Three-Dimensional Response of the Supported-Deep Excavation System: Case Study of a Large Scale Underground Metro Station
Abstract
:1. Introduction
2. Case Study
2.1. Site Conditions
2.2. Stages of Construction
- 1st Stage: Construction of diaphragm walls to a depth of 48.0 m. Bentonite slurry installation procedure was involved in this stage.
- 2nd Stage: Grouting the essential water plug with a thickness of 7.0 m between the diaphragm walls.
- 3rd Stage: Dewatering the groundwater table to level of (–3.30), excavation to roof slab level, and roof slab concreting.
- 4th Stage: Excavation to technical slab level and technical slab concreting.
- 5th Stage: Excavation to the level of the first row of struts and installation of steel beams. Also, a pre-stressing force of 1500 kN was applied on each strut steel beam in this stage.
- 6th Stage: Excavation to the level of the second row of struts, then installation and pre-stressing of the second row of steel struts.
- 7th Stage: Excavation to raft slab level and raft slab concreting.
- 8th Stage: Removal of the first and the second rows of struts.
- 9th Stage: Concreting the ticket slab and stopping the dewatering process.
2.3. Field Measurements
3. Numerical Modeling
3.1. Properties of the Soil Model
3.2. Two Dimensional Numerical Modeling
3.3. Three Dimensional Numerical Modeling
3.4. Analysis Stages
4. Results and Discussion
5. Conclusions
- Excellent agreement was obtained between field measurements and results of the three-dimensional finite element model in both wall lateral displacement and neighboring soil vertical settlement.
- In this case, the three-dimensional finite element model was superior to the two-dimensional plane strain model, in terms of prediction of both the diaphragm wall lateral deformation and the vertical soil settlement. The maximum wall lateral deformation obtained using the 2D model was 54% greater than the in-situ measured values.
- In the Rod El Farag case, despite the relatively high aspect ratio (6.25) of the plan dimensions, the existence of cross walls significantly affected the lateral wall deformation. This is because the location of the maximum lateral wall deformation point was shifted from the mid-span of the whole primary wall length, to be at the mid-span point of every single panel.
- The higher stiffness not only at the primary wall corners but also at the cross wall locations significantly causes the three-dimensional behavior of the supported deep excavation systems, and the lateral wall deformation decreased with decreasing distance from both the wall corners and the cross walls.
- The three-dimensional stiffening effect at corners and cross walls has a significant impact not only on the lateral wall deformations but also on the neighboring soil vertical settlement.
- The zone influenced by deep excavation may be affected and depends mainly on the magnitude of absolute settlement and the slope angle of the settlement rough. For the Rod El Farag case, the vertical ground settlement became insignificant at a horizontal distance equal to one times the excavated depth from the diaphragm wall.
- In this case, the lateral wall movements (0.11% of excavated depth) were in good agreement with the practical approach proposed by Clough and O’Rourke (1990). However, Peck’s (1969) approach overestimated the induced deformation resulting due to deep excavation.
- Three-dimensional finite element analysis is recommended for deep excavation cases with internal cross walls, even for cases with relatively high aspect ratios.
Author Contributions
Funding
Conflicts of Interest
References
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Soil Layer Soil | Fill | Sandy Silty Clay | Sandy Clayey Silt | Silty Sand | Sandy Cobbles | Dense Sand/Gravel | Cobbles and Gravel | Med. to Fine Sand | |
---|---|---|---|---|---|---|---|---|---|
Parameter | |||||||||
Unit weight γsat (kN/m3) | 17 | 18 | 18 | 19.9 | 21 | 21 | 22 | 21 | |
Triaxial loading stiffness E50 (MPa) | 4 | 10 | 16 | 30 | 40 | 50 | 75 | 40 | |
Oedometer loading stiffness Eoed (MPa) | 4 | 10 | 16 | 30 | 40 | 50 | 75 | 40 | |
Triaxial unloading stiffness Eur (MPa) | 16 | 30 | 48 | 90 | 120 | 150 | 220 | 120 | |
Poisson’s ratio v (-) | 0.30 | 0.35 | 0.30 | 0.30 | 0.30 | 0.30 | 0.30 | 0.30 | |
Cohesion Cref (kPa) | 0.1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | |
Friction angle ϕ (degrees) | 28 | 30 | 30 | 34 | 36 | 38 | 40 | 36 | |
Dilatancy angle ψ (degrees) | 0 | 0 | 0 | 0 | 2 | 3 | 5 | 3 | |
lateral earth pressure coefficient (K0) | 0.53 | 0.5 | 0.5 | 0.44 | 0.412 | 0.38 | 0.33 | 0.412 | |
interface reduction factor (R) | 0.67 | 0.67 | 0.67 | 0.67 | 0.67 | 0.67 | 0.67 | 0.67 |
Element | Material | Unit Weight (kN\m3) | Thickness (m) | Poisson’s Ratio (-) | Modulus of Elasticity (MPa) |
---|---|---|---|---|---|
Diaphragm wall | Concrete | 25.0 | 1.20 | 0.15 | 24,100 |
Raft slab | Concrete | 25.0 | 2.20 | 0.15 | 24,100 |
Roof slab | Concrete | 25.0 | 1.40 | 0.15 | 24,100 |
Technical slab | Concrete | 25.0 | 1.10 | 0.15 | 24,100 |
Ticker slab | Concrete | 25.0 | 1.20 | 0.15 | 24,100 |
Strut Beams | Steel | 78.0 | 12.7 mm | 0.3 | 210,000 |
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Hefny, A.; Al-Atroush, M.E.; Abualkhair, M.; Alnuaimi, M.J. Three-Dimensional Response of the Supported-Deep Excavation System: Case Study of a Large Scale Underground Metro Station. Geosciences 2020, 10, 76. https://doi.org/10.3390/geosciences10020076
Hefny A, Al-Atroush ME, Abualkhair M, Alnuaimi MJ. Three-Dimensional Response of the Supported-Deep Excavation System: Case Study of a Large Scale Underground Metro Station. Geosciences. 2020; 10(2):76. https://doi.org/10.3390/geosciences10020076
Chicago/Turabian StyleHefny, Ashraf, Mohamed Ezzat Al-Atroush, Mai Abualkhair, and Mariam Juma Alnuaimi. 2020. "Three-Dimensional Response of the Supported-Deep Excavation System: Case Study of a Large Scale Underground Metro Station" Geosciences 10, no. 2: 76. https://doi.org/10.3390/geosciences10020076
APA StyleHefny, A., Al-Atroush, M. E., Abualkhair, M., & Alnuaimi, M. J. (2020). Three-Dimensional Response of the Supported-Deep Excavation System: Case Study of a Large Scale Underground Metro Station. Geosciences, 10(2), 76. https://doi.org/10.3390/geosciences10020076