An experimental analysis of bed load transport in gravel-bed braided rivers with high grain Reynolds numbers

作者：De Vincenzo Annamaria; Brancati Francesco; Pannone Marilena

来源：Advances in Water Resources, 2016, 94: 160-173.

DOI：10.1016/j.advwatres.2016.05.007

• River morphology
• Gravel-bed braided rivers
• Bed load transport
• Stream power
• Laboratory experiments
• Bed profile semivariogram

Laboratory experiments were performed with nearly uniform fluvial gravel (D-50=9 mm, D-10=5 mm and D-90=13 mm) to analyse the relationship between stream power and bed load transport rate in gravel-bed braided rivers at high grain Reynolds numbers. The values of the unit-width dimensionless bed-load rate q(b)* and unit-width dimensionless stream power omega* were evaluated in equilibrium conditions based on ten different experimental runs. Then, they were plotted along with values obtained during particularly representative field studies documented in the literature, and a regression law was derived. For comparison, a regression analysis was performed using the data obtained from laboratory experiments characterized by smaller grain sizes and, therefore, referring to relatively low grain Reynolds numbers. A numerical integration of Exner's equation was performed to reconstruct the local and time-dependent functional dependence of q(b)* and w*. The results led to the following conclusions: 1) At equilibrium, the reach averaged bed load transport rate is related to the reach-averaged stream power by different regression laws at high and low grain Reynolds numbers. Additionally, the transition from bed to suspended load transport is accelerated by low Re*, with the corresponding bed load discharge increasing with stream power at a lower, linear rate. 2) When tested against the gravel laboratory measurements, the high Re* power law derived in the present study performs considerably better than do previous formulas. 3) The longitudinal variability of the section-averaged equilibrium stream power is much more pronounced than that characterizing the bed load rate, at least for high Re*. Thus, the stream power and its local-scale heterogeneity seem to be directly responsible for transverse sediment re-distribution and, ultimately, for the determination of the spatial and temporal scales that characterize the gravel bedforms. 4) Finally, the stochastic interpretation of the wetted bed elevation function mapped in a particularly representative sample run reveals that gravel-bed transport and braiding are associated with the persistence of multiple equilibrium energy states due to the presence of truly non-stationary, local-scale pseudo-periodicity.

• 出版日期2016-8