3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul
A numerical investigation utilizing the 3D displacement discontinuity method is performed to examine the stress perturbations and induced displacements near a weak fault with arbitrary orientations and dip, assuming zero shear stress and normal displacement. The in-situ stress field near the fault is...
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Yandy Scientific Press
2021
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oai:doaj.org-article:cdb6108159bd4339a0383bc7244c4f362021-11-08T07:07:57Z3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul10.46690/ager.2021.03.052208-598Xhttps://doaj.org/article/cdb6108159bd4339a0383bc7244c4f362021-09-01T00:00:00Zhttps://www.yandy-ager.com/index.php/ager/article/view/342https://doaj.org/toc/2208-598XA numerical investigation utilizing the 3D displacement discontinuity method is performed to examine the stress perturbations and induced displacements near a weak fault with arbitrary orientations and dip, assuming zero shear stress and normal displacement. The in-situ stress field near the fault is taken as known and varied with depth. The modelling is constructed based on indirect boundary integral equations. In this work, the fault plane is first modelled as a rectangular plane with negligible thickness between the adjacent surfaces. The fault plane is then divided into numerous rectangular boundary elements with imposed shear singularities on the surface, which is normal to the fault plane to simulate a traction-free scenario. The numerical results of the total induced stresses and displacements are then compared to the existing solutions of a penny-shaped crack for validation purpose. With validated results, the paper moves on to the discussion of various factors that have impacts on the induced stress and displacements, including: aspect ratio which is defined by strike over dip; orientation of the strike on the horizontal ground surface; as well as dip. The boundary integration method with modification is also used to model an elliptical distribution of singularities with inner, corner, and edge elements to accommodate more complex shape of a discontinuity; small differences are observed.Yutong ChaiShunde YinYandy Scientific Pressarticledisplacement discontinuityin-situ stressweak faultnumerical analysisEngineering geology. Rock mechanics. Soil mechanics. Underground constructionTA703-712GeologyQE1-996.5ENAdvances in Geo-Energy Research, Vol 5, Iss 3, Pp 286-296 (2021) |
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displacement discontinuity in-situ stress weak fault numerical analysis Engineering geology. Rock mechanics. Soil mechanics. Underground construction TA703-712 Geology QE1-996.5 |
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displacement discontinuity in-situ stress weak fault numerical analysis Engineering geology. Rock mechanics. Soil mechanics. Underground construction TA703-712 Geology QE1-996.5 Yutong Chai Shunde Yin 3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
description |
A numerical investigation utilizing the 3D displacement discontinuity method is performed to examine the stress perturbations and induced displacements near a weak fault with arbitrary orientations and dip, assuming zero shear stress and normal displacement. The in-situ stress field near the fault is taken as known and varied with depth. The modelling is constructed based on indirect boundary integral equations. In this work, the fault plane is first modelled as a rectangular plane with negligible thickness between the adjacent surfaces. The fault plane is then divided into numerous rectangular boundary elements with imposed shear singularities on the surface, which is normal to the fault plane to simulate a traction-free scenario. The numerical results of the total induced stresses and displacements are then compared to the existing solutions of a penny-shaped crack for validation purpose. With validated results, the paper moves on to the discussion of various factors that have impacts on the induced stress and displacements, including: aspect ratio which is defined by strike over dip; orientation of the strike on the horizontal ground surface; as well as dip. The boundary integration method with modification is also used to model an elliptical distribution of singularities with inner, corner, and edge elements to accommodate more complex shape of a discontinuity; small differences are observed. |
format |
article |
author |
Yutong Chai Shunde Yin |
author_facet |
Yutong Chai Shunde Yin |
author_sort |
Yutong Chai |
title |
3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
title_short |
3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
title_full |
3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
title_fullStr |
3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
title_full_unstemmed |
3D displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
title_sort |
3d displacement discontinuity analysis of in-situ stress perturbation near a weak faul |
publisher |
Yandy Scientific Press |
publishDate |
2021 |
url |
https://doaj.org/article/cdb6108159bd4339a0383bc7244c4f36 |
work_keys_str_mv |
AT yutongchai 3ddisplacementdiscontinuityanalysisofinsitustressperturbationnearaweakfaul AT shundeyin 3ddisplacementdiscontinuityanalysisofinsitustressperturbationnearaweakfaul |
_version_ |
1718442947881467904 |