Английская Википедия:Barchan
Шаблон:Short description Шаблон:For multi
A barchan or barkhan dune (from Kazakh бархан Шаблон:IPA-kk) is a crescent-shaped dune. The term was introduced in 1881 by Russian naturalist Alexander von Middendorf,[1] based on their occurrence in Turkestan and other inland desert regions. Barchans face the wind, appearing convex and are produced by wind action predominantly from one direction. They are a very common landform in sandy deserts all over the world and are arc-shaped, markedly asymmetrical in cross section, with a gentle slope facing toward the wind sand ridge, comprising well-sorted sand.
This type of dune possesses two "horns" that face downwind, with the steeper slope known as the slip face, facing away from the wind, downwind, at the angle of repose of the sand in question, approximately 30–35 degrees for medium-fine dry sand.[2][3][4] The upwind side is packed by the wind, and stands at about 15 degrees. Barchans may be Шаблон:Convert high and Шаблон:Convert wide at the base measured perpendicular to the wind.
Simple barchan dunes may appear as larger, compound barchan or megabarchan dunes, which can gradually migrate with the wind as a result of erosion on the windward side and deposition on the leeward side, at a rate of migration ranging from about one meter to 100 meters per year. Barchans usually occur as groups of isolated dunes and may form chains that extend across a plain in the direction of the prevailing wind. Barchans and mega-barchans may coalesce into ridges that extend for hundreds of kilometers. Dune collisions[5][6] and changes in wind direction spawn new barchans from the horns of the old ones and govern the size distribution of a given field.[7]
As barchan dunes migrate, smaller dunes outpace larger dunes, catching-up the rear of the larger dune and eventually appear to punch through the large dune to appear on the other side. The process appears superficially similar to waves of light, sound, or water that pass directly through each other, but the detailed mechanism is very different. The dunes emulate soliton behavior, but unlike solitons, which flow through a medium leaving it undisturbed (similar to waves passing through water), the sand particles themselves are moved. When the smaller dune catches up 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.[8]
Barchan dunes have been observed on Mars, where the thin atmosphere produces winds strong enough to move sand and dust.[9] Marine barchan dunes appear underwater as sands shift their way across the seabed.[10][11]
See also
- Шаблон:Annotated link
- Шаблон:Annotated link, about snowforms of similar mechanism
References
External links
- Dune types—Great Sand Dunes National Park
- Шаблон:URL
- ↑ Шаблон:Cite web
- ↑ Ошибка цитирования Неверный тег
<ref>; для сносокPye2008не указан текст - ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite journal
- ↑ Ошибка цитирования Неверный тег
<ref>; для сносокElbelrhiti2005не указан текст - ↑ Ошибка цитирования Неверный тег
<ref>; для сносокSchwammle2003не указан текст - ↑ Ошибка цитирования Неверный тег
<ref>; для сносокmarsне указан текст - ↑ Шаблон:Cite journal
- ↑ Шаблон:Cite web
