agreement is observed for Pr = 1 temperature fields and can be observed also for the mean temperature profiles at Pr = 0.01. These differences can be attributed to the statistical uncertainties of the DNS. However, second-order moments, i.e., RMS temperature fluctuations of standard and large computational domains at Pr = 0.01 show significant differences of up to 20%. Stronger temperature fluctuations in the “large” and “very large” domains confirm the existence of the large-scale structures. Their influence is more or less invisible in the main velocity field statistics or in the statistics of the temperature fields at Prandtl numbers around 1. However, these structures play visible role in the temperature fluctuations at low Prandtl number, where high temperature diffusivity effectively smears the small-scale structures in the thermal field and enhances the relative contribution of large-scales. These large thermal structures represent some kind of an echo of the large scale velocity structures: the highest temperature-velocity correlations are not observed between the instantaneous temperatures and instantaneous streamwise velocities, but between the instantaneous temperatures and velocities averaged over certain time interval.
    Materialart: Online-Ressource
    ISSN: 1070-6631 , 1089-7666
    Sprache: Englisch
    Verlag: AIP Publishing
    Publikationsdatum: 2014
    ZDB Id: 1472743-2
    ZDB Id: 241528-8
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
    Online-Ressource
    Online-Ressource
    Elsevier BV ; 2013
    In:  International Journal of Heat and Mass Transfer Vol. 66 ( 2013-11), p. 781-790
    In: International Journal of Heat and Mass Transfer, Elsevier BV, Vol. 66 ( 2013-11), p. 781-790
    Materialart: Online-Ressource
    ISSN: 0017-9310
    Sprache: Englisch
    Verlag: Elsevier BV
    Publikationsdatum: 2013
    ZDB Id: 240652-4
    ZDB Id: 2012726-1
    Standort Signatur Einschränkungen Verfügbarkeit
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