English  |  正體中文  |  简体中文  |  全文筆數/總筆數 : 94201/94201 (100%)
造訪人次 : 81474325      線上人數 : 3297
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/987654321/102411


    題名: Numerical assessment of CO2 geological sequestration in sloping and layered heterogeneous formations: A case study from Taiwan
    作者: 李明旭;Sung, Rui-Tang;Li, Min-Hsu;Dong, Jia-Jyun;Lin, Andrew Tien-Shun;Hsu, Shu-Kun;Wang, Chien-Ying;Yang, Chien-Nan
    貢獻者: 地球科學學院水文與海洋科學研究所
    關鍵詞: Changhu Coastal Industrial Park (CCIP) site;CO2 geological sequestration;Taiwan;TOUGHREACT/ECO2N
    日期: 2014-01-01
    上傳時間: 2026-04-23 11:08:14 (UTC+8)
    出版者: Elsevier;Elsevier Ltd
    摘要: 摘要: •Geological structure of the site was revealed by seismic reflection surveys.•CO2 evaluation at the CCIP was simulated with locally refined grids.•Migration of CO2 plume did not penetrate low permeability formation in 500 years.•Solubility and residual trapping account for 46% of injected CO2 after 500 years. Carbon dioxide geological sequestration (CGS) has been recognized as one of the potential solutions for reducing anthropogenic CO2 emissions. The Changhua Coastal Industrial Park (CCIP) in central Taiwan has been preliminarily evaluated as a potential site for CGS. The CCIP site possesses sloping and layered heterogeneous formations with stagnant groundwater flow. Previous geophysical investigations of seismic reflection survey have found no significant faults near this site. Prior to the actual application of CGS in the field, it is important to carry out numerical simulations to predict the short- and long-term evolution of injected CO2 into deep geological formations. In this study, the TOUGHREACT/ECO2N simulator is employed in order to conduct comprehensive CGS assessments at the CCIP site. Field scale CGS simulations are utilized to capture the details of the physical features, such as the displacement of saline brine by the injection of CO2, buoyancy/gravity convection, and salt precipitation due to pore water dry-out, in the vicinity of the CO2 injection well. Simulation results show that (1) the migration of CO2 plume did not penetrate the low permeability formation at 500 years, (2) formation tilting caused a slightly asymmetric CO2 plume oriented toward the up-tilt direction, and (3) the amount of solubility and residual gas trapping accounted for 26.8% and 19.0%, respectively, of injected CO2 by weight at 500 years.
    出版者: Elsevier Ltd
    出版日期: 2014-01
    出處: International journal of greenhouse gas control, 2014-01, Vol.20, p.168-179
    版權: 2013 Elsevier Ltd
    識別號: ISSN: 1750-5836
    識別號: EISSN: 1878-0148
    識別號: DOI: 10.1016/j.ijggc.2013.11.003
    顯示於類別:[水文與海洋科學研究所] 期刊論文

    文件中的檔案:

    檔案 描述 大小格式瀏覽次數
    index.html0KbHTML22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