[1]尹念文,魏玉涛.月牙泉的成因分析[J].地下水,2010,32(2):22-22.[2]丁宏伟,龚开诚.敦煌月牙泉湖水位持续下降原因及对策分析[J].水文地质工程地质,2004,6:74-77.[3]张伟民,王涛.巴丹吉林沙漠高大沙山形成演化初步探讨[J].中国沙漠,2005,25(2):281-286.[4]孙显科,吕亚军,张大治,等.风成沙地地形1/10定律的研究与敦煌鸣沙山成因的猜想[J].中国沙漠,2006,26(5):704-710.[5]桑吉梅朵.保卫沙漠第一泉——甘肃敦煌月牙泉抢救纪实[J].生态经济,2005,3:14-21.[6]董霁红,卞正富.敦煌市鸣沙山月牙泉自然遗产保全的研究[J].自然资源学报,2004,19(5):561-567.[7]温国盛.敦煌风景区风沙活动的初步研究[J].内蒙古林学院学报,1990,2:49-54.[8]Bullard J E.A note on the use of the “Fryberger method” for evaluating potential sand transport by wind[J].Journal of Sedimentary Research,1997,67:499-501.[9]Thomas D S G.The nature and deposition setting of arid and semi-arid Kalahari sediments,southern Africa[J].Journal of Arid Environments,1988,14:17-26.[10]柳本立,张伟民,刘小宁,等.莫高窟顶戈壁偏东风作用下输沙率变化的观测研究[J].中国沙漠,2010,30(3):516-521.[11]Wasson R J,Hyde R.Factors determining desert dune type[J].Nature,1983,304:337-339.[12]Wasson R J,Hyde R.A test of granulometric control of desert dune geometry[J].Earth Surface Processes and Landforms,1983,8:301-312.[13]Lancaster N.The dynamics of star dunes:An example from the Gran Desierto,Mexico[J].Sedimentology,1989,36:273-289.[14]Livingstone I,Warren A.Aeolian geomorphology—an introduction [M].London:Addison Wesley Longman Limited,1996.[15]张克存,俎瑞平,屈建军,等.腾格里沙漠东南缘输沙势与最大可能输沙量之比较[J].中国沙漠,2008,28(4):605-610.[16]李晋昌,苏志珠,胡光印.风沙活动强度的常用判断指标及其应用评述[J].中国沙漠,2010,30(4):788-795.[17]李红军,杨青,何清.近40年来新疆输沙势的分析[J].中国沙漠,2004,24(6):706-710.[18]张华,李锋瑞,李玉霖,等.科尔沁沙地奈曼旗近5年来风况及合成输沙势[J].中国沙漠,2004,24(5):623-627.[19]黄翠华,张伟民,李爱敏.莫高窟窟顶风况及输沙势研究[J].中国沙漠,2006,26(3):394-398.[20]张克存,牛清河,屈建军,等.青藏铁路沱沱河路段风沙危害特征及其动力环境分析[J].中国沙漠,2010,30(5):1006-1011.[21]Fryberger S G.Dune form and wind regime[C]//McKee E D.A Study of Global Sand Seas.US Geological Survey Professional Paper 1052,1979:137-169.[22]Lettau K,Lettau H.Experimental and micrometeorological field studies of dune migration[C]//Lettau K,Lettau H.Exploring the Worlds Driest Climate.University of Wisconsin-Madison,IES Report 101,1977:110-147. |