Assessing the effect of vegetation-related bank strength on channel morphology and stability in gravel-bed streams using numerical models

Bank strength Clue to vegetation dominates the geometry of small stream channels, but has virtually no effect on the geometry of larger ones. The dependence of bank strength on channel scale affects the form of downstream hydraulic geometry relations and the meandering-braiding threshold. It is also associated with a lateral migration threshold discharge, below which channels do riot migrate appreciably across their floodplains. A rational regime model is used to explore these scale effects it parameterizes vegetation-related bank strength using a dimensionless effective cohesion, C(r)*. The scale effects are explored primarily using all alluvial state space defined by the dimension less formative discharge, Q*, and channel slope, S, which is analogous to the Q-S diagrams originally used to explore meandering-braiding thresholds. The analyses show that the effect of vegetation on both downstream hydraulic geometry and the meandering-braiding threshold is strongest for the smallest streams in a watershed, but that the effect disappears for Q* > 10(6). The analysis of the migration threshold suggests that the critical discharge ranges from about 5 m(3)/s to 50 m(3)/s, depending on the characteristic rooting depth for the vegetation. The analysis also suggests that, where fires frequently affect riparian forests, channels may alternate between, laterally stable gravel plane-bed channels and laterally active riffle-pool channels. These channels likely do riot exhibit the classic dynamic equilibrium associated with alluvial streams, but instead exhibit a cyclical morphologic evolution, Oscillating between laterally stable and laterally Unstable end-members with a frequency determined by the forest fire recurrence interval. Copyright (C) 2008 John Wiley & sons, Ltd.