Dissolved organic carbon (DOC) dynamics were investigated over a two y
ear period in the Upper Rhone River to examine the role of side-arms i
n providing DOC to the main channel in relation to discharge fluctuati
ons, especially floods. Concentrations of DOC are shown to remain low
in space and in time (average 1.5 mgl(-1)) and to be more related to g
lobal hydrological events (precipitation) than to any local flushing f
or backwaters during floods. The results do not support the general as
sumption that side-arms are the providers of DOC to the main channel.