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Encyclopedia > Barchan

A barchan dune is an arc-shaped sand ridge, comprised of well-sorted sand. This type of dune possesses two "horns" that face downwind, with the slip face (the downwind slope) at the angle of repose, or approximately 32 degrees. The upwind side is packed by the wind, and stands at about 15 degrees. Simple barchan dunes may stretch from meters to a hundred meters or so between the tips of the horns. Image File history File linksMetadata Barchan. ... Mesquite Flat Dunes in Death Valley National Park In physical geography, a dune is a hill of sand built by eolian (wind-related) processes. ... For the engineering term, see Angle of repose. ...


Simple barchan dunes may appear as larger, compound barchan or megabarchan dunes, which may migrate with the wind. Barchans and megabarchans may coalesce into ridges that extend for hundreds of kilometers.


As barchan dunes migrate, smaller dunes outpace larger dunes, bumping into the rear of the larger dune and eventually appear to punch through the large dune to appear on the other side. The process seems to be similar to waves of light, sound or water that pass directly through each other; the detailed mechanism is, however, very different, being nonlinear. These are known as solitons. A soliton is a self-reinforcing solitary wave caused by nonlinear effects in the medium. ...


The dunes emulate soliton behavior but unlike solitons, the sand particles do not pass through each other. When the smaller dune rear-ends the larger dune, the winds begin to deposit sand on the rear dune while blowing sand off the front dune without replenishing it. Eventually, the rear dune has assumed dimensions similar to the former front dune which has now become a smaller, faster moving dune that pulls away with the wind. (Schwämmle & Herrmann, 2003)


The Great Sand Dunes National Park in the American state of Colorado has spectacular examples of barchan dunes. Great Sand Dunes National Park and Preserve became a United States national park on September 13, 2004. ... Official language(s) English Capital Denver Largest city Denver Area  - Total  - Width  - Length  - % water  - Latitude  - Longitude Ranked 8th 269,837 km² 451 km 612 km 0. ...


==Referenc



es==

  • [[|Schwämmle, V., and H.J. Herrmann]] () ({{{Month}}} 2003). [ Solitary wave behaviour of sand dunes]. Nature 426 (Dec. 11): 619-620 Abstract. .
  • [[|H. Elbelrhiti, P. Claudin, and B. Andreotti]] () ({{{Month}}} 2005). [ Field evidence for surface-wave-induced instability of sand dunes]. Nature 437 (Sep. 29): 720-723 Abstract. .

External link

  • Barchan Dunes - Great Sand Dunes National Park

  Results from FactBites:
 
Edgewater Technology Tapped by Barchan Associates for Compliance Support in State and Local Organizations - Edgewater ... (529 words)
Barchan is delivering an automated solution that handles the tasks required to comply with new financial reporting standards applicable to state and local organizations.
Barchan has developed a solution for state and local governments that makes it very easy to comply with the financial reporting requirements of GASB 34.
Barchan was founded in 2002 by Dr. John B. Miller, then Associate Professor of Civil and Environmental Engineering in the Construction Engineering and Management program at the Massachusetts Institute of Technology.
Chapter 4: Dune systems (3574 words)
Barchan dunes have curved slipfaces and two horns extending downwind, with proportions, in plan view, much like a horseshoe (Figure 4-3A, and Figure 4-5).
Crossbedding and main bounding surfaces present in the main and cross trenches for barchan and transverse ridge dunes are shown as Figures 4-12, 4-13, and 4-14.
Figure 4-15—Drawing of a trench at the base of the slipface of a barchan dune, showing the episodic (once a week, roughly) pace of accumulation of individual avalanche strata during April and May (windy season).
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