Sidewall effects of a wind tunnel on wind velocity and mass flux in   aeolian sand transport

doi:10.1016/j.geomorph.2008.11.006

CORC > 北京大学 > 环境科学与工程学院

	Sidewall effects of a wind tunnel on wind velocity and mass flux in aeolian sand transport
	Feng, D. J. ; Li, Z. S. ; Ni, J. R.
刊名	geomorphology
	2009
关键词	Aeolian transport Wind tunnel Sidewall effects Wind velocity Mass flux SALTATION THRESHOLD PROFILES BEHAVIOR SLOPE AIR
DOI	10.1016/j.geomorph.2008.11.006
英文摘要	The sidewall effects of a wind tunnel on aeolian sand transport were investigated experimentally. A. wind tunnel was used to conduct the experiments with a given channel height of 120 cm and varying widths (B) of 40, 60, 80, 100 and 120 cm. Both vertical profiles of wind velocity and sand mass flux were measured at different locations across the test section. The results show that the wind velocity with saltation first increases and then decreases to a minimum, from the sidewall to the central line of the wind tunnel. The discrepancy among wind velocities at different locations of the transverse section decreases with decreasing tunnel width. The wind friction velocity across the wind tunnel floor, with the exception of the region closest to the sidewalls, does not deviate strongly in wide wind tunnels from that along the central line, whereas it does vary in narrow tunnels. The sand mass fluxes, with the exception of some near-bed regions, are larger along the central line of the wind tunnel than they are at the quarter width location from the sidewall. Unlikely previously reported results, the dimensionless sand transport rate, Qg/(rho p()(3)) (where Q is the total sand transport rate, g is the gravitational acceleration constant, p is the air density, and u() is the wind friction velocity), first decreases and then increases with the dimensionless friction velocity, u()/ u(t) (where u(t) is the threshold friction velocity). The above differences may be attributed to the sidewall effects of the wind tunnel. A dimensionless parameter. F(B) = u()/(gB)(1/2), is defined to reflect the sidewall effects on aeolian sand transport The flows with F(B) of 0.33 or less may be free from the sidewall effects of the wind tunnel and can ensure accurate saltation tunnel simulation. (C) 2008 Elsevier B.V. All rights reserved.; Geography, Physical; Geosciences, Multidisciplinary; SCI(E); 2; ARTICLE; 3-4; 253-260; 106
语种	英语
内容类型	期刊论文
源URL	[http://ir.pku.edu.cn/handle/20.500.11897/158522]
专题	环境科学与工程学院
推荐引用方式 GB/T 7714	Feng, D. J.,Li, Z. S.,Ni, J. R.. Sidewall effects of a wind tunnel on wind velocity and mass flux in aeolian sand transport[J]. geomorphology,2009.
APA	Feng, D. J.,Li, Z. S.,&Ni, J. R..(2009).Sidewall effects of a wind tunnel on wind velocity and mass flux in aeolian sand transport.geomorphology.
MLA	Feng, D. J.,et al."Sidewall effects of a wind tunnel on wind velocity and mass flux in aeolian sand transport".geomorphology (2009).