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格状沙障内风速波动特征初步研究
引用本文:张克存,屈建军,董治宝,俎瑞平,方海燕. 格状沙障内风速波动特征初步研究[J]. 干旱区研究, 2006, 23(1): 93-97
作者姓名:张克存  屈建军  董治宝  俎瑞平  方海燕
作者单位:中国科学院寒区旱区环境与工程研究所,沙漠与沙漠化重点实验室,甘肃,兰州,730000;中国科学院寒区旱区环境与工程研究所,沙漠与沙漠化重点实验室,甘肃,兰州,730000;中国科学院寒区旱区环境与工程研究所,沙漠与沙漠化重点实验室,甘肃,兰州,730000;中国科学院寒区旱区环境与工程研究所,沙漠与沙漠化重点实验室,甘肃,兰州,730000;中国科学院寒区旱区环境与工程研究所,沙漠与沙漠化重点实验室,甘肃,兰州,730000
基金项目:中国科学院知识创新工程项目 , 中国科学院知识创新工程项目
摘    要:通过对不同孔隙度格状沙障内风沙流中风速波动特征研究发现:风沙流中各高度层风速波动具有很好的相关性,其波动幅度随孔隙度的增加而减小;瞬时风速在时间序列上波动的均一性随不同高度间距离增加呈递减趋势;瞬时风速的波动性一方面受下垫面性质及外在环境条件的影响,另一方面与其所在高度层沙粒数量和运动状态有关.

关 键 词:格状沙障  孔隙度  风速波动
文章编号:1001-4675(2006)01-0093-05
收稿时间:2005-03-23
修稿时间:2005-03-232005-06-09

Preliminary Research on Fluctuation Characteristics of Wind Speed over Checkerboard Sand Barriers
ZHANG Ke-cun,QU Jian-jun,DONG Zhi-bao,ZU Rui-ping,FANG Hai-yan. Preliminary Research on Fluctuation Characteristics of Wind Speed over Checkerboard Sand Barriers[J]. Arid Zone Research, 2006, 23(1): 93-97
Authors:ZHANG Ke-cun  QU Jian-jun  DONG Zhi-bao  ZU Rui-ping  FANG Hai-yan
Affiliation:Key Laboratory of Desert and Desertification Control, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
Abstract:In this paper, an experimental study on fluctuation characteristics of wind speed within blowing sand flow over the Nylon checkerboard sand barriers with different porosities in wind tunnel in carried out. The experimental wind tunnel is 21 m in length and 1.2 m in width and height. The sampling heights are 1.0, 1.5, 3.0, 6.0, 12.0, 20.0, 35.0 and 50.0 cm respectively, and the temporal alternation of data collection is 2 seconds. However, the temporal alternation of data collection is a little long due to the instrument limitation, and the distribution of different sand barriers is simplex. Especially, the effects of porosity, pore shape, density and height of sand barriers on fluctuation of wind speed and transported sand amount need to be further researched using exacter instrument. The study results reveal that the fluctuation of wind speed over sand barriers is highly correlated with the height of blowing sand flow because the features of underlaying surface play an important role in affecting the energy of blowing sand flow; the fluctuation of wind speed is decreased with the increase of porosity of sand barriers; simultaneity of fluctuation of the instantaneous wind speed at deferent heights is decreased with the increase of the space between different heights; fluctuation of the instantaneous wind speed is affected by both underlying surface and environmental conditions, and is also related to wind-carried sand amount and movement status.
Keywords:checkerboard sand barrier   porosity   wind speed fluctuation.
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