Sensitivity Analyses of Three-Dimensional Discrete Fracture Network Modeling of Rock Mass

J. C. Park, Seung-Hun Park, Ha Yung Kim, Geon-Young Kim, Sangki Kwon
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Abstract

Abstract This study analyzes the relationship between parameters of the discontinuity in Discrete Fracture Network model such as fracture intensity, fracture orientation, fracture size, fracture shape etc. In this paper, FracMan code was used to model and analyze 3D DFN. A sensitivity analysis was performed in order to analyze the relationship between linear fracture intensity measure (   ) and parameters of the discontinuity in 100 m × 100 m × 100 m model area. As a result the sensitivity analysis showed that key parameters affecting fracture intensity are fracture orientation (Trend / Plunge). Conversion factor(   ) for   , to calculate volumetric fracture intensity measure (   ), is derived in case of vertical well and horizontal well when trend is 10°, 30°, 60°, 90°, 120°, 150°, 180° (7cases) and plunge is 5°, 15°, 30°, 45°, 60°, 75°, 85° (7cases). It is expected that this paper can be used effectively for modeling and understanding DFN model.Key words Discontinuous rock masses, 3D Discrete Fracture Network, Fracture intensity, FracMan code초 록 본 연구에서는 불연속암반의 모사기법인 3차원 불연속균열망(Discrete Fracture Network, DFN)모델의 구성 및 해석 코드인 FracMan을 이용하여, DFN모델에서의 불연속면의 밀도(fracture intensity), 불연속면의 방향성(fracture orientation), 불연속면의 크기(fracture size), 불연속면의 모양(fracture shape) 등의 불연속면의 특성인자간의 관계를 분석하고자 하였다. 100 m × 100 m × 100 m 모델영역에서 균열의 선형밀도(
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岩体三维离散裂隙网络建模敏感性分析
摘要本文分析了离散裂缝网络模型中裂缝强度、裂缝方向、裂缝尺寸、裂缝形状等不连续参数之间的关系。本文采用FracMan代码对三维DFN进行建模和分析。在100 m × 100 m × 100 m模型区内,对线性断裂强度测量值( )与不连续面参数之间的关系进行敏感性分析。结果表明,影响裂缝强度的关键参数是裂缝方向(Trend / Plunge)。推导出竖直方向为10°、30°、60°、90°、120°、150°、180°(7例),垂直方向为5°、15°、30°、45°、60°、75°、85°(7例)时,用于计算体积压裂强度指标( )的转换因子()。期望本文能够有效地用于DFN模型的建模和理解。关键词不连续岩体,3 d离散裂缝网络,断裂强度,FracMan代码초록본연구에서는불연속암반의모사기법인3차원불연속균열망(离散裂缝网络,DFN)모델의구성및해석코드인FracMan을이용하여,DFN모델에서의불연속면의밀도(断裂强度)불연속면의방향성(裂缝方向)불연속면의크기(裂缝大小),불연속면의모양(裂缝形状)등의불연속면의특성인자간의관계를분석하고자하였다。100m × 100m × 100m
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