English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 94274/94274 (100%)
造訪人次 : 82842925      線上人數 : 1821
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/987654321/104099


    題名: Seismic velocity variations at TCDP are controlled by MJO driven precipitation pattern and high fluid discharge properties
    作者: 馬國鳳;Hillers, G.;Campillo, M.;Ma, K.-F.
    貢獻者: 地球科學學院地球科學學系
    關鍵詞: ambient noise;Amplitudes;borehole seismology;Computational fluid dynamics;Diffusion;Discharge;Fluid flow;Fluids;ground water table;Groundwater;Madden–Julian oscillation;monitoring;Precipitation;Water tables
    日期: 2014-04-01
    上傳時間: 2026-04-23 11:43:33 (UTC+8)
    出版者: Elsevier BV;Elsevier B.V
    摘要: 摘要: Using seismic noise based monitoring techniques we find that seismic velocity variations (dv/v) observed with the borehole array of the Taiwan Chelungpu-fault Drilling Project (TCDP) are controlled by strong precipitation events associated with the Madden–Julian Oscillation (MJO), a dynamic intraseasonal atmospheric pattern in the tropical atmosphere. High-frequency noise (>1 Hz) excited by steady anthropogenic activity in the vicinity of the TCDP allows daily resolution of dv/v time series. Relatively large fluid discharge properties control the equilibration of the ground water table and hence seismic velocities on time scales smaller than the average precipitation recurrence interval. This leads to the observed synchronous 50–80 day periodicity in dv/v and rainfall records in addition to the dominant annual component. Further evidence for the governing role of hydraulic properties is inferred from the similarity of observed dv/v timing, amplitude, and recovery properties with dv/v synthetics generated by a combined model of ground water table changes and diffusive propagation of seismic energy. The lapse time (τ) dependent increase of dv/v amplitudes is controlled by the sensitivity of the diffuse wave field sampled at 1100 m depth to shallower water level fluctuations. The significant vertical offset between stations and water level explains the direct τ dependence which is opposite to the trend previously inferred from measurements at the surface. •Seismic velocities at TCDP are monitored with anthropogenic noise.•Variations of the ground water level control relative velocity changes (dv/v).•Rainfall and dv/v patterns are governed by the Madden–Julian Oscillation.•An efficient percolation network facilitates rapid fluid discharge.•Lapse time dependence of dv/v amplitudes constrains elastic mean free path.
    出版者: Elsevier B.V
    出版日期: 2014-04-01
    出處: Earth and Planetary Science Letters, 2014-04, Vol.391, p.121-127
    資源來源: Elsevier ScienceDirect Journals Complete **
    版權: 2014 Elsevier B.V.
    識別號: ISSN: 0012-821X
    識別號: EISSN: 1385-013X
    識別號: DOI: 10.1016/j.epsl.2014.01.040
    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.html0KbHTML23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