Effect of flexible and rigid roughness elements on aeolian sand transport

被引:20
作者
Abulaiti, Abulitipu [1 ]
Kimura, Reiji [1 ]
Kodama, Yoshinori [2 ]
机构
[1] Tottori Univ, Arid Land Res Ctr, Hamasaka 1390, Tottori 6800001, Japan
[2] Tottori Univ, Fac Reg Sci, Tottori, Japan
关键词
Actual frontal area; arid regions; flexibility; vegetative roughness; wind tunnel; ATMOSPHERIC INERTIAL SUBLAYER; VEGETATION COVER; WIND EROSION; SEDIMENT TRANSPORT; SPARSE VEGETATION; DRAG PARTITION; LARGE PATCHES; FOREST EDGE; NEW-MEXICO; DESERT;
D O I
10.1080/15324982.2016.1260665
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In developing countermeasures to reduce the negative effects of strong dust events, the fundamental relationship between surface conditions and sand transport remains problematic. We conducted field observations and wind tunnel experiments to examine the effect on sand transport efficiency of actual frontal area when using flexible roughness elements (artificial grass) and rigid roughness elements (tufts of stiff wire). In the field observations, the sand trap ratio approached a limit as the frontal area of artificial grass, measured as the Actual Frontal Area Index (AFAI), approached 25%, equivalent to a vegetation cover of 20%. The wind tunnel experiments showed that the height of deposited sediment decreased downwind with both roughness elements, due to their reduction of both shear velocity and sand transport rates. The sediment flux decreased as the AFAI increased, and the rigid roughness element trapped more sand particles than the flexible one except at higher wind speeds and lower AFAI values. The sand trapping efficiency was greater for rigid roughness elements than for flexible ones, probably due to their high aerodynamic resistance, and thus wire tufts were more effective for trapping sand than artificial grass at higher AFAI values.
引用
收藏
页码:111 / 124
页数:14
相关论文
共 50 条
[1]  
Abulaiti A., 2012, J. Arid l. Study, V22, P427
[2]  
Abulitipu A., 2011, SAND DUNE RES, V58, P31
[3]  
Allgaier A., 2008, V200, P211
[4]  
[Anonymous], 2013, Sand Dune Res.
[5]  
[Anonymous], MONGOLIAN POPULATION
[6]   Analysis of a Severe Dust Storm Event over China: Application of the WRF-Dust Model [J].
Bian, Hai ;
Tie, Xuexi ;
Cao, Junji ;
Ying, Zhuming ;
Han, Suqin ;
Xue, Yong .
AEROSOL AND AIR QUALITY RESEARCH, 2011, 11 (04) :419-428
[7]   THE EFFECT OF SPARSE VEGETATION ON THE TRANSPORT OF DUNE SAND BY WIND [J].
BUCKLEY, R .
NATURE, 1987, 325 (6103) :426-428
[8]   Predicting wind erodibility of loessial soils in the pacific northwest by particle sizing [J].
Chandler, DG ;
Saxton, KE ;
Busacca, AJ .
ARID LAND RESEARCH AND MANAGEMENT, 2005, 19 (01) :13-27
[9]   GROWING-SEASON MICROCLIMATIC GRADIENTS FROM CLEAR-CUT EDGES INTO OLD-GROWTH DOUGLAS-FIR FORESTS [J].
CHEN, JQ ;
FRANKLIN, JF ;
SPIES, TA .
ECOLOGICAL APPLICATIONS, 1995, 5 (01) :74-86
[10]  
Chung Y S., 2003, Wat. Air. Soil Poll, V3, P21, DOI DOI 10.1023/A:1023261717206