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20242026
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physics.geo-ph2026

Barchan-barchan and barchan-obstacle interactions: insights from grain-scale studies

Erick de Moraes Franklin, Willian Righi Assis, Danilo da Silva Borges +1

Sand dunes are bedforms that grow due to the action of a fluid flow over a sand bed or pile. Whenever the fluid flow is mainly in one direction and the availability of sand is limi…

physics.geo-ph2025

When barchan dunes move over craters

Paulo Vitor Ribeiro Plácido, Danilo da Silva Borges, Willian Righi Assis +1

We investigate the possible outcomes of a subaqueous barchan moving over a crater-like depression in the bed. For that, we carried out experiments where we varied the dune size, cr…

physics.geo-ph2025

Barchans interacting with dune-size obstacles: details of the fluid flow and motion of grains

Nicolao Cerqueira Lima, Willian Righi Assis, Danilo da Silva Borges +1

We investigate details of the interaction of subaqueous barchans with dune-size obstacles by carrying out numerical simulations where the fluid is solved at the grain scale and the…

physics.geo-ph2025

Evolving dunes under flow reversals: from an initial heap toward an inverted dune

Willian Righi Assis, Erick de Moraes Franklin, Nathalie Vriend

Sand dunes are ubiquitous in nature, and are found in abundance on Earth and other planetary environments. One of the most common types are crescent-shaped dunes known as barchans,…

physics.geo-ph2024

On the effect of two-direction seasonal flows on barchans and the origin of occluded dunes

Willian Righi Assis, Danilo da Silva Borges, Erick de Moraes Franklin

We inquire into the morphodynamics of barchans under seasonal flows. For that, we carried out grain-scale numerical computations of a subaqueous barchan exposed to two-directional…