Localized stress field modelling around fractures using three-dimensional discrete element method
Autor: | Ehtesham Karatela, Abbas Taheri |
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Rok vydání: | 2018 |
Předmět: |
0211 other engineering and technologies
Borehole 02 engineering and technology Mechanics Classification of discontinuities 010502 geochemistry & geophysics Geotechnical Engineering and Engineering Geology 01 natural sciences Discrete element method Stress field Stress drop Fuel Technology Discontinuity (geotechnical engineering) Anisotropy Rock mass classification Geology 021101 geological & geomatics engineering 0105 earth and related environmental sciences |
Zdroj: | Journal of Petroleum Science and Engineering. 171:472-483 |
ISSN: | 0920-4105 |
DOI: | 10.1016/j.petrol.2018.07.038 |
Popis: | Understanding of field stress condition in fractured rock mass is required to investigate stability of underground excavations. To analyze stress perturbation in fractured rock mass, a regional model is generated using a DEM based code, 3DEC.Three major steep faults were considered in the model. The regional model then was used to estimate stresses on the boundaries of smaller descriptive model termed as the base model. Stresses were observed to vary in magnitude at the intersection of discontinuity sets and stress drop was observed at the discontinuity. In addition, stress tensors in the model were observed to rotate parallel to the discontinuity. A vertical borehole in base model revealed that high stresses concentrated along discontinuities may result in forming yield zones around the borehole. Furthermore, the base mode was subjected to strength and stress anisotropy analysis. Effect of stress anisotropy on stress perturbation was significant, whereas, stress values slightly changed by strength anisotropy. In both cases, due to the effect of discontinuities the induced stress field was non-linear and fluctuating. Effect of stress anisotropy on stress perturbation found to be more significant for the maximum principal stress as compare with the minimum principal stress. |
Databáze: | OpenAIRE |
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