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Journal of Arid Land
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Journal of Arid Land  2017, Vol. 9 Issue (5): 743-752    DOI: 10.1007/s40333-017-0101-8
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Effects of wind guide plates on wind velocity acceleration and dune leveling: a case study in Ulan Buh Desert, China 
HAN Yanlong, GAO Yong*, MENG Zhongju, DANG Xiaohong, JIA Xu, DING Yanlong, LI Peng 
College of Desert Control Science and Engineering, Inner Mongolia Agricultural University, Huhhot 010018, China
Effects of wind guide plates on wind velocity acceleration and dune leveling: a case study in Ulan Buh Desert, China 
HAN Yanlong, GAO Yong*, MENG Zhongju, DANG Xiaohong, JIA Xu, DING Yanlong, LI Peng 
College of Desert Control Science and Engineering, Inner Mongolia Agricultural University, Huhhot 010018, China
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摘要 The areas used to be covered by shifting sand dunes have been reclaimed rapidly in recent years. However, it is a challenge to reclaim high sand dunes because it is rather costly to level the high dunes to gentle arable lands. In this study, a wind guide plate was used to change the characteristics of natural wind to level the sand dunes. The use of wind energy could significantly increase the efficiency of dune leveling and decrease the cost. Low wind velocity is a typical characteristic in Ulan Buh Desert of China where the average wind speed is much lower than the threshold velocity for sand movement. The experiment of this study was conducted to accelerate the wind velocity by a wind guide plate to level a sand dune. Results show that the threshold velocity for sand movement is 3.32 m/s at 10 cm above the sand surface in Ulan Buh Desert. A wind guide plate set at an angle less than 50° could significantly increase the wind velocity. The wind velocity could be accelerated up to the threshold velocity for sand movement behind a plate when the plate is at the angles of 20°, 25°, 35° and 40°. The most significant acceleration of wind velocity appears at 1.5 and 3.0 m behind the plate with an angle of 25°. An obvious wind velocity acceleration zone exists behind the wind guide plate when the angles are at 25°, 35°, 40° and 45°, with the most obvious zone under the angle of 45°. The results also show that the total amount of sand transferred over the experimental period increased by 6.1% under the effects of wind guide plates compared to the sand moved without wind guide plates. The results of the study will provide theoretical and practical supports for desert management in sand dune areas. 
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关键词wind guide plate   sand dune   dune leveling   wind velocity   sandy desert   Ulan Buh Desert      
Abstract: The areas used to be covered by shifting sand dunes have been reclaimed rapidly in recent years. However, it is a challenge to reclaim high sand dunes because it is rather costly to level the high dunes to gentle arable lands. In this study, a wind guide plate was used to change the characteristics of natural wind to level the sand dunes. The use of wind energy could significantly increase the efficiency of dune leveling and decrease the cost. Low wind velocity is a typical characteristic in Ulan Buh Desert of China where the average wind speed is much lower than the threshold velocity for sand movement. The experiment of this study was conducted to accelerate the wind velocity by a wind guide plate to level a sand dune. Results show that the threshold velocity for sand movement is 3.32 m/s at 10 cm above the sand surface in Ulan Buh Desert. A wind guide plate set at an angle less than 50° could significantly increase the wind velocity. The wind velocity could be accelerated up to the threshold velocity for sand movement behind a plate when the plate is at the angles of 20°, 25°, 35° and 40°. The most significant acceleration of wind velocity appears at 1.5 and 3.0 m behind the plate with an angle of 25°. An obvious wind velocity acceleration zone exists behind the wind guide plate when the angles are at 25°, 35°, 40° and 45°, with the most obvious zone under the angle of 45°. The results also show that the total amount of sand transferred over the experimental period increased by 6.1% under the effects of wind guide plates compared to the sand moved without wind guide plates. The results of the study will provide theoretical and practical supports for desert management in sand dune areas. 
Key wordswind guide plate   sand dune   dune leveling   wind velocity   sandy desert   Ulan Buh Desert    
收稿日期: 2016-12-28; 出版日期: 2017-07-03
基金资助:This study was supported by the National Key Technology Research and Development Program of the Ministry of Science and Technology of China (2015BAC06B00) and the Natural Science Foundation of the Inner Mongolia Autonomous Region of China (2014ZD03). 
通讯作者: GAO Yong      E-mail: 13948815709@163.com
引用本文:   
. Effects of wind guide plates on wind velocity acceleration and dune leveling: a case study in Ulan Buh Desert, China [J]. Journal of Arid Land, 2017, 9(5): 743-752.
. Effects of wind guide plates on wind velocity acceleration and dune leveling: a case study in Ulan Buh Desert, China [J]. Journal of Arid Land, 2017, 9(5): 743-752.
 
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[1] JIA Fengqin, Tashpolat TIYIP, WU Nan, TIAN Changyan, ZHANG Yuanming. Characteristics of soil seed banks at different geomorphic positions within the longitudinal sand dunes of the Gurbantunggut Desert, China[J]. Journal of Arid Land, 2017, 9(3): 355-367.
[2] ZHANG Yang, WANG Yuan, ZHOU Xiaosi, YANG Bin. Evolution of crescent-shaped sand dune under the influence of injected sand flux: scaling law and wind tunnel experiment[J]. Journal of Arid Land, 2017, 9(2): 270-277.
[3] ZHAN Kejie, LIU Shizeng, YANG Zihui, FANG Etian, ZHOU Lanping, HUANG Ning. Effects of sand-fixing and windbreak forests on wind flow: a synthesis of results from field experiments and numerical simulations[J]. Journal of Arid Land, 2017, 9(1): 1-12.
[4] LI Jinchang, LIU Haixia, SU Zhizhu, FAN Xiaohui. Changes in wind activity from 1957 to 2011 and their possible influence on aeolian desertification in northern China[J]. Journal of Arid Land, 2015, 7(6): 755-764.
[5] LANG Lili, WANG Xunming, WANG Guangtao, HUA Ting, WANG Hongtao. Effects of aeolian processes on nutrient loss from surface soils and their significance for sandy desertification in Mu Us Desert, China: a wind tunnel approach[J]. Journal of Arid Land, 2015, 7(4): 421-428.
[6] FeiLong HU, WenKai SHOU, Bo LIU, ZhiMin LIU, Carlos A BUSSO. Species composition and diversity, and carbon stock in a dune ecosystem in the Horqin Sandy Land of northern China[J]. Journal of Arid Land, 2015, 7(1): 82-93.
[7] JiLiang LIU, WenZhi ZHAO, FengRui LI. Shrub presence and shrub species effects on ground beetle assemblages (Carabidae, Curculionidae and Tenebrionidae) in a sandy desert, northwestern China[J]. Journal of Arid Land, 2015, 7(1): 110-121.
[8] QuanLai ZHOU, DeMing JIANG, ZhiMin LIU, Alamusa, XueHua LI, YongMing LUO, HongMe. The return and loss of litter phosphorus in different types of sand dunes in Horqin Sandy Land, northeastern China[J]. Journal of Arid Land, 2012, 4(4): 431-440.
[9] DaoYuan ZHANG, Xiang SHI, JianCheng WANG, HuiLiang LIU John F GASKIN. Breeding system and its consequence on fruit set of a rare sand dune shrub Eremosparton songoricum (Fabaceae: Papilionoideae): implications for conservation[J]. Journal of Arid Land, 2011, 3(4): 231-239.
[10] DaoYuan ZHANG, HuiLiang LIU, Xiang SHI, JianCheng WANG, YongKuan ZHANG. Limitations on the recruitment of the rare sand shrubby legume Eremosparton songoricum (Fabaceae) in Gurbantunggut Desert, China[J]. Journal of Arid Land, 2011, 3(2): 75-84.
[11] JianCheng WANG, Xiang SHI, DaoYuan ZHANG, LinKe YIN. Phenotypic plasticity in response to soil moisture availability in the clonal plant Eremosparton songoricum (Litv.) Vass.[J]. Journal of Arid Land, 2011, 3(1): 34-39.
[12] KeCun ZHANG, KenJi KAI, JianJun QU, YuQuan LING, QingHe NIU. Dynamic changes of a typical linear dune in the Tengger Desert[J]. Journal of Arid Land, 2010, 2(4): 272-278.
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