[1]YU Xiangxiang,LI Shengyu,MA Xuexi,et al.Spatial Variation of Grain-size Characteristics of Near Surface Aeolian Sand Transport Under Desert Highway Shelterbelt[J].Research of Soil and Water Conservation,2017,24(01):334-341.
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Spatial Variation of Grain-size Characteristics of Near Surface Aeolian Sand Transport Under Desert Highway Shelterbelt

References:
[1] 张正偲,董治宝.人工卵石床面风沙流粒度特征[J].中国沙漠,2014,34(3):639-644.
[2] 钱广强,董治宝,罗万银,等.巴丹吉林沙漠地表沉积物粒度特征及区域差异[J].中国沙漠,2011,31(6):1357-1364.
[3] 董玉祥,马骏.海岸横向沙脊表面风沙流结构粒度响应的野外观测研究[J].中国沙漠,2008,28(6):1022-1028.
[4] 何清,杨兴华,艾力,等.塔克拉玛干沙漠风蚀起沙观测研究:试验介绍与观测结果初报[J].中国沙漠,2011,31(2):315-322.
[5] 董玉祥,马骏.输沙量对海岸沙丘表面风沙流中不同粒径沙粒垂向分布的影响[J].中山大学学报:自然科学版,2009,48(3):102-108.
[6] 冯大军,倪晋仁,李振山.风沙流中沙粒粒度的垂直和水平分布特征[J].泥沙研究,2008(5):22-30.
[7] Wai D V D. Grain-size-selective aeolian sand transport on a nourished beach[J]. Journal of Coastal Research, 2000,16(3):896-908.
[8] Arens S M, Van Boxel J H, Abuodha J O Z. Changes in grain size of sand in transport over a foredune[J]. Earth Surface Processes & Landforms, 2002,27(11):1163-1175.
[9] Farrell E J, Sherman D J, Ellis J T, et al. Vertical distribution of grain size for wind blown sand[J]. Aeolian Research, 2012,7(140):51-61.
[10] 刘钰华,张纯.新疆防沙林带优化模式的研究[J].干旱区研究,1992,9(2):13-26.
[11] Wolfe S A, Nickling W G. The protective role of sparse vegetation in wind erosion[J]. Progress in Physical Geography, 1993,17(1):50-68.
[12] 刘千枝.景电灌区植被类型对风沙流结构的影响[J].甘肃林业科技,1997,22(3):13-17.
[13] 哈斯.腾格里沙漠东南缘沙丘表面风沙流结构变异的初步研究[J].科学通报,2004,49(11):1099-1104.
[14] 武建军,罗生虎,闫光虎,等.脉动风场下风沙流结构的数值模拟[J].中国沙漠,2011,31(3):602-606.
[15] 任春勇,武生智.沙源供给条件对风沙流结构的影响[J].中国沙漠,2011,31(3):597-601.
[16] Zhang K, Qu J, Zu R, et al. Characteristics of wind-blown sand on Gobi/mobile sand surface[J]. Environmental Geology, 2008,54(2):411-416.
[17] 王自龙,赵明,冯向东,等.民勤绿洲外围不同下垫面条件下风沙流结构的观测研究[J].水土保持学报,2009(4):72-75.
[18] 张克存,屈建军,俎瑞平,等.不同下垫面对风沙流特性影响的风洞模拟研究[J].干旱区地理,2004,27(3):352-355.
[19] 钟卫,孔纪名,杨涛.植被沙障对近地表风沙流特征影响的风洞实验[J].干旱区研究,2009,26(6):872-876.
[20] 汪季,胡志敏.近地表风沙流结构对不同植被覆盖度的响应[J].干旱区资源与环境,2005,19(5):30-33.
[21] 范冬冬,李生宇,雷加强,等.塔克拉玛干沙漠腹地高大复杂纵向沙垄区沙丘分形特征[J].干旱区地理,2009,32(6):941-947.
[22] 凌裕泉.塔克拉玛干沙漠的流场特征与风沙活动强度的关系[J].中国沙漠,1988,8(2):25-37.
[23] 杨兴华,何清,艾力,等.1996-2008年塔中地区的风沙环境特征[J].沙漠与绿洲气象,2010,4(2):21-25.
[24] 杨兴华,何清,艾力.塔克拉玛干沙漠塔中地区春夏季风蚀起沙研究[J].中国沙漠,2010,30(4):770-776.
[25] Wentworth C K. A scale of grade and class terms for clastic sediments[J]. The Journal of Geology, 1922,30(5):377-392.
[26] Folk R L. Brazos river bar:a study in the significance of grain size parameter[J]. Jour. Sediment Petrol, 1957,27(1):3-26.
[27] 徐满厚,刘彤,赵新俊,等.绿洲-荒漠交错带防护林与自然植被的协同防风效能及优化模式探讨[J].中国沙漠,2012,32(5):1224-1232.
[28] 刘芳,郝玉光,辛智鸣,等.乌兰布和沙漠东北缘地表风沙流结构特征[J].中国沙漠,2014,34(5):1200-1207.
[29] 王翠,李生宇,雷加强,等.近地表风沙流结构对过渡带不同下垫面的响应[J].水土保持学报,2014,28(3):52-56.
[30] Leys J, McTainsh G. Soil loss and nutrient decline by wind erosion-cause for concern[J]. Australian Journal of Soil and Water Conservation, 1994,7(3):30-35.
[31] Zobeck T M, Fryrear D W. Chemical and physical characteristics of windblown sediment I. Quantities and physical characteristics[J]. Transactions of the ASAE,1986,29(4):1032-1036.
[32] Dong Z, Liu X, Wang H, et al. The flux profile of a blowing sand cloud:a wind tunnel investigation[J]. Geomorphology, 2003,49(3):219-230.
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