Abstract We investigate the use of the short-lived fallout radionuclide beryllium-7 (7Be; t1/2 = 53.4 days) as a tracer of medium and coarse sand (0.25 – 2 mm), which transitions between transport in suspension and as bed load, and to further evaluate the effects of impoundment on seasonal and spatial variations in bed sedimentation. We measure 7Be activities in approximately monthly samples from point bar and streambed sediments in one unregulated and one regulated stream. In the regulated stream our sampling spanned an array of flow and management conditions during the annual transition from flood control in the winter and early spring to run-of-the-river operation from late spring through fall. Sediment stored behind the dam during the winter quickly became depleted in 7Be activity. This resulted in a pulse of “dead” sediment released when the dam gates were opened in the spring which could be tracked as it moved downstream. Measured average sediment transport velocities (30 – 80 m/d) exceed those typically reported for bulk bed load transport and are remarkably constant across varied flow regimes, possibly due to corresponding changes in bed sand fraction. Results also show that the length scale of the downstream impact of dam management on sediment transport is short (~1km); beyond this distance the sediment trapped by the dam is replaced by new sediment from tributaries and other downstream sources.
Salant, N.L., Renshaw, C.E., Magilligan, F.J., Kaste, J.M., Nislow, K.H., Heimsath, A.M., The use of short-lived radionuclides to quantify transitional bed material transport in a regulated river, Earth Surface Processes and Landforms, 32:509-524, 2007.