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Importance of advective zone in longitudinal mixing experiments

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Języki publikacji
EN
Abstrakty
EN
One-dimensional Fickian dispersion models such as the advection diffusion equation (ADE) are commonly used to analyse and predict concentration distributions downstream of contamination events in watercourses. Such models are only valid once the tracer had entered the equilibrium zone. This paper compares previous theoretical, experimental and numerical estimates of the distance to reach the equilibrium zone with new experimental values, obtained by examining the change of skewness in a tracer profile, downstream of a cross-sectionally well mixed source. Closer agreement was found with Fischers’ theoretical estimate than prior experimental and numerical studies.
Czasopismo
Rocznik
Strony
95--103
Opis fizyczny
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autor
autor
Bibliografia
  • Chatwin, P.C., 1972, The cumulents of the distribution of concentration of a solute in a solvent flowing along a straight tube, J. Fluid Mechanics 51, 1, 63-67.
  • Fischer, H.B., 1967, The mechanics of dispersion in natural streams, J. Hydraulics Division 93, HY 6, 187.
  • Fischer, H.B., 1973, Longitudinal dispersion and turbulent mixing in open channel flow, Ann. Rev. Fluid Mech. 5, 59-78.
  • Rutherford, J.C., 1994, River Mixing, J. Wiley and Sons Ltd., New York, 347 pp.
  • Sayre, W.W., 1968a, Dispersion of mass in open channel flow, PhD Thesis, Colorado State University, Fort Collins.
  • Taylor, G.I., 1921, Diffusion by continuous movement, Proc. London Mathematics Soc. Ser 2, 20, 196-212.
  • Tsai, Y.H., and E.R. Holley, 1978, Temporal moments for longitudinal dispersion, Am. Soc. Civ. Engin. 104, HY12, 1617-1634.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0021-0011
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