Annotation
Experimental studies of kinematic flow characte ristics and turbulent - fluctuation energy spectra on a model estuarine reach are described. They are compared with measurements made on the channel reach of the model. It is shown that feeding additional sediment into the stream changes the nature of the vertical distribution of turbulence intensity: it decreases in the region near the bottom and increases in the subsurface region.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
N.A. Mikhаilоva, О.P. Petrоsyan, V.A. Platоnоv
Science News of the Faculty of Physics, Lomonosov Moscow State University
This new information publication, which is intended to convey to the staff, students and graduate students, faculty colleagues and partners of the main achievements of scientists and scientific information on the events in the life of university physicists.