Rozelle立交工程复杂地面条件的特征

IF 0.3 Q4 ENGINEERING, GEOLOGICAL
B. Estrada, T. Nash, Andrew de Ambrosis, I. Chan
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引用次数: 0

摘要

悉尼的Rozelle立交项目(RIC)是一个地下高速公路立交,连接多条地下和地面主干道,以及未来的西部海港隧道和海滩连接。RIC完成了WestConnex项目的工程,是一个由大约22公里的多层隧道组成的复杂阵列,所有隧道都在2.5公里长、1.5公里宽的区域内建造。RIC位于复杂的地面条件下,包括深层土壤、区域断层、构造带和火成岩侵入体。罗泽尔湾附近山谷的深层天然土壤主要是全新世冲积、边缘海相和海相沉积物。这些土壤是层间的,不连续的,通常有轻微的固结,并被19世纪填海造地的沙子和粗石料覆盖。钻孔资料和CPT资料在详细程度上有很大的差别。将其提炼出来,为多个结构的设计师提供一个项目范围的解释报告的地质和岩土模型,需要一种混合的模型呈现方法。这包括提供简化的图形模型,包括具体调查和实验室测试的细节,允许设计师灵活地采用适合其特定应用的适当参数。同样,岩石构造模式也从构造域的开发发展到覆盖构造模式的区域地质构造的识别和包裹。在设计之前和整个设计过程中,对区域规模的逆冲断层、构造复杂的廊道和火成岩侵入体进行了识别和完善。在设计中通过修改开挖顺序和改变隧道支护来考虑这些问题。隧道开挖在预测的位置遇到了这些区域特征,并且与模型中描述的特征相似,从而允许隧道的安全施工。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characterisation Of Complex Ground Conditions For The Rozelle Interchange Project
The Rozelle Interchange Project (RIC) in Sydney is an underground motorway interchange connecting multiple underground and surface arterial roads as well as the future Western Harbour Tunnel and Beaches Link. RIC completes the WestConnex program of works and is a complex array of approximately 22 km of multiple level tunnels, all constructed in an area 2.5 km long and 1.5 km wide. RIC is located within complex ground conditions that include deep soils, regional faults, structural zones and igneous intrusions. Deep natural soils infilling a valley near Rozelle Bay are mostly recent Holocene alluvial, marginal marine and marine deposits. These soils are interlayered, discontinuous, normally to slightly over consolidated and capped by sand and coarse rockfill from 19th century reclamation. There is a strong contrast in the level of detail between borehole and CPT data. Distilling this to provide a geological and geotechnical model for a project wide interpretive report for designers of multiple structures required a hybrid approach to model presentation. This included providing a simplified graphical model and including details from specific investigations and laboratory testing allowing designers flexibility to adopt appropriate parameters for their specific application. Similarly, the rock structural model evolved from development of structural domains to identification and inclusion of regional geological structures overprinting the structural model. Regional scale thrust faults, corridors of structural complexity and igneous intrusions were identified and refined prior to and throughout the design process. These were considered in the design by modification of excavation sequencing and changes to tunnel support. Tunnel excavations encountered these regional features at the locations predicted and with similar character as those described in the model allowing the safe construction of the tunnels.
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来源期刊
Australian Geomechanics Journal
Australian Geomechanics Journal ENGINEERING, GEOLOGICAL-
CiteScore
0.40
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0.00%
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1
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