敦煌鸣沙山金字塔沙丘的形成模式研究  

THE STUDY ON THE MODEL FOR PYRAMID DUNE FORMATION IN THE MINGSHA MOUNTAIN, DUNHUANG CITY

作　　者：胡世雄[1] 吴正[1] 

机构地区：[1]中国科学院,国家计划委员会地理研究所,华南师范大学地理系

出　　处：《地理研究》1997年第1期60-67,共8页Geographical Research

基　　金：国家自然科学基金

摘　　要：选择敦煌鸣沙山地区金字塔沙丘作为研究对象，在前人研究的基础上，采用实地考察与观测资料相结合的方法，从分析金字塔沙丘形成的条件入手，通过野外流场观测及室内风洞模拟实验，建立了金字塔沙丘形成的区域动力模式。The forming mechanism and the model for pyramid dune formation were not fully studied. In this paper . the forming conditions of pyramid dunes are analysed , and a regional model is estab- lished based on the observation of airflow and the experiment in wind-tunnel. The forming conditions of pyramid dune include : a rich sand source and a wind regime which contains three or more directions which have similar windforces. The mountain-valley wind resulted from local landforms is one of main factors that cause the changable wind directions. The forming mechanism of Pyramid dune can be inferred from the air flow analysis and the ex- periment in wind-tunnel. Under the changeable wind directions in one season , a barchan appears firstly ; then , the em- bryo-pyramid dune emerges , which embodys three slip-faces and three tounge-shaped protrudings between them. With the three-direction winds modifying alternatively from season to season , a cross-axis eddy result in the lee-side and inclined helical eddies to form at the slope turn , which take sands from lee-side to slope turn and transport some of them upslope simultanneously. Finally , ma- ture pyramid dune arises , which is made up of a pyramid top , three sharp ridges and three concave slopes. Sometimes , the pyramid dune may break down and become a barchan when the wind blows to- ward one of its slopes .continously for a very long period.

关 键 词：敦煌鸣沙山 金字塔沙丘 沙丘形成模式 沙丘 

分 类 号：P931.3[天文地球—自然地理学]