• The Design Procedure of Groundwater Monitoring Wells for the Site Selection of the High Level Radioactive Waste Disposal
  • Kim Taehee*

  • Korea Institute of Geosceince and Moneral Resources, Daejeon, 34132, Korea

  • 고준위 방사성 폐기물 처분장 부지 평가를 위한 배경 지하수위 관측정의 설계와 절차
  • 김태희*

  • 한국지질자원연구원

  • This article is an open access article distributed under the terms of the Creative Commons Attribution Non-Commercial License (http://creativecommons.org/licenses/by-nc/4.0) which permits unrestricted non-commercial use, distribution, and reproduction in any medium, provided the original work is properly cited.

Abstract

The performance of natural barriers at high-level radioactive waste disposal sites heavily depends on the regional groundwater system, which regulates the leakage of waste and radionuclides. Waste disposal sites require homogeneous and mechanically stable formations, making groundwater characterization difficult due to restricted discontinuities like fractures and faults. In the fractured media, conventional groundwater level observation methods in a single borehole only provide averaged hydraulic head data, failing to distinguish individual permeable fractures. To improve the interpretation of the groundwater monitoring results in the fractured media, it is essential to separate each of permeable fractures within a borehole and implement independent hydraulic head observation systems. Flow-logging is currently the most effective method for identifying permeable fractures from each others, supplemented by lithologic and geophysical loggings. Once permeable fractures are identified, their hydraulic connectivity can be examined, and multi-level monitoring wells can be designed accordingly. Despite this, Korea still lacks sufficient technical expertise in constructing various observation wells, highlighting the need for further development in this area.


Keywords: Crystalline rock, Conductive fractures, Connectivity, Design of monitoring well, Investigation procedure

This Article

  • 2025; 30(3): 14-28

    Published on Jun 30, 2025

  • 10.7857/JSGE.2025.30.3.014
  • Received on May 28, 2025
  • Revised on Jun 13, 2025
  • Accepted on Jun 26, 2025

Correspondence to

  • Kim Taehee
  • Korea Institute of Geosceince and Moneral Resources, Daejeon, 34132, Korea

  • E-mail: katzura@kigam.re.kr