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Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow

[Image: see text] In the process of reservoir exploration, the weak horizontal structural surface easily slips and cracks, and casing shearing often occurs during the formation process, which significantly affects the economic viability and effective development of an oilfield. Additionally, repeate...

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Autores principales: Hu, Chaoyang, Wang, Fengjiao, Ai, Chi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Chemical Society 2021
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8427775/
https://www.ncbi.nlm.nih.gov/pubmed/34514260
http://dx.doi.org/10.1021/acsomega.1c03441
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author Hu, Chaoyang
Wang, Fengjiao
Ai, Chi
author_facet Hu, Chaoyang
Wang, Fengjiao
Ai, Chi
author_sort Hu, Chaoyang
collection PubMed
description [Image: see text] In the process of reservoir exploration, the weak horizontal structural surface easily slips and cracks, and casing shearing often occurs during the formation process, which significantly affects the economic viability and effective development of an oilfield. Additionally, repeated damage at the same casing position indicates the possibility of numerous cracks in the weak structural surface. In this study, we propose the geomechanical stick–slip theory to verify the above phenomenon. The stress calculation method for the weak horizontal structural surface in the upper part of the reservoir is devised under the influence of inter-regional pore pressure differences. Based on the process of accumulation–release–reaccumulation–rerelease in the formation and deformation processes, we construct the calculation model of shear stress release and slips on the cracked surface. While considering the influence of water inflow on the cracked surface, the pressure exerted on the formation stick–slip is analyzed. Then, the model was verified by the data of block X in the Daqing oilfield. The results demonstrate that under wet conditions, the maximum static and dynamic frictional stresses on the cracked surface decrease significantly, and this makes the cracked surface more prone to a greater slip degree. After the weak horizontal structural surface cracks and slips occur for the first time, the pressure difference between regions required for formation of the next slip decreases significantly. With the continuous formation of slips, the slip range gradually expands with an increase in inter-regional pressure variance. The research work in this study provides a theoretical basis for the prevention and control of casing damage in oil development zones.
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spelling pubmed-84277752021-09-10 Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow Hu, Chaoyang Wang, Fengjiao Ai, Chi ACS Omega [Image: see text] In the process of reservoir exploration, the weak horizontal structural surface easily slips and cracks, and casing shearing often occurs during the formation process, which significantly affects the economic viability and effective development of an oilfield. Additionally, repeated damage at the same casing position indicates the possibility of numerous cracks in the weak structural surface. In this study, we propose the geomechanical stick–slip theory to verify the above phenomenon. The stress calculation method for the weak horizontal structural surface in the upper part of the reservoir is devised under the influence of inter-regional pore pressure differences. Based on the process of accumulation–release–reaccumulation–rerelease in the formation and deformation processes, we construct the calculation model of shear stress release and slips on the cracked surface. While considering the influence of water inflow on the cracked surface, the pressure exerted on the formation stick–slip is analyzed. Then, the model was verified by the data of block X in the Daqing oilfield. The results demonstrate that under wet conditions, the maximum static and dynamic frictional stresses on the cracked surface decrease significantly, and this makes the cracked surface more prone to a greater slip degree. After the weak horizontal structural surface cracks and slips occur for the first time, the pressure difference between regions required for formation of the next slip decreases significantly. With the continuous formation of slips, the slip range gradually expands with an increase in inter-regional pressure variance. The research work in this study provides a theoretical basis for the prevention and control of casing damage in oil development zones. American Chemical Society 2021-08-26 /pmc/articles/PMC8427775/ /pubmed/34514260 http://dx.doi.org/10.1021/acsomega.1c03441 Text en © 2021 The Authors. Published by American Chemical Society https://creativecommons.org/licenses/by-nc-nd/4.0/Permits non-commercial access and re-use, provided that author attribution and integrity are maintained; but does not permit creation of adaptations or other derivative works (https://creativecommons.org/licenses/by-nc-nd/4.0/).
spellingShingle Hu, Chaoyang
Wang, Fengjiao
Ai, Chi
Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title_full Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title_fullStr Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title_full_unstemmed Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title_short Calculation Model for Stick–Slip Deformation in Weak Horizontal Structural Surface Formation after Water Inflow
title_sort calculation model for stick–slip deformation in weak horizontal structural surface formation after water inflow
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8427775/
https://www.ncbi.nlm.nih.gov/pubmed/34514260
http://dx.doi.org/10.1021/acsomega.1c03441
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