Numerical simulation study of a tree windbreak

被引:51
作者
Bitog, Jessie P. [1 ,2 ,3 ]
Lee, In-Bok [1 ,2 ]
Hwang, Hyun-Seob [1 ,2 ]
Shin, Myeong-Ho [4 ]
Hong, Se-Woon [1 ,2 ]
Seo, Il-Hwan [1 ,2 ]
Kwon, Kyeong-Seok [1 ,2 ]
Mostafa, Ehab [1 ,2 ,5 ]
Pang, Zhenzhen [1 ,2 ,6 ]
机构
[1] Seoul Natl Univ, Coll Agr & Life Sci, Dept Rural Syst Engn, Seoul 151921, South Korea
[2] Seoul Natl Univ, Coll Agr & Life Sci, Res Inst Agr & Life Sci, Seoul 151921, South Korea
[3] Nueva Vizcaya State Univ, Dept Agr Engn, Bayombong 3700, Nueva Vizcaya, Philippines
[4] Korea Rural Community & Agr Corp, Saemangeum Project Off, Shi Jeon Buk, South Korea
[5] Cairo Univ, Fac Agr, Dept Agr Engn, Giza 12613, Egypt
[6] Hainan Univ, Coll Hort & Gardening, Sch Trop Agr & Life Sci, Haikou, Hainan Province, Peoples R China
关键词
ATMOSPHERIC BOUNDARY-LAYER; WIND-TUNNEL; TURBULENT-FLOW; FENCES; CFD; POROSITY; VELOCITY; EROSION; ARRAY;
D O I
10.1016/j.biosystemseng.2011.10.006
中图分类号
S2 [农业工程];
学科分类号
0828 ;
摘要
In this study, computational fluid dynamics (CFD) was utilised to investigate the flow characteristics around tree windbreaks. The efficiency of windbreaks depends on many factors which can be investigated in field experiments, though this is limited due to several reasons such as unstable weather conditions, few measuring points, etc. Fortunately, the investigation is possible via computer simulations. The simulation technique allows the trees to be modelled as a porous media where the aerodynamic properties of the trees are utilised in the model. The trees employed are Black pine trees (Pinus thunbergii) with a drag coefficient value of 0.55. The simulation provides analysis of the effect of gaps between trees, rows of trees, and tree arrangements in reducing wind velocity. The simulations revealed that 0.5 m gap between trees was more effective in reducing wind velocity than 0.75 and 1.0 m. The percentage reduction in velocity at the middle of the tree section for 0.5, 0.75 and 1.0 m gap distance was found to be 71, 65 and 56%, respectively. Two-rows of alternating trees were also found to be more effective than one-row and two-rows of trees. The reduction at the middle of the tree region for one-row and two-rows of trees and two-rows arranged alternately was 71, 88 and 91%, respectively. Results revealed that the percentage reduction in wind velocity measured at distance 15H, where H is the tree height, for one-row, two-rows of trees and two-rows arranged alternately was approximately 20, 30 and 50%, respectively. (C) 2011 IAgrE. Published by Elsevier Ltd. All rights reserved.
引用
收藏
页码:40 / 48
页数:9
相关论文
共 41 条
  • [1] [Anonymous], 2006, FLUENT MAN
  • [2] Bakker A., 2002, Applied Computational Fluid Dynamics: Turbulence models
  • [3] A wind tunnel study on aerodynamic porosity and windbreak drag
    Bitog, J. P.
    Lee, I. -B.
    Hwang, H. -S.
    Shin, M. -H.
    Hong, S. -W.
    Seo, I. -H.
    Mostafa, E.
    Pang, Z.
    [J]. FOREST SCIENCE AND TECHNOLOGY, 2011, 7 (01) : 8 - 16
  • [4] Numerical simulation of an array of fences in Saemangeum reclaimed land
    Bitog, J. P.
    Lee, I-B.
    Shin, M-H.
    Hong, S-W.
    Hwang, H-S.
    Seo, I-H.
    Yoo, J-I
    Kwon, K-S.
    Kim, Y-H.
    Han, J-W.
    [J]. ATMOSPHERIC ENVIRONMENT, 2009, 43 (30) : 4612 - 4621
  • [5] CFD evaluation of wind speed conditions in passages between parallel buildings - effect of wall-function roughness modifications for the atmospheric boundary layer flow
    Blocken, Bert
    Carmeliet, Jan
    Stathopoulos, Ted
    [J]. JOURNAL OF WIND ENGINEERING AND INDUSTRIAL AERODYNAMICS, 2007, 95 (9-11) : 941 - 962
  • [6] CFD simulation of the atmospheric boundary layer: wall function problems
    Blocken, Bert
    Stathopoulos, Ted
    Carmeliet, Jan
    [J]. ATMOSPHERIC ENVIRONMENT, 2007, 41 (02) : 238 - 252
  • [7] Windbreak aerodynamics: Is computational fluid dynamics reliable?
    Bourdin, P.
    Wilson, John D.
    [J]. BOUNDARY-LAYER METEOROLOGY, 2008, 126 (02) : 181 - 208
  • [8] Calvert J. B., 2004, WIND EXPLORATION WIN
  • [9] Castro I. P., 1998, MEFD9891 U SURR
  • [10] Turbulent Kinetic Energy Dissipation in the Surface Layer
    Charuchittipan, D.
    Wilson, J. D.
    [J]. BOUNDARY-LAYER METEOROLOGY, 2009, 132 (02) : 193 - 204