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Development of a non-contact survey method of tunnel excavation face for DEM modelling

机译:用于DEM建模的隧道开挖面非接触测量方法的开发

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The excavation of underground voids, both for mining or civil purpose, inevitably determine a variation of the acting state of stress and consequently of the safety condition. The results are: a general deformation state induced around the excavation and, possibly, localized displacements in correspondence with pre existing discontinuities. Moreover, during tunnel excavation, there is a constant need to verify the real fracture state of the rock mass since, during the design phase, the rock mass condition has been determined on the base of borehole or surface rock mass surveys with low reliable level. All these reasons lead to the common practice to monitor tunnel excavation with convergence measurements, face extrusion measurements and structural survey of the rock mass at the tunnel face. The structural survey can be a complex and dangerous operation when dealing with low qualitaty rock mass due to the possible unstable condition of the face due to the quoted reasons. Moreover in certain delicate cases the face must be rapidly consolidated and this makes the survey even more difficult to be realized. Finally the tunnel section can be some meters high making impossible to reach it all without a special lifting system. All these reasons led the authors to develop a method for the geostructure survey based on photogrammetry. The core of the method is the possibility to obtain all face information by taking just few photographs, reconstructing automatically a digital surface model (DSM) of the face and then applying a code developed by the authors called Rockscan for the determination of the discontinuity in terms of orientation and location on the face. The method has been developed trough the application to a real case at a railway tunnel face in the province of Parma (North Italy). The paper describes the method, the developed code and the application to the tunnel.
机译:无论是采矿目的还是民用目的,地下空隙的开挖不可避免地决定了应力作用状态的变化,进而决定了安全状况。结果是:在开挖周围引起的一般变形状态,以及可能与先前存在的不连续性相对应的局部位移。此外,在隧道开挖过程中,始终需要验证岩体的真实断裂状态,因为在设计阶段,已经根据井眼或地表岩体勘测确定了岩体状态,而可靠度较低。所有这些原因导致了一种通行的做法,即采用会聚测量,面挤出测量和隧道面岩体结构勘测来监测隧道开挖。当处理低质量的岩体时,结构性测量可能是复杂而危险的操作,因为引用的原因可能导致工作面不稳定。此外,在某些微妙的情况下,必须快速整容脸部,这使得调查变得更加困难。最终,隧道断面可能会高出几米,如果没有特殊的提升系统,就不可能全部到达。所有这些原因促使作者开发了一种基于摄影测量的地理结构调查方法。该方法的核心是通过仅拍摄几张照片,自动重建人脸的数字表面模型(DSM),然后应用由作者开发的称为Rockscan的代码来确定不连续性的方法来获取所有人脸信息的可能性。在脸上的方向和位置。该方法是通过将其应用到帕尔马省(意大利北部)的铁路隧道工作面的实际案例中而开发出来的。本文介绍了该方法,开发的代码及其在隧道中的应用。

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