Stage dependent variability in tractive force distribution through a riffle-pool sequence

High resolution data on spatial and temporal variability in flow hydraulics and sediment transport within riffle-pool sequences are required to improv e understanding of how fluvial processes maintain these meso-scale bedforms . This paper addresses this issue by providing velocity and boundary shear stress data over a range of discharges from base flow (0.07 m(3) s(-1)) to just over bankfull (8.52 m(3) s(-1)), fl om a sequence of four pools and th ree riffles in the River Rede, Northumberland. The data supports the revers al hypothesis of Keller [Geol. Sec. Am. Bull. 87 (1971) 753.] as the primar y explanation for the maintenance of the riffle-pool sequence, although the y also indicate that spatial variability in tractive force is highly stage dependent and complex. Section-averaged velocity data indicate reversal to be evident at four our of six riffle-pool units. An equalisation in velocit y was: found for the other two riffle-pool units close to bankfull stage. T he spatial patterns of tractive force exhibited in the study reach as a res ult of increased discharge demonstrate that riffle-pool units operate indep endently of one another. Shear stress reversals were observed in individual riffle-pool units at different river stages during a flood hydrograph. and in some instances, two occurred in the same riffle-pool unit during a sing le flow event. Pools were characterised by coarser bed sediments and narrow er channel widths in comparison to riffles, increasing the likelihood of tr active force reversal in the River Rede. Areas of predicted bed sediment en trainment obtained from tau (o) - tau (c), matched observed channel changes in the upper part of the study reach, but over-estimated change in the mid dle portion of the reach. (C) 2001 Elsevier Science B.V. All rights reserve d.