The transport of sand and dust by wind is a potent erosional force, creates sand dunes and
ripples, and loads the atmosphere with suspended dust aerosols. This paper presents an …

Predicting the morphodynamics of sedimentary landscapes due to fluvial and aeolian flows
requires answering the following questions: Is the flow strong enough to initiate sediment …

This article deals with the resuspension phenomenon whereby particles adhering on a wall
surface can be re-entrained by a flowing fluid. This is an area where significant progress has …

Flow-type landslides, such as debris flows and rock avalanches, erode soil bed material as
they flow downslope. The eroded material increases the volume of a landslide, and thus, its …

A major advance in the study of wind-blown sand started seventy years ago with the seminal
work of Bagnold [1]. Since then and in particular in the last decades, important progress has …

In this paper, the impact of a block on a coarse granular soil corresponding to rockfall events
is investigated using the Discrete Element Method. Different impacting particle and medium …

The wind‐driven saltation of granular material plays a key role in various geophysical
processes on Earth, Mars, Venus, and Titan. Although interparticle cohesion is known to limit …

Despite being the main sediment entrainment mechanism in aeolian transport, granular
splash is still poorly understood. We provide a deeper insight into the dynamics of sand and …

We review selected experimental saltation studies performed in laboratory wind tunnels and
collision experiments performed in (splash-) laboratory facilities that allow detailed …

This paper reviews the literature on the nature of aeolian creep, the field and wind tunnel
methods used to measure creep transport, the relative contribution of creep transport to total …