Evaluation of the bank stability and toe erosion model (BSTEM) for predicting lateral retreat on composite streambanks

@article{Midgley2012EvaluationOT,
  title={Evaluation of the bank stability and toe erosion model (BSTEM) for predicting lateral retreat on composite streambanks},
  author={Taber L. Midgley and Garey A. Fox and Derek M. Heeren},
  journal={Geomorphology},
  year={2012},
  volume={145},
  pages={107-114}
}
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125 Citations
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125 Citations

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Modeling streambank erosion and failure along protected and unprotected composite streambanks
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High streambank erosion and failure rates on streams in the Ozark ecoregion of Oklahoma may be attributed to land use change and degradation of riparian areas. Numerous benefits may be achieved from…
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Streambanks can be a significant source of sediment and phosphorus to aquatic ecosystems. Although the streambank-erosion routine in the Soil and Water Assessment Tool (SWAT) has improved in recent…
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Bank retreat in the Jingjiang Reach is closely related not only to the near‐bank intensity of fluvial erosion but also to the composition and mechanical properties of bank soils. Therefore, it is…
Watershed and streambank erosion modeling in a coldwater stream using the GWLF-E model: application and evaluation
While many watershed models estimate overland flow-related soil loss, streambank erosion is often overlooked even though it can be the dominant source of sediment in a catchment. We used the enhanced…
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Two fluvial erosion models are commonly used to simulate the erosion rate of cohesive soils: the empirical excess shear stress model and the mechanistic Wilson model. Both models include two soil…
Quantifying Sediment Loads from Streambank Erosion and Potential Load Reductions from Streambank Stabilization Using Process-based Modeling
Unstable streambanks contribute a significant sediment load to surface waters in some watersheds. Streambank stabilization techniques are available to increase stability of streambanks or reduce…
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References

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Soil properties controlling seepage erosion contributions to streambank failure
The majority of sediment leaving catchments may be from streambank failure. Seepage erosion of unconsolidated sand above a restrictive layer is an important erosion process in incised streams that…
Coupled simulations of fluvial erosion and mass wasting for cohesive river banks
The erosion of sediment from riverbanks affects a range of physical and ecological issues. Bank retreat often involves combinations of fluvial erosion and mass-wasting, and in recent years bank…
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Influence of seepage undercutting on the stability of root‐reinforced streambanks
Several mechanisms contribute to streambank failure including fluvial toe undercutting, reduced soil shear strength by increased soil pore‐water pressure, and seepage erosion. Recent research has…
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The Role of Subsurface Flow in Hillslope and Stream Bank Erosion: A Review
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