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A two-scale hydromechanical model for fault zones accounting for their heterogeneous structure

机译:断裂带非均质结构的两尺度水力力学模型

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Fault zones show generally hetergeneous structures constituted of a fault core surrounded by damaged zones containing different fracture families. Taking into account this hetergeneous architecture of fault zones on their hydromechanical response to a pore pressure increase in their vicinity is the main goal of the present paper. The hydromechanical behavior of a fault running across a reservoir during a CO2 injection scenario has been modeled by a two-scale model. At the fault zone scale, statistically distributed fractures are considered to evaluate the equivalent permeability of the fault zone. At the site scale, a specific fault model that takes into account the permeability of different parts of the fault zone is used. The change of the permeability of each damage zone due to the pressure build-up within the reservoir is taken into account. Finally, the proposed model is used to perform large-scale simulations of the injection operation through a multilayered geological site. The model permits to simulate brine flow through the fault zone. The failure reactivation risk can also be estimated through the failure criterion of the fault core's materials, here considered following an elastic perfectly plastic Drucker-Prager criterion. (C) 2015 Elsevier Ltd. All rights reserved.
机译:断层带显示出一般的非均质结构,由断层岩心构成,周围分布着包含不同断裂族的破坏区。考虑到断层带在其对附近孔隙压力增加的流体力学响应上的这种非均质结构是本论文的主要目标。在CO2注入过程中,贯穿储层的断层的流体力学行为已通过两尺度模型进行了建模。在断层带范围内,考虑统计分布的裂缝来评估断层带的等效渗透率。在现场规模上,使用考虑了断层带不同部分渗透率的特定断层模型。考虑了由于储层内压力的增加而引起的每个破坏区渗透率的变化。最后,提出的模型用于通过多层地质现场进行注入操作的大规模模拟。该模型可以模拟流过断层带的盐水。也可以通过断层芯材料的破坏准则来估计失效重新激活的风险,这里遵循弹性完全塑性Drucker-Prager准则。 (C)2015 Elsevier Ltd.保留所有权利。

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