A fluid contained between two parallel walls, one of which is at rest
and the other moving in the longitudinal direction with a constant vel
ocity, is examined when a standing sound wave is imposed in the transv
erse direction. Vortical acoustic streaming appears in the region betw
een the walls. The streaming is not affected by the main flow. A quali
tative analysis is presented for the Navier-Stokes equations governing
the steady-streaming component of the motion. The study considers the
case of flow with high streaming Reynolds number and makes an explici
t determination of the vorticity in the inviscid core region. The effe
ct of the streaming upon the shear flow in the longitudinal direction
is then analysed asymptotically. A periodic structure of the wall shea
r stress in the transverse direction is detected in which vast areas o
f vanishing wall shear stress alternate with narrow regions where it i
ncreases significantly. A relation expressing the mean wall shear stre
ss in terms of the streaming Reynolds number is derived. Results obtai
ned show that acoustic streaming results in a marked enhancement of th
e mean wall shear stress at the walls.