A linear stability analysis of lateral motions in shallow flow open channel
s with a free surface is presented. Unlike previous studies, this work does
not employ the rigid-lid assumption. Computations revealed that the rigid-
lid assumption works well for weak shear flows and/or small Froude numbers.
However, the validity of the rigid-lid assumption is reduced as the Froude
number increases. Also, when Reynolds numbers are larger than 1,000, the s
tability domain is insensitive to the Reynolds number for all Froude number
s. The size of the stability domain is found strongly affected by the veloc
ity and length scales of base velocity and the shape of the velocity profil
e. The analysis shows that the stability domains obtained by the Manning fo
rmula are larger than those obtained by the Chezy formula for the same Frou
de number. The analysis shows that a compound channel, whose floodplain has
larger flow resistance than the main channel does, has larger lateral tran
sport of flow mass, momentum, and energy.