This paper reports the results of an experimental investigation on flow res
istance law for a gravel-bed channel having bed arrangements characterized
by different values of the number of boulders. The dependence is studied of
a parameter, proposed for describing the gravel-bed surfaces, on the bould
er concentration and on the ratio between the median diameter of the coarse
r particles and the median diameter of the bed layer. Flume measurements ca
rried out for the hydraulic condition of transition and large-scale roughne
ss (1.5 less than or equal to h/d(50) less than or equal to 6.9) show that
the intercept of the semilogarithmic flow resistance law depends on the rat
io and on boulder concentration. For concentration values less than 50%, a
relationship is developed between the intercept and proposed parameter; for
higher concentration values, the intercept is assumed constant and equal t
o -1.5. Further differences between the experimentally determined values of
the friction-factor parameter and values calculated using the semi-logarit
hmic expression for flow resistance are explained in terms of the ratio bet
ween the Shields parameter and its critical value.