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首页> 外文期刊>Journal of Hydrology >Responses of retaining wall and surrounding ground to pre-excavation dewatering in an alternated multi-aquifer-aquitard system
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Responses of retaining wall and surrounding ground to pre-excavation dewatering in an alternated multi-aquifer-aquitard system

机译:交替多含水层 - 水产系统中挡土墙与围绕前脱水预防脱水的反应

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摘要

Pre-excavation dewatering (PED) is an important construction stage in deep excavation. Field measurements show that retaining walls can develop obvious deflections during PED, which has been rarely considered in the past. The characteristics of PED-induced wall deflection, and the relationship of this deflection to surrounding ground deformation are still unclear. In this study, a PED test is simulated by a numerical model. The model is verified by field observations and used to investigate the responses of retaining wall and surrounding ground to PED. Results indicate that the maximum wall defection (delta(hm)) and surface settlement (delta(vm)) can all reach centimeter level under common conditions of PED. The ratio of delta(vm) to delta(hm) varies at the range of 0.45-0.67. Wall and soil deformations will be more obvious if the soils within the dewatering depth (H-d) have better permeability. The relative positions between H-d and strata (i.e., aquifer or aquitard) have great influence on the PED-induced deformations. If an aquifer appears below H-d, further increasing H-d can induce a rapid growth of wall and soil deformations. If thick aquitard appears below H-d, the deformation increments by further increasing H-d are not apparent. However, once H-d exceeds the center of the thick aquitard and reaches a thick confined aquifer, the wall deflections and soil deformation zones behind the wall will enlarge significantly. Meanwhile, a large bending moment in the retaining wall will arise around the bottom of the confined aquifer. The designers should consider this condition and allocate enough steel rebars there, preventing the appearance of wall cracks in the confined aquifer. (C) 2018 Elsevier B.V. All rights reserved.
机译:前挖掘脱水(PED)是深度挖掘的重要施工阶段。现场测量表明,挡土墙可以在PED期间发育明显的偏转,这已经很少在过去考虑。 PED引起的壁偏转的特性,以及这种偏转与周围地变形的关系仍然不清楚。在该研究中,通过数值模型模拟PED测试。该模型通过现场观察验证,并用于研究挡土墙和周围地面的响应。结果表明,最大壁逸线(δ(HM))和表面沉降(Delta(VM))可以在PED的常见条件下达到厘米水平。 Delta(VM)与δ(HM)的比率在0.45-0.67的范围内变化。如果脱水深度(H-D)内的土壤具有更好的渗透性,墙壁和土壤变形将更加明显。 H-D和地层之间的相对位置(即含水层或水流)对PED引起的变形有很大影响。如果含水层出现在H-D下方,则进一步增加的H-D可以诱导墙壁和土壤变形的快速生长。如果厚的水管出现在H-D下方,则通过进一步增加H-D的变形增量并不明显。然而,一旦H-D超过厚腹水的中心,达到厚厚的受限含水层,墙壁后面的墙壁偏转和土壤变形区域就会显着增大。同时,围绕围绕含水层的底部围绕挡土墙的大弯矩。设计师应考虑这种情况并在那里分配足够的钢筋,防止围绕含水层的墙壁裂缝的出现。 (c)2018年elestvier b.v.保留所有权利。

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