ELECTRIC CURRENTS OF SALTATION IN WINDSAND FLUX

dc.contributor.author	Gorchakov G.I.
dc.contributor.author	Kopeikin V.M.
dc.contributor.author	Isakov A.A.
dc.contributor.author	Karpov A.V.
dc.contributor.author	Ul'yanenko A.V.
dc.contributor.author	Ermakov V.I.
dc.date.accessioned	2024-11-02T11:07:41Z
dc.date.available	2024-11-02T11:07:41Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520553
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1109-1111
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46325
dc.description.abstract	Electric currents in the surface atmospheric layer in desertized areas were measured for the first time. At wind velocities equal to 5–7 m/s, the density of electric current due to saltation of sand grains at a height of 3 cm reaches 3–5 μA/m2, which is six orders of magnitude greater than the density of electric current in the unperturbed atmosphere (2–3 pA/m2). The burst-shaped currents are positive in the main (lower) saltation layer and alternating in the upper layer, which is approximately 0.5 m thick.
dc.title	ELECTRIC CURRENTS OF SALTATION IN WINDSAND FLUX
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070245

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