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Numerical Approach for a Rock Mechanics Descriptive Model

机译:岩石力学描述模型的数值方法

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This paper addresses the methodology developed in Sweden for the rock mechanics descriptive model,rnwhich utilized empirical methods such as RMR, Q and GSI but also developed a methodology forrnestimating the strength and deformation properties of the confined rock mass using the numericalrnprogram UDEC. One of the difficulties in describing the rock mass behaviour is assigning thernappropriate constitutive model. With the progress in discrete element software, this limitation may bernovercome as the user is not required to prescribe a constitutive model for the rock mass. In stead thernmicro-scale properties of the intact rock and joints are defined and the macro-scale response resultsrnfrom those properties and the geometry of the problem. In this paper a rock mass is simulated using arndiscrete model and the results compared to the traditional model where the constitutive model isrnprescribed. In the PFC model the behaviour of the rock mass changed from brittle to perfectly plasticrnwith increase in the number of joints. As expected, the presence of joints had a pronounced effect onrnpost peak response of the rock mass. More importantly the post-peak response of the PFC model wasrnnot determined by a user specified constitutive model, while the UDEC results were determined by thernconstitutive model applied to the joints.
机译:本文介绍了瑞典为岩石力学描述模型开发的方法,该方法运用了经验方法(例如RMR,Q和GSI),还开发了一种使用数值程序UDEC估算承压岩体强度和变形特性的方法。描述岩体行为的困难之一是分配适当的本构模型。随着分立元件软件的进步,可以克服该限制,因为不需要用户为岩体开出本构模型。取而代之的是,定义完整岩石和节理的微观尺度特性,并从这些特性和问题的几何形状得出宏观尺度响应。本文使用arndiscrete模型对岩体进行了模拟,并将结果与​​规定了本构模型的传统模型进行了比较。在PFC模型中,随着节理数量的增加,岩体的行为从脆性变为完全塑性。不出所料,节理的存在对岩体的峰值后响应有明显的影响。更重要的是,PFC模型的峰后响应不是由用户指定的本构模型确定的,而UDEC结果是由应用于关节的本构模型确定的。

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