The paper presents an analysis of the composition of bedload transport and
changes to bed structure and topography during three graded sediment degrad
ation experiments. The analysis suggests that variations in channel hydraul
ics and active layer composition alone may not explain the observed reducti
ons in sediment transport. Further, the experiments appear to cover a cruci
al range of mean bed shear stresses for armouring studies, ranging between
a condition of passive winnowing, to one of more active armour development
in which the coarse grains play a role in determining bed structure. This i
ndicates that the active layer concept, commonly applied in computer models
of graded sediment transport, may be Limited in its application.