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Simulation of the Fracture Network in the Inter-Bed Layered Rock Masses

机译:床间层状岩体中骨折网络的模拟

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Different to the fracture network in general rock masses, the rules of the fracture developed in inter-bed layered rock masses has its particular characters. The fracture in inter-bed layered rock masses can be divided into two kinds: bed fracture and tectonic fracture. According to the relation between the bed fracture and tectonic fracture, the tectonic fracture can be subdivided into two kinds: bed bounded fracture and unbounded fracture. And there are some approximately linear relations or non-linear relations between the beds bounded fracture space and the thickness of the strata. In this paper, the development rules of these fractures are generalized firstly, and then the development mechanism of tectonic fractures is introduced. Based on the development rules and the mechanism, a method of simulated the fracture network in inter-bed layered rock masses is put forward. Lastly, through an example the simulation method is applied into the analysis of seepage field in inter-bed layered rock masses. The result shows that the water flow in the inter-bed layered rocks is controlled by the bed fracture and the unbounded joints, and shows that it is necessary to research the simulation of fracture network in the inter-bed layered rock masses.
机译:与一般岩体中的骨折网络不同,卧间分层岩体中发育的骨折的规则具有其特殊的特点。床间层状岩体的骨折可分为两种:床骨折和构造骨折。根据床骨骨折和构造骨折之间的关系,构造骨折可以细分为两种:床有界骨折和无染性的骨折。并且床之间有一些大致的线性关系或床之间有界裂缝空间和地层的厚度之间的非线性关系。本文首先推出了这些裂缝的发展规则,然后介绍了构造骨折的发展机制。基于开发规则和机制,提出了一种模拟层间层状岩体中裂缝网络的方法。最后,通过一个示例,仿真方法应用于床间层状岩体中渗流场的分析。结果表明,床间层状岩石中的水流由床骨折和未束缚的关节控制,并表明需要研究床间层状岩体中骨折网络的模拟。

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