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 69
7 0.142 2 186 64.2 0.154 2 268 63.9 0.165 2 357 64.2 0.174 2 447 64.8 0.184 2 5.8 64.9 0.192 ** 2 612 66.0 VARIATION- OF SLOPE AFFECTING VARIATION OF c. 41 If we plot the values c for six similar v^alues of R of thesix comparable series Nos. 6 to 11 (rectangular channels linedwith boards) as… … Xv. h R=.l>34/S=.0O2O .0050 Fig. 3. ]\I. Bazin has indeed demonstrated this effect, but he did-not regard it as of sufficient moment to require recognition inhis formula. Upon this point he expresses himself as follows :* The form rt + ^ is superior to the form a -f -,f becauseR ■ the two…
Hydraulics · Stream measurements
Internet Archive · Gerstein Library, University of Toronto · Public Domain Mark 1.0. Free to use for anything.
