Comparison of Fixed- and Moving-Vessel Flow Measurements with an aDp in a Large River-Reference-Cited by-同舟云学术

Comparison of Fixed- and Moving-Vessel Flow Measurements with an aDp in a Large River

Published:2007-12 Issue:12 Volume:133 Page:1299-1309
ISSN:0733-9429
Container-title:Journal of Hydraulic Engineering
language:en
Short-container-title:J. Hydraul. Eng.

Author:

Szupiany Ricardo N.¹²³⁴,Amsler Mario L.¹²³⁴,Best James L.¹²³⁴,Parsons Daniel R.¹²³⁴

Affiliation:

1. Ph.D. Fellow of the National Council of Scientific and Technical Researches (CONICET), College of Engineering and Water Sciences, Littoral National Univ., Ciudad Universitaria, C.C. 217, (3000), Santa Fe, Argentina. E-mail: rszupian@fich1.unl.edu.ar

2. Researcher, National Council of Scientific and Technical Researches (CONICET), College of Engineering and Water Sciences, Littoral National Univ., Ciudad Universitaria, C.C. 217, (3000), Santa Fe, Argentina. E-mail: mamsler@fich1.unl.edu.ar

3. Threet Professor of Sedimentary Geology and Professor of Geography, Dept. of Geology and Geography and Ven Te Chow Hydrosystems Laboratory, Univ. of Illinois at Urbana-Champaign, 1301 W. Green St., Urbana, IL 61801. E-mail: jimbest@uiuc.edu

4. Research Fellow, Natural Environment Research Council, Earth and Biosphere Institute, School of Earth and Environment, Univ. of Leeds, Woodhouse Lane, Leeds, LS2 9JT, U.K. E-mail: d.parsons@see.leeds.ac.uk

Publisher

American Society of Civil Engineers (ASCE)

Subject

Mechanical Engineering,Water Science and Technology,Civil and Structural Engineering

Link

http://ascelibrary.org/doi/pdf/10.1061/%28ASCE%290733-9429%282007%29133%3A12%281299%29

Reference53 articles.

1. Amsler M. L. and Gaudin H. E. (1994). “Influencia de la superposición de dunas en el transporte de la carga de fondo en el Río Paraná.” XV Congreso Nacional del Agua La Plata Argentina (in Spanish).

2. Some aspects of turbulent flow structure in large alluvial rivers

3. Mean flow and turbulence structure over fixed, two-dimensional dunes: implications for sediment transport and bedform stability

4. The morphology of river channel confluences

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