A general formula for the uniform flow of water in rivers and other channels; by E. Ganguillet and W.R. Kutter. Tr. from the German, with numerous additions, including tables, diagrams, and the elements of over 1200 gaugings of rivers, small channels and pipes, in English measure (1889)
Ganquillet, E, Hering, Rudolph, 1847-, Kutter, Wilhelm R., 1818-1888, Trautwine, John Cresson, 1850-1924 · New York J. Wiley · leaf 41
ccu-racy of the results. From the resulting mass of evidence the VELOCITIES VARY AS THE ABSCISSA OF A PARABOLA. 15 elements were obtained from which Humphreys and Abbot de-rived their new formula. 9. The velocities found to vary as the abscissae of a parabola. The results of these measurements were… … Fig.2, Mississippi Velocities at different depths.* The scale of icind -forces ranfjesfrom 0<.cat/n)to 10{hurricanc\ tal lines drawn at their respective depths, form the abscissaeof a parabolic curve, with its axis parallel to the surface andsituated at the depth of the maximum velocity. This…
Hydraulics · Stream measurements
Internet Archive · Gerstein Library, University of Toronto · Public Domain Mark 1.0. Free to use for anything.
