[1] Palchan D,Stein M,Almogi-Labin A,et al.Dust transport and synoptic conditions over the Sahara-Arabia deserts during the MIS6/5 and 2/1 transitions from grain-size,chemical and isotopic properties of Red Sea cores[J].Earth & Planetary Science Letters,2013,382(6):125-139. [2] Zhu B,Yu J.Aeolian sorting processes in the Ejina desert basin (China) and their response to depositional environment[J].Aeolian Research,2014,12(2):111-120. [3] Zhu B Q,Yu J J,Rioual P,et al.Particle size variation of aeolian dune deposits in the lower reaches of the Heihe River basin,China[J].Sedimentary Geology,2014,301(3):54-69. [4] Flood R P,Orford J D,Mckinley J M,et al.Effective grain size distribution analysis for interpretation of tidal-deltaic facies:West Bengal Sundarbans[J].Sedimentary Geology,2015,318:58-74. [5] 陈渭南,董治宝,杨佐涛,等.塔克拉玛干沙漠的起沙风速[J].地理学报,1995,50(4):360-367. [6] 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):18-22. [7] 钱亦兵,吴兆宁,杨海峰,等.古尔班通古特沙漠南部风沙土粒度分布的空间异质性[J].干旱区地理,2009,32(5):655-661. [8] 唐进年,王继和,苏志珠,等.库姆塔格沙漠羽毛状沙丘表面沙粒度分布特征[J].干旱区地理,2008,31(6):918-925. [9] Qiao Y S,Guo Z T,Hao Q Z,et al.Grain-size features of a Miocene loess-soil sequence at Qinan:Inplications on its origin[J].Science in China:Series D Earth Sciences,2006,49(7):731-738. [10] 汪海斌,陈发虎,张家武.黄土高原西部地区黄土粒度的环境指示意义[J].中国沙漠,2002,22(1):21-26. [11] Robert Louis Folk,William C.Ward.Brazos River Bar:a study in the significance of grain size parameters[J].Journal of Sedimentary Research,1957,27:3-26. [12] 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):215-220. [13] 李森,孙武,李孝泽,等.浑善达克沙地全新世沉积特征与环境演变[J].中国沙漠,1995,15(4):323-331. [14] MartíNez-Mena M,Castillo V,Albaladejo J.Relations between interrill erosion processes and sediment particle size distribution in a semiarid Mediterranean area of SE of Spain[J].Geomorphology,2002,45(3):261-275. [15] Hamdan M A,Refaat A A,Anwar E A,et al.Source of the aeolian dune sand of Toshka area,southeastern Western Desert,Egypt[J].Aeolian Research,2014,17:275-289. [16] Dong G R,Wang G Y,Li X Z,et al.Palaeomonsoon vicissitudes in eastern desert region of China since last interglacial period[J].Science in China (Series D),1996,41(2):215-224. [17] 孙继敏,丁仲礼.中国东部沙区的荒漠化过程与起因[J].第四纪研究,1998(2):156-164. [18] 黄杏珍,潘中海.应用粒度资料探讨毛乌素沙漠西南部的风砂特征[J].地理学报,1981,36(1):70-78. [19] 李智佩,岳乐平,薛祥煦,等.毛乌素沙地东南部边缘不同地质成因类型土地沙漠化粒度特征及其地质意义[J].沉积学报,2006,24(2):267-275. [20] 苏永中,赵哈林,文海燕.退化沙质草地开垦和封育对土壤理化性状的影响[J].水土保持学报,2002,16(4):5-8. [21] 曹振,胡克,张永光,等.科尔沁沙地地表沉积物粒度分析与可风蚀性讨论[J].中国沙漠,2005,25(1):15-19. [22] 张洪,靳鹤龄,苏志珠,等.全新世浑善达克沙地粒度旋回及其反映的气候变化[J].中国沙漠,2005,25(1):1-7. [23] 吴霞,哈斯,杜会石,等.库布齐沙漠南缘抛物线形沙丘表面粒度特征[J].沉积学报,2012,30(5):937-944. [24] Han G,Zhang G F,Yang W B,et al.A Quantitative analysis on the sources of dune sand in the Hulun Buir Sandy Land:application of the stepwise discriminant analysis (SDA) to the granulometric data[J].Journal of Geographical Sciences,2004,14(2):177-186. [25] 董建林,雅洁.呼伦贝尔沙地近十年来土地沙漠化变化分析[J].林业资源管理,2002,(4):39-43. [26] 刘树林,王涛.浑善达克沙地的土地沙漠化过程研究[J].中国沙漠,2007,27(5):719-724. [27] 刘海霞,李晋昌,苏志珠,等.毛乌素沙地西南缘灌丛沙丘沉积物的粒度和元素特征[J].中国沙漠,2015,35 (1):24-31. [28] 包小庆,陈渠昌.库布齐沙漠侵蚀状况及治理构想[J].水土保持研究,1998,5(3):26-29. [29] 马娜,胡云锋,庄大方,等.基于遥感和像元二分模型的内蒙古正蓝旗植被覆盖度格局和动态变化[J].地理科学,2012,32(2):251-256. [30] Folk R L,Ward W C.Brazos River Bar:A study in the significance of grain size parameters[J].Journal of Sedimentary Petrology,1957,27(1):3-26. [31] 哈斯.腾格里沙漠东南缘格状沙丘粒度特征与成因探讨[J].地理研究,1998,17(2):178-184. [32] 陈渭南.塔克拉玛干沙漠84°E沿线沙物质的粒度特征[J].地理学报,1993,48(1):33-46. [33] 李志忠,关有志,孙忠,等.塔克拉玛干沙漠腹地纵向沙垄的粒度分布特征[J].干旱区研究,1996,13(2):37-43. [34] 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. |