沙漠与沙漠化 |
|
|
|
|
Study on Wind-tunnel Simulated Flow Pattern over Nabkha Dunes in Hetian River Basin, Xinjiang (Ⅱ) |
LI Zhi-zhong1, WU Sheng-li1,2, XIAO Chen-xi1, LIU Li-mei1, SUN Qiu-mei1, ZHANG Zhong-hua1 |
1.School of Life and Environmental Sciences, Xinjiang Normal University, Urumqi 830054, China; 2.School of Resources and Environmental Sciences, East China Normal University, Shanghai 200062, China |
|
|
Abstract In this paper, two models of nabkhas were made in 40:1 proportion in wind tunnel, according to similarity theory in wind-sand movement experiments, and on the base of nabkhas data surveyed in the Hetian river basin in Xinjiang. The airflow patterns over the semispherical and the conical models were simulated under pure wind with speed of 6, 8, 10, 12, 14 m\5s-1 separately. Experimental results showed that plants at the top of sand mounds can enhance the roughness of sand surface, reduce airflow energy and retard airflow to get over the sand mounds, and can eliminate the eroded region by strong wind that appeared commonly on bare sand mounds, and reinforce the influencing range of vortex at leeward side. Consequently, the structural characters of wind-sand flow in front of and behind the sand mounds must change. Therefore, the vegetation on sand mounds is benefit to hold flowing dust and sand, and to promote dunes to be accumulated. Vegetation has played a very important role in the course of nabkhas development.
|
Received: 12 September 2005
Published: 20 January 2007
|
|
[1]Cook R C,Warren A,Goudie A S.Desert Geomorphology[M].Gower Street,London WC1E 6BT:UCL Press Limited,University College London,1993. [2]朱震达,陈治平,吴正,等.塔克拉玛干沙漠风沙地貌研究[M].北京:科学出版社,1981. [3]Pye K,Tsoar H. Aeolian Sand and Dunes[M].15/17 Broadwick Street,London W1V 1FP,UK:Unwin Hyman Ltd,1990. [4]Nickling W G,Wolfe S A.The morphology and origin of Nabkhas,region of Mopti,Mali,West Africa[J].Journal of Arid Environments,1994,28:13-30. [5]Mares M A.Encyclopedia of Deserts[M].Norman: University of Oklahoma Press,1999:189. [6]吴正.风沙地貌与治沙工程学[M].北京:科学出版社,2003:163,400-404. [7]王涛.中国沙漠与沙漠化[M].石家庄:河北科学技术出版社,2003:404-405. [8]朱震达,陈广庭.中国土地沙质荒漠化[M].北京:科学出版社,1994:24. [9]何兴东,高玉宝,任安芝.风沙干扰在濒危植物柽柳群落形成演变过程中的作用[J].植物学报,2003,45(11):1285-1290. [10]岳兴玲,哈斯,庄燕美,等.沙质草原灌丛沙堆研究综述[J].中国沙漠,1996,16(4):360-363. [11]Hesp P A.The formation of shadow dunes[J].Journal of Sedimentary Petrology,1981,51:101-112. [12]Arens S M.Patterns of sand transport on vegetated foredunes[J].Geomorphology,1996,17:339-350. [13]Tengberg A,Cheng Deliang.A comparative analysis of nebkhas in central Tunisia and northern Burkina Faso[J].Geomorphology,1998,22:181-192. [14]Hesp P,McLachlan A.Morphology,dynamics,ecology and fauna of Arctotheca populifolia and Gazania rigens nabkha dunes[J]. Journal of Arid Environments,2000, 44:155-172. [15]Khalaf F I,Misak R,Al-Dousari A.Sedimentological and morphological characteristics of some nabkha deposits in the northern coastal plain of Kuwait,Arabia[J].Arid Environment,1995,29:267-292. [16]刘贤万.实验风沙物理与风沙工程学[M].北京:科学出版社,1995:66-68. [17]刘千枝.井电灌区植被类型对风沙流结构的影响[J].甘肃林业科技,1997(3):13-18. [18]韩致文,董治宝. 塔克拉玛干沙漠风沙运动若干特征观测研究[J].中国科学(D辑),2003,33(3):255-264. [19]刘小平,董治宝.砾石床面的空气动力学粗糙度[J].中国沙漠,2003,23(1):38-46. [20]胡孟春,赵爱国,李农.沙坡头铁路防护体系阻沙效益风洞实验研究[J].中国沙漠,2002,22(6):598-602. [21]刘小平,董治宝.直立植被粗糙度和阻力分解的风洞实验研究[J].中国沙漠,2002,22(1):82-88. [22]李志忠,关有志.纵向沙丘和横向沙丘模拟流场的实验研究[J].中国沙漠,1996,16(4):360-363. [23]李志忠,陈广庭.金字塔沙丘风洞流场结构的实验研究——兼论金字塔沙丘的发育模式[J].中国沙漠,1995,15(3):227-233. [24]李恒鹏,陈广庭.新月形沙丘迎风坡气流加速模拟[J].中国沙漠,2001,21(1):24-28. [25]王洪涛,董治宝.关于风沙流中风速廓线的进一步实验研究[J].中国沙漠,2003,23(6):721-72. [26]吕萍,董治宝.戈壁风蚀面与植被覆盖面地表性质粗糙度长度的确定[J].中国沙漠,2004,24(3):279-284. [27]董治宝,Fryrear D W,高尚玉.直立植物防沙措施粗糙特征的模拟实验[J].中国沙漠,2000,20(3):260-264. [28]Hesp P.Morphodynamics of incipient foredunes in New South Wales,Australia[C]//Brookfield M E,Ahlbrandt T S.Aeolian Sediments and Processes.Amsterdam:Elsevier,1983:325-342. [29]Wasson R J,Nanninge P M.Estimating wind transport of on vegetated surfaces[J].Earth Surface and Landforms,1986,11(5):505-514. [30]凌裕泉,屈建军.稀疏天然植被对输沙量的影响[J].中国沙漠,2003,23(1):12-18. |
No Suggested Reading articles found! |
|
|
Viewed |
|
|
|
Full text
|
|
|
|
|
Abstract
|
|
|
|
|
Cited |
|
|
|
|
|
Shared |
|
|
|
|
|
Discussed |
|
|
|
|