Bank retreat plays a fundamental role in fluvial and estuarine dynamics. It affects the cross‐
sectional evolution of channels, provides a source of sediment, and modulates the diversity …

The spatio‐temporal heterogeneity in process–form–vegetation interactions has enabled the
Brahmaputra river system to dissipate the fluvial energy at hierarchical scales. The present …

Gully head collapse is caused by the combined action of water and gravity, resulting in the
loss of soil and water in granite soil slope of southern China. However, the soil moisture …

The present paper utilizes the Google Earth Engine (GEE) cloud computing platform and
hydro-morphological dataset to understand the complex process-form relationships of the …

Recent significant channel evolution in the **gjiang Reach has raised much attention,
particularly the remarkable bank erosion. A coupled model for simulating bed deformation …

Suffusion is a typical kind of internal erosion that changes the permeability property of soil
without destroying its structure. A horizontal laboratory test was conducted to analyze the …

Bank failures in alluvial rivers are a typical soil-water interaction problem, which is related to
many factors including the direct action of flow, river stage change, and human actions (such …

Abstract In the Wind-Water Erosion Crisscross Region of the northern Loess Plateau, parts
of loess slopes have been covered by layers of aeolian sand of different thicknesses …

Bank erosion is a key process in a fluvial system in the context of river dynamics and
geomorphology. Since the operation of the Three Gorges Project (TGP), the Lower **gjiang …

Seepage in contour ridge systems is a common phenomenon that can exacerbate soil
erosion, however, the characteristics of soil erosion under seepage conditions in contour …