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Titlebook: Aeolian Grain Transport 1; Mechanics Ole E. Barndorff-Nielsen,Brian B. Willetts Conference proceedings 1991 Springer-Verlag Wien 1991 Sedim

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期刊全稱(chēng)Aeolian Grain Transport 1
期刊簡(jiǎn)稱(chēng)Mechanics
影響因子2023Ole E. Barndorff-Nielsen,Brian B. Willetts
視頻videohttp://file.papertrans.cn/151/150460/150460.mp4
學(xué)科分類(lèi)Acta Mechanica. Supplementa
圖書(shū)封面Titlebook: Aeolian Grain Transport 1; Mechanics Ole E. Barndorff-Nielsen,Brian B. Willetts Conference proceedings 1991 Springer-Verlag Wien 1991 Sedim
影響因子Wind erosion has such a pervasive influence on environmental and agricultural matters that academic interest in it has been continuous for several decades. However, there has been a tendency for the resulting publications to be scattered widely in the scientific litera- ture and consequently to provide a less coherent resource than might otherwise be hoped for. In particular, cross-reference between the literature on desert and coastal morphology, on the deterioration of wind affected soils, and on the process mechanics of the grain/air- flow system has been disappointing. A successful workshop on "The Physics of Blown Sand", held in Aarhus in 1985, took a decisive step in collecting a research community with interests spanning geomorphology and grain/wind process mechanics. The identification of that Community was reinforced by the Binghampton Symposium on Aeolian Geomorphology in 1986 and has been fruitful in the development of a number of international collaborations. The objectives of the pre- sent workshop, which was supported by a grant from the NATO Scientific Affairs Division, were to take stock of the progress in the five years to 1990 and to extend the scope of the commun
Pindex Conference proceedings 1991
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Thomas Reichmann,Alfred Vo?schulte obtain explicit analytic expressions, approximations are made in all of the three subprocesses constituting the model: the trajectory model, the wind modification model, and the grain-bed collision model. Explicit formulae are derived for the transport rate and for the flux of grains from the bed i
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https://doi.org/10.1007/978-3-658-18380-6ere made at one second intervals to assess mass-flux response to velocity variations. Resulting grain flux and velocity series demonstrate the variability concealed by conventional time-averaged data. In steady tunnel winds, time-dependent mass transport rates are found to correlate better with fluc
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Prospects of the further development of EISquilibrium boundary layer over a rough bed with saltation may bias the wind gradient measurements, especially in short wind tunnels. Other discrepancies may be due to transient transport conditions caused by changes in bed texture and grain size composition. Wind profile data show that the aerodynam
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