Sediment is one of the most common causes of stream impairment. Great progress has been
made in understanding the processes of soil erosion due to surface runoff and incorporating …

It is predicted that 60% of all new energy investments over the next 20 years will be in
renewables. The estimation for new hydropower production is 25% of all new renewables …

The awareness of the transmission of the sticky sediments for the development and
maintenance of reservoirs and water transfer network is very important. This research was …

This study identifies and assesses the controls on hydraulic erosion of cohesive riverbanks
on a 600-m reach of an urban ephemeral stream with active bank erosion. We examined …

A numerical model of river morphology for meander bends with erodible cohesive banks is
herein developed and tested. The new model has three key features. First, it couples a two …

The dynamic component in hydrology, sedimentology, and, consequently, river morphology
serves as a backbone for the entire river environment (Maddock 1999). In addition to water …

Dynamic interaction between river morphodynamics and vegetation affects river channel
patterns and populations of riparian species. A range of numerical models exists to …

Streambank erosion is known to be a major source of sediment in streams and rivers. The
Bank Stability and Toe Erosion Model (BSTEM) was developed in order to predict …

Incision and ensuing widening of alluvial stream channels is widespread in the midsouth
and midwestern United States and represents an important form of channel adjustment …

Limited information exists on one of the mechanisms governing sediment input to streams:
streambank erosion by ground water seepage. The objective of this research was to …