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Excavation cycle dependent changes of hydraulic properties of granular soil at the tunnel face during slurry shield excavations

机译:泥浆盾构开挖过程中开挖周期对粒状土水力特性的影响

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Increased pore pressure heads in front of the tunnel face are frequently observed during excavations with slurry shields. It is expected that the excess pressures are caused by a flow in front of the tunnel face resulting from the interaction between the face supporting fluid (bentonite slurry) and the soil. The flow is assumed to be unsteady from two points of view. First, it is influenced by a time dependent change of hydraulic properties of the soil at the tunnel face. The time dependent change is governed by the interaction with bentonite slurry. Second, the area of the soil on the tunnel face with changed hydraulic properties is disturbed periodically by passing cutting tools which are rotating with the cutting wheel. After each passing of the cutting tool through a particular point at the tunnel face, new local flow is induced. The aim of this paper is to investigate experimentally the transient changes of hydraulic properties of granular soils due to interaction with bentonite slurries. The time dependent change of the soil properties is compared with excavation data of real shield machine describing the time scale of the cutting process. Based on the comparison, the hydraulic properties of soil on the real tunnel face during excavation can be evaluated. Thus, a better assessment of the pore pressure heads in front of the tunnel face can be performed.
机译:在使用泥浆护盾进行挖掘的过程中,经常会观察到隧道面前孔压头的增加。可以预料,过大的压力是由于工作面支撑液(膨润土浆)与土壤之间的相互作用而在隧道工作面前方产生流动而引起的。从两个角度来看,假定流量不稳定。首先,它受隧道面土壤水力特性随时间变化的影响。时间变化取决于与膨润土浆液的相互作用。其次,通过使随切割轮一起旋转的切割工具周期性地扰动具有改变的水力特性的隧道面上的土壤区域。每次切削工具通过隧道面的特定点后,都会引发新的局部流动。本文的目的是通过实验研究由于与膨润土浆液相互作用而引起的粒状土壤水力特性的瞬态变化。将随时间变化的土壤特性与描述盾构切割过程时间尺度的真实盾构机挖掘数据进行比较。基于比较,可以评估开挖过程中真实隧道面上土壤的水力特性。因此,可以更好地评估隧道面前的孔隙压力头。

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