Review on Methods of Hydro-Mechanical Coupled Modeling for Long-term Evolution of the Natural Barriers

서지정보

ㆍ발행기관 : 한국방사성폐기물학회 ㆍ수록지정보 : 방사성폐기물학회지 / 20권 / 4호
ㆍ저자명 : Chae-Soon Choi, Yong-Ki Lee, Sehyeok Park, Kyung-Woo Park

목차

1. Introduction
2. Hydro-Mechanical Evolution of theNatural Barriers
2.1 Categorization of FEPs and Configurationof an Interaction System
2.2 Mechanism of a Natural Barrier EvolutionProcess
3. Numerical Method for Simulation ofHydro-Mechanical Behavior of Rock
3.1 Hydro-Mechanical Modeling in DistinctElement Method
3.2 Hydro-Mechanical Modeling by the FiniteElement Method
4. Case Studies to Review the Hydro-Mechanical Modeling Method
4.1 Case Study 1: Boundary Condition forthe Long-term Evolution of TectonicStructure
4.2 Case Study 2: Upscaling Problem inFractured Rock Simulation
4.3 Case Study 3: Stress Field Distributionand Disturbance Problem
5. Conclusions
Acknowledgements
REFERENCES

영어 초록

Numerical modeling and scenario composition are needed to characterize the geological environment of the disposal site and analyze the long-term evolution of natural barriers. In this study, processes and features of the hydro-mechanical behavior of natural barriers were categorized and represented using the interrelation matrix proposed by SKB and Posiva. A hydro-mechanical coupled model was evaluated for analyzing stress field changes and fracture zone re-activation. The processes corresponding to long-term evolution and the hydro-mechanical mechanisms that may accompany critical processes were identified. Consequently, practical numerical methods could be considered for these geological engineering issues. A case study using a numerical method for the stability analysis of an underground disposal system was performed. Critical stress distribution regime problems were analyzed numerically by considering the strata’s movement. Another case focused on the equivalent continuum domain composition under the upscaling process in fractured rocks. Numerical methods and case studies were reviewed, confirming that an appropriate and optimized modeling technique is essential for studying the stress state and geological history of the Korean Peninsula. Considering the environments of potential disposal sites in Korea, selecting the optimal application method that effectively simulates fractured rocks should be prioritized.

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