地理学报 ›› 2016, Vol. 71 ›› Issue (9): 1562-1570.doi: 10.11821/dlxb201609008
收稿日期:
2016-04-21
修回日期:
2016-06-22
出版日期:
2016-11-25
发布日期:
2016-11-25
作者简介:
作者简介:孙禹(1987-), 男, 吉林长春人, 博士生, 主要从事干旱区地貌与环境研究。E-mail:
基金资助:
Yu SUN1(), Huishi DU2, Eerdun HASI1(
), Meiping LIU1
Received:
2016-04-21
Revised:
2016-06-22
Published:
2016-11-25
Online:
2016-11-25
Supported by:
摘要:
风蚀坑是固定沙丘活化的标志,也是沙漠化的首要环节。本文利用三杯风速仪、风向标及阶梯式集沙仪,对浑善达克沙地南缘固定沙丘风蚀坑的气流及输沙进行了观测。结果表明,气流进入风蚀坑后,经历了扩散减速—辐合加速—分离减速—逐渐恢复的过程。入风方向的微小变化、地形及植被导致风蚀坑气流结构、强度及输沙模式趋于复杂。与轴线平行(< 10°)的纵向气流使侵蚀坑内减速区西移,风速及输沙率由坑底向两侧壁及积沙区增加;与轴线斜交(≥ 10°)的气流使减速区东移,气流沿两侧壁向东加速及输沙。积沙区顶部的气流汇集与植被的作用使其加积增高。气流—形态相互作用使风蚀坑加深和纵向延伸并伴随侧向扩展。
孙禹, 杜会石, 哈斯额尔敦, 刘美萍. 固定沙丘风蚀坑风沙动力学观测研究[J]. 地理学报, 2016, 71(9): 1562-1570.
Yu SUN, Huishi DU, Eerdun HASI, Meiping LIU. Aeolian dynamical process of blowout on the fixed dune[J]. Acta Geographica Sinica, 2016, 71(9): 1562-1570.
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