English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 94201/94201 (100%)
造訪人次 : 81564005      線上人數 : 3974
RC Version 7.0 © Powered By DSPACE, MIT. Enhanced by NTU 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://ir.lib.ncu.edu.tw/handle/987654321/104180


    題名: Simulation of the records of the 27 March 2013 Nantou Taiwan earthquake using modified semi-empirical approach
    作者: 温國樑;Joshi, A.;Kuo, Chun-Hsiang;Dhibar, Piu;Sandeep;Sharma, M. L.;Wen, Kuo-Liang;Lin, Che-Min
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: Acceleration;Amplification;Bedrock;Civil Engineering;Computer simulation;Earth and Environmental Science;Earth Sciences;Earthquakes;Environmental Management;Geophysics/Geodesy;Geotechnical Engineering & Applied Earth Sciences;Hydrogeology;Mathematical models;Natural Hazards;Original Paper;Rupture;Seismic activity;Seismology;Stations;Statistical analysis
    日期: 2015-09-27
    上傳時間: 2026-04-23 11:45:05 (UTC+8)
    出版者: Springer Netherlands;Dordrecht: Springer Netherlands
    摘要: 摘要: It is seen that strong motion generation area plays an important role in the shaping of strong motion records at the observation point. Strong motion generation areas identified within the rupture plane of the 27 March 2013 Nantou, Taiwan, earthquake ( M w = 5.9) have been modelled in this work. It is seen that all available records are at the surface which include site amplification terms. The modified semi-empirical technique effectively simulates records at rock site. The site amplification terms in all records have been removed using SHAKE 91 program and velocity input at each site. The observed records corrected for site amplification terms are further used for comparison with simulated record at the bedrock from several models. Once the observed records at soil sites are transferred at the bedrock, the next task is selection of final model that gives best fit records. Peak ground acceleration from simulated record at four sites is compared with that from corrected observed data. Since the semi-empirical technique of simulation is strongly dependent on various modelling parameters such as dip, strike, rake, rupture velocity and starting points of rupture, these parameters change iteratively in a specified range in a heuristic way to obtain best modelling parameters. The model giving minimum root mean square error (RMSE) is retained at final model. It is seen that minimum root mean square error of the wave form comparison has been obtained at four stations for the source model having single strong motion generation area. Strong motion records have been simulated at four different recording stations. Comparison of observed and simulated records has been made in terms of RMSE between simulated and observed acceleration records, velocity records and the response spectra at each of four stations. Comparison of waveforms and parameters extracted from observed and simulated records confirms the efficacy of the modified technique to model earthquake characterized by SMGAs.
    其他題名: Nat Hazards
    出版者: Dordrecht: Springer Netherlands
    出版日期: 2015-09-01
    出處: Natural hazards (Dordrecht), 2015-09, Vol.78 (2), p.995-1020
    資源來源: Agricultural & Environmental Science Collection
    版權: Springer Science+Business Media Dordrecht 2015
    識別號: ISSN: 0921-030X
    識別號: EISSN: 1573-0840
    識別號: DOI: 10.1007/s11069-015-1754-2
    顯示於類別:[地球科學學系] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML16檢視/開啟


    在NCUIR中所有的資料項目都受到原著作權保護.

    社群 sharing

    ::: Copyright National Central University. | 國立中央大學圖書館版權所有 | 收藏本站 | 設為首頁 | 最佳瀏覽畫面: 1024*768 | 建站日期:8-24-2009 :::
    DSpace Software Copyright © 2002-2004  MIT &  Hewlett-Packard  /   Enhanced by   NTU Library IR team Copyright ©   - 隱私權政策聲明