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篇目详细内容 |
【篇名】 |
Wind tunnel experiments of air flow patterns over nabkhas modeled after those from the Hotan River basin, Xinjiang, China (II): vegetated |
【刊名】 |
Frontiers of Earth Science in China |
【刊名缩写】 |
Front. Earth Sci. China |
【ISSN】 |
1673-7385 |
【EISSN】 |
1673-7490 |
【DOI】 |
10.1007/s11707-008-0020-2 |
【出版社】 |
Higher Education Press and Springer-Verlag |
【出版年】 |
2008 |
【卷期】 |
2
卷3期 |
【页码】 |
340-345
页,共
6
页 |
【作者】 |
LI Zhizhong;
WU Shengli;
DALE Janis;
GE Lin;
HE Mudan;
WANG Xiaofeng;
JIN Jianhui;
LIU Jinwei;
LI Wanjuan;
MA Rong;
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【关键词】 |
nabkhas; artificial vegetation; wind tunnel experiment |
【摘要】 |
This paper examines the results of wind tunnel experiments on models of nabkha, based on those studied in the Hotan River basin. Semi-spherical and conical models of nabkhas were constructed at a ratio of 40:1 in light of the on-site observation. Artificial vegetation of simulated Tamarix spp. was put on top of each model. Parameters of the shape, including height, width, and diameter of vegetated semi-spherical and conical nabkha, were measured in the Hotan River basin. Wind tunnel experiments on the semi-spherical and conical nabkha used clean air devoid of additional sediments at five different wind speeds (6–14 m/s) to study the influence of vegetation on airflow patterns. Results of the experiments indicate that vegetation at the top of the nabkhas enhances the surface roughness of the sand mounds, retards airflow over the sand mounds, reduces airflow energy, eliminates erosional pits occurring on the top surface of non-vegetated sand mounds and enhances the range of influence of the vortex that forms on the leeward slope. Vegetation changes the airflow pattern upwind and downwind of the sand mound and reduces the transport of sand away from the nabkha. This entrapment of sediment by the vegetation plays an important role in sustaining the nabkha landscape of the study area. The existence of vegetation makes fine materials in wind-sand flow to possibly deposit, and promotes nabkha formation. The imitative flow patterns of different morphological nabkhas have also been verified by on-site observation in the river basin. |
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