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Barchans are isolated mobile dunes often organized in large dune fields. Dune fields seem to present a characteristic dune size and spacing, which suggests a cooperative behavior based on dune interaction. In Duran et al. (2009), we propose…

软凝聚态物质 · 物理学 2011-05-20 Orencio Durán , Veit Schwämmle , Pedro G. Lind , Hans J. Herrmann

Barchan dunes emerge as a collective phenomena involving the generation of thousands of them in so called barchan dune fields. By measuring the size and position of dunes in Moroccan barchan dune fields, we find that these dunes tend to…

软凝聚态物质 · 物理学 2011-03-29 Orencio Durán , Veit Schwämmle , Pedro G. Lind , Hans J. Herrmann

In nature, barchan dunes typically exist as members of larger fields that display striking, enigmatic structures that cannot be readily explained by examining the dynamics at the scale of single dunes, or by appealing to patterns in…

软凝聚态物质 · 物理学 2013-07-15 S. Worman , A. B. Murray , R. Littlewood , B. Andreotti , P. Claudin

The collision processes of two crescentic dunes called barchans are systematically studied using a simple computer simulation model. The simulated processes, coalescence, ejection and reorganization, qualitatively correspond to those…

软凝聚态物质 · 物理学 2009-11-10 Atsunari Katsuki , Hiraku Nishimori , Noritaka Endo , Keisuke Taniguchi

Barchan dunes were found to transform into parabolic dunes and vice versa when the amount of vegetation on and around them changes. This work presents the first numerical simulation of this effect. We propose a continuum model for the…

其他凝聚态物理 · 物理学 2007-05-23 O. Duran , V. Schatz , H. J. Herrmann , H. Tsoar

In a recent experimental breakthrough, Hersen et al. [1] demonstrated that by changing the agitating medium from air to water, one can obtain, on laboratory scale, dunes that are downsized copies of desert dunes, thereby overcoming a major…

软凝聚态物质 · 物理学 2009-11-10 Klaus Kroy , Xiang Guo

Barchans are eolian dunes of crescent shape found on Earth, Mars and other celestial bodies. Among the different types of barchan-barchan interaction, there is one, known as chasing, in which the dunes remain close but without touching each…

In this work, we report measurements of the height profile of transverse dunes in the coastal dune field known as ``Len\c{c}\'ois Maranhenses'', northeastern Brazil. Our measurements show that transverse dunes with approximately the same…

统计力学 · 物理学 2007-05-23 E. J. R. Parteli , V. Schwaemmle , H. J. Herrmann , L. H. U. Monteiro , L. P. Maia

Barchans are crescent-shaped dunes commonly found in diverse environments and scales: from the 10-cm-long barchans found under water to the 1-km-long barchans on Mars, passing by the 100-m-long dunes on Earth's deserts. Although ubiquitous…

Barchans are crescentic dunes propagating on a solid ground. They form dune fields in the shape of elongated corridors in which the size and spacing between dunes are rather well selected. We show that even very realistic models for…

凝聚态物理 · 物理学 2009-11-10 P. Hersen , K. H. Andersen , H. Elbelrhiti , B. Andreotti , P. Claudin , S. Douady

Barchan dunes are found where sand availability is low and wind direction quite constant. The two dimensional shear stress of the wind field and the sand movement by saltation and avalanches over a barchan dune are simulated. The resulting…

凝聚态物理 · 物理学 2007-05-23 V. Schwaemmle , H. Herrmann

Barchans are dunes of crescentic shape found on Earth, Mars and other celestial bodies, growing usually on polydisperse granular beds. In this Letter, we investigate experimentally the growth of subaqueous barchans consisting of bidisperse…

To analyze theoretically the stability of the shape and the migration process of transverse dunes and barchans, we propose a {\it skeleton model} of 3D dunes described with coupled dynamics of 2D cross-sections. First, 2D cross-sections of…

斑图形成与孤子 · 物理学 2012-01-05 Hirofumi Niiya , Akinori Awazu , Hiraku Nishimori

We demonstrate the feasibility of studying dunes in a laboratory experiment. It is shown that an initial sand pile, under a wind flow carrying sand, flattens and gets a shape recalling barchan dunes. An evolution law is proposed for the…

凝聚态物理 · 物理学 2009-11-07 O. Dauchot , F. Lechenault , C. Gasquet , F. Daviaud

Corridors of size-selected crescent-shaped dunes, known as barchans, are commonly found in water, air, and other planetary environments. The growth of barchans results from the interplay between a fluid flow and a granular bed, but their…

地球物理 · 物理学 2021-08-24 Willian Righi Assis , Erick de Moraes Franklin

Three dimensional dunes of crescentic shape, called barchans, are commonly found on Earth and other planetary environments. In the great majority of cases, barchans are organized in large fields in which corridors of size-selected barchans…

地球物理 · 物理学 2021-12-03 Willian Righi Assis , Fernando David Cúñez , Erick de Moraes Franklin

Crescent shaped barchan dunes are highly mobile dunes that are usually presented as a prototypical model of sand dunes. Although they have been theoretically shown to be unstable when considered separately, it is well known that they form…

地球物理 · 物理学 2015-06-12 Mathieu Génois , Pascal Hersen , Sylvain Courrech du Pont , Guillaume Grégoire

Barchans are crescent-shape dunes ubiquitous on Earth and other celestial bodies, which are organized in barchan fields where they interact with each other. Over the last decades, satellite images have been largely employed to detect…

地球物理 · 物理学 2024-08-15 Esteban Andrés Cúñez Benalcázar , Erick de Moraes Franklin

Barchans are crescent-shaped sand dunes forming in aride regions with unidirectional wind and limited sand supply. We report analytical and numerical results for dune shapes under different environmental conditions as obtained from the…

软凝聚态物质 · 物理学 2009-11-11 Klaus Kroy , Sebastian Fischer , Benedikt Obermayer

We present results of numerical simulations to estimate scaling exponents associated with driven surface growth in two spatial dimensions. We have simulated the restricted solid--on--solid growth model and used the time and system size…

凝聚态物理 · 物理学 2009-10-22 T. Ala-Nissila , O. Venalainen
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