Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2008, Vol. 28 Issue (1): 16-20    DOI:
沙漠与沙漠化     
Wind Tunnel Simulation on Flow Reattachment on Lee of Transverse Dunes
QIAN Guang qiang; DONG Zhi bao; LUO Wan yin; WANG Hong tao
Key Laboratory of Desert and Desertification, Chinese Academy of Sciences; Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Download:  PDF (747KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  Secondary airflow plays an important role in dune initiation and form maintenance. Airflow speeding\|up over the stoss slope and separating at the crest were described and mentioned widely in the dune dynamic researches. Secondary airflow in the lee side of dune, especially the flow separation (i.e. reversal vortex) and the reattachment, has an important significance in shaping the lee slope and in controlling the dune spacing and alignment. In this paper, a series experiments were conducted in a wind tunnel using Particle Image Velocimetry (PIV) to study the factors in controlling flow reattachment in the lee side of transverse dunes. The results showed that the flow reattachment distance in the lee side of various dune models are ranged from 4\^8H to 10\^8H (H is dune height) depending on different stoss slopes, the maximum of flow reattachment distance was found in the lee side of the transverse dune with a 15° stoss slope angle. The stoss slope angles have more influence in controlling the flow reattachment than free stream velocities. Finally, the sedimentary significance of the flow separation and the reattachment was discussed in detail.
Key words:  transverse dune      secondary airflow      lee\|side of a dune      flow reattachment      Particle Image Velocimetry     
Received:  01 November 2006      Published:  20 January 2008
ZTFLH:  X169:P931.3  

Cite this article: 

QIAN Guang qiang;DONG Zhi bao;LUO Wan yin;WANG Hong tao. Wind Tunnel Simulation on Flow Reattachment on Lee of Transverse Dunes. JOURNAL OF DESERT RESEARCH, 2008, 28(1): 16-20.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2008/V28/I1/16

[1]董治宝,王涛,屈建军. 100 a来沙漠科学的发展[J].中国沙漠,2003,23(1):1-5.
[2]董治宝.中国风沙物理研究50年(I)[J].中国沙漠,2005,25(3):293-305.
[3]哈斯,董光荣,王贵勇.腾格里沙漠东南缘沙丘表面气流与坡面形态的关系[J].中国沙漠,1999,19(1):1-4.
[4]张春来,郝青振,邹学勇,等.新月形沙丘迎风坡形态及沉积物对表面气流的响应[J].中国沙漠,1999,19(4):359-363.
[5]李恒鹏,陈广庭,李波.新月形沙丘迎风坡气流加速模拟[J].中国沙漠,2001,21(1):24-27.
[6]Frank A,Kocurek G.Towards a model of airflow on the lee side of aeolian dunes [J].Sedimentology,1996,43:451-458.
[7]Walker I,Nickling W G.Simulation and measurement of surface shear stress over isolated and closely spaced transverse dune in a wind tunnel [J].Earth Surface Processes and Landforms,2003,28:1111-1124.
[8]Wiggs G F S,Livingstone I,Warren A.The role of streamline curvature in sand dune dynamics:evidence from field and wind tunnel measurements [J].Geomorphology,1996,17:29-46.
[9]Hoyt J.Air and sand movements to the lee of dunes [J].Sedimentology,1966,7:137-43.
[10]Walker I,Nickling W G.Dynamics of secondary airflow and sediment transport over and in the lee of transverse dunes [J].Progress in Physical Geography,2002,26(1):47-75.
[11]Sweet M L,Kocurek G.An empirical model of aeolian dune lee-face airflow [J].Sedimentology,1990,37:1023-1038.
[12]Parsons D,Walker I,Nickling W G.Numerical modeling of flow structures over idealized transverse aeolian dunes of varying geometry [J].Geomorphology,2004,59:149-164.
[13]吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2003:1-448.
[14]Lancaster N.Geomorphology of Desert Dunes [M].London:Routledge,1995:1-290.
[15]Nickling W G,McKenna Neuman C K,Lancaster N.Grainfall processes in the lee of transverse dunes,Silver Peak,Nevada [J].Sedimentology,2002,49:191-209.
No Suggested Reading articles found!