An important difficulty in understanding turbulence in natural flows is tha
t one does not see what is being measured by devices recording velocity flu
ctuations. This study shows how visualization of turbulent structures can b
e effectively implemented in natural river flows. In order to match turbule
nt flow structures with their velocity signatures, flow visualization is co
mbined with high-frequency (20 Hz) velocity measurements from electromagnet
ic current meters. Two fluvial environments are examined. In a river conflu
ence where the difference in turbidity provides a natural tracer, very stro
ng negative velocity fluctuations for the streamwise component are concomit
ant with an upwelling motion. A video recording made from a bridge of the p
assage of turbulent structures delineated by turbid and clear water allowed
us to relate the marked fluctuations in velocity to eddies of a duration o
f 1-2 s in the mixing layer. In a gravel-bed river we have examined pattern
s of eddy shedding in the lee of a pebble cluster. These patterns were high
lighted by dye (milk) injected in the separation zone downstream. Black and
white images were obtained from an underwater lens linked to a video camer
a recorder. We observed a complex dynamic characterized by two dominant pat
terns of eddy shedding: one with a clear motion of eddies toward the water
surface and another with a downward expansion toward the bed of the structu
res. This pattern is related to the passage of intermittent wedges of low-s
peed fluid separated by wedges of fast moving fluid.