Browse Illinois Water Resources Center - Hydrology and Hydraulics by Subject "Mixing"

  • Lin, Chi-Yu; Holley, Edward R.; Maxwell, W. Hall C. (University of Illinois at Urbana-Champaign. Water Resources Center, 1977-04)
    Analytical and experimental investigations were carried out for three-dimensional buoyant surface jets with strong ambient flow but without boundary attachment. A numerical model in curvilinear coordinates was developed ...

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  • Alavian, Vahid; Broeren, Sally M. (University of Illinois at Urbana-Champaign. Water Resources Center, 1984-10)
    This paper presents the results of an investigation of mass transport by diffusion and advection in two-dimensional steady, spatially varied confined flow. In practice, this type of flow occurs in recirculating regions ...

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  • Maxwell, W. Hall C.; Demissie, Misganaw (University of Illinois at Urbana-Champaign. Water Resources Center, 1976-02)
    Detailed velocity traverses are presented for shallow submerged slot jets without lateral confinement. With wing-walls in place maximum velocities and temperatures were traced for both unheated and heated discharges. These ...

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  • Fitzgerald, Steven D.; Holley, Edward R. (University of Illinois at Urbana-Champaign. Water Resources Center, 1979-12)
    In order to mix an additive or a tracer with the fluid flowing in a pipe, it may be desirable to avoid the energy required and the possible maintenance problems for mixers or obstructions in a pipe and to avoid the relatively ...

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  • Maxwell, W. Hall C.; Snorrason, Arni (University of Illinois at Urbana-Champaign. Water Resources Center, 1981-01)
    Previous measurements of the velocity field in the vicinity of two intersecting submerged turbulent jets provided evidence that, contrary to the usual assumptions, intersecting flows may not necessarily be combined using ...

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  • Alavian, Vahid; Broeren, Sally M.; Bintz, David W. (University of Illinois at Urbana-Champaign. Water Resources Center, 1983-10)
    State-of-the-art of hydraulic and water quality modeling in streams and rivers does not include the role of large, slowly circulating regions in dilution and transport of effluents discharged in such water bodies. Examples ...

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