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 …

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 …

We propose a method for evaluating the risks of slope failure induced by heavy rain over a
wide area by combining infiltration analysis, surface flow analysis, and slope stability …

Many studies on shallow landslides have focused on seepage mechanisms. However, most
of these studies assumed that the hillslope was parallel to the seepage direction and force; …

摘要金沙江白鹤滩水电工程坝区发育有数条规模较大的, 对工程有直接影响的玄武岩层间错动带
. 错动带内充填碎屑夹泥, 当大坝建成蓄水之后, 在高水头差下容易发生渗透破坏 …

Seepage is the prominent hydrological process on tilled hillslopes covered by purple soil,
which can easily exacerbate slope instability and soil loss. Laboratory simulated …

The construction of the Three Gorges Reservoir dam in China has led to an increase in
reservoir landslide events. To mitigate these geohazards, multiple rows of stabilizing piles …

The dominant mechanism of riverbank cantilever failure is soil erosion of the bank toe and
near bank zone. This paper demonstrates that the shape of the riverbank cantilever failure …

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 …

Effectively managing and reducing high suspended sediment loads in rivers requires an
understanding of the magnitude of major sediment sources as well as erosion and transport …