淡江大學機構典藏:Item 987654321/119477
English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 62830/95882 (66%)
造訪人次 : 4038038      線上人數 : 557
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU Library & TKU Library IR team.
搜尋範圍 查詢小技巧:
  • 您可在西文檢索詞彙前後加上"雙引號",以獲取較精準的檢索結果
  • 若欲以作者姓名搜尋,建議至進階搜尋限定作者欄位,可獲得較完整資料
  • 進階搜尋
    請使用永久網址來引用或連結此文件: https://tkuir.lib.tku.edu.tw/dspace/handle/987654321/119477


    題名: Estimation of Turbulence Effects on Wind-Induced Suctions on the Roof of a Low-Rise Building
    作者: Wu, Chieh-Hsun
    關鍵詞: Wind loads;Low-rise building aerodynamics;Turbulence;Separated-reattached flow;Mean pressures;Fluctuating pressures;Pressure integration technique;Quasi-steady theory
    日期: 2017-08-29
    上傳時間: 2020-10-29 12:11:16 (UTC+8)
    摘要: The effects of turbulence in the atmospheric boundary layer (ABL) on surface pressures of a typical low-rise building roof are investigated in this thesis. A 1/50 geometrically-scaled model of the Texas Tech University Wind Engineering Field Research Lab (WERFL) building model is used for pressure measurements in wind tunnel experiments. ABL wind turbulence intensities ranging from about 10% to 30%, and length scales ranging from 6 to 12 times of the building height (H) are generated. The effects of ABL turbulence on the mean roof pressures within the separated flow are explained from the time-averaged Navier-Stokes equations. The pressure fields are reconstructed by integrating the pressure gradients using an analytic interpolation approach. For high turbulence intensity levels, the maximum suction coefficient on the roof surface was found to be increased. Such increasing magnitudes are directly related to reduced sizes of mean separation bubbles, more rapid variation of the velocity magnitude near the leading edge and enhanced variation of the turbulence stresses. On the other hand, higher surface pressure recovery found in the leeward portion of the separation bubble is mainly due to the more rapid variation of the turbulence stresses. The effects of ABL turbulences on the fluctuating roof surface pressures are explained by the quasi-steady (QS) theory. Basically, the QS model assumes that the instantaneous roof surface pressure is induced by a modified local mean flow field. The selection of the mean flow pattern and the amplification of the velocity magnitudes are determined so that the resulted instantaneous velocity vector is matched to the measurement at the reference location, i.e., 1H above the roof leading edge in this thesis. The QS model is found to explain the effects of large length scale turbulences very well. Better QS-predictions are observed if vertical component of the velocities are included. A statistical method for estimating the surface pressure probability distribution, based on the assumptions from the QS model, is derived and validated. This method relates the pdf of building surface pressures to the joint pdf of wind speed, azimuth angle, and elevation angle.
    顯示於類別:[土木工程學系暨研究所] 專書

    文件中的檔案:

    檔案 大小格式瀏覽次數
    index.html0KbHTML92檢視/開啟

    在機構典藏中所有的資料項目都受到原著作權保護.

    TAIR相關文章

    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library & TKU Library IR teams. Copyright ©   - 回饋