[1] Bagnold.The Physics of Blown Sand and Desert Dunes[M].London,UK:Methuen,1941:65-70. [2] Marticorena B,Berganmetti G.Modeling the atmospheric dust cycle:1.Design of a soil-derived dust emission scheme[J].Journal of Geophysical Research,1995,100(D8):16415-16430. [3] Shao Y.A model for mineral dust emission[J].Journal of Geophysical Research,2001,106(D17):20239-20254. [4] Dong Z B,Liu X P,Wang H T,et al.Aeolian sand transport:wind tunnel model[J].Sedimentary Geology,2003,161(1/2):71-83. [5] Mei F M,Zhang X Y,Lu H Y,et al.Characterization of MASDs of surface soils in north China and its influence on estimating dust emission[J].Chinese Science Bulletin,2004,49(20):2169-2175. [6] 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,1981:8-18. [7] 哈斯,王贵勇.腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系[J].中国沙漠,1996,16(3):216-221. [8] 钱亦兵,周兴佳,吴兆宁.准噶尔盆地沙物质粒度特征研究[J].干旱区研究,2000,17(2):34-41. [9] Wang X M,Dong Z B,Zhang J W,et al.Grain size characteristics of dune sands in the central Taklimakan Sand Sea[J].Sedimentary Geology,2003,161(1/2):1-14. [10] 李智佩,岳乐平,薛祥熙,等.毛乌素沙地东南缘不同地质成因类型土地沙漠化粒度分布特征及其地质意义[J].沉积学报,2006,24(2):267-276. [11] 何清,杨兴华,霍文,等.库姆塔格沙漠粒度分布特征及环境意义[J].中国沙漠,2009,29(1):18-23. [12] 张正偲,董治宝.土壤风蚀对表层土壤粒度特征的影响[J].干旱区资源与环境,2012,26(12):86-89. [13] 张号,张克存,安志山,等.敦煌月牙泉景区沙丘粒度特征[J].中国沙漠,2014,34(3):645-649. [14] 李超,董治宝,崔徐甲.腾格里沙漠东南缘不同发育阶段横向沙丘粒度分布特征[J].中国沙漠,2015,35(1):129-135. [15] Chatenet B,Marticorena B,Gomes L,et al.Assessing the microped size distrbutions of desert soils erodible by wind[J].Seimentology,1996,43:901-911. [16] Blott S J,Kenneth P.Particale size distributin analysis of sand-sized particles by laser diffraction:an experimental investigation of instrument sensitivity and the effects of particle shape[J].Sedimentology,2006,53:671-685. [17] 梅凡民.中国北方典型区域风蚀粉尘释放的实验观测和数值模拟研究[M].西安:西北工业大学出版社,2013. [18] Stefano C D,Ferro V,Mirabile S.Comparison between grain-size analyses using laser diffraction and sedimentation methods[J].Biosystems Enginerring,2010,106(2):205-215. |