Introduction
The upsurge in construction of large scale excavations meeting the increasing demand for underground infrastructure in urban environments is made possible by either the top-down method [
1–
5] or the bottom-up method [
6–
8]. Consequently, subsequent or potential impacts on adjacent buildings and underground utilities due to ground movements have received more attention than ever before. A vast amount of field measurements has been obtained regarding performance of excavations. Many empirical or semi-empirical correlations have been developed for predicting excavation deformations based on these field measurements over the last two decades [
4,
7–
15]; however, the most of the excavations were in a rectangular shape or a pattern of strip with area sizes in a plan less than 10,000 m
2 and/or depths less than 30 m. Not much field monitored data is available for skyscraper development involved with the deep foundation pit. Since the performance of an excavation is affected by a complex set of factors that mainly consist of pit size, soil conditions, workmanship, retaining system, and underground water, the validity of these empirical or semi-empirical correlations may not be guaranteed when they are applied to large scale foundation pits. Tan and Wang conducted a series of investigations on the deformation of excavations, induced ground movements, and behaviors of unpropped/multipropped diaphragm walls based on two large-scale deep foundation pits and rectangular pits peripheral to the main buildings, one of which is the 420.5 m high skyscraper Jinmao Tower (JT), the other of which is 492 m Shanghai World Financial Center (SWFC) [
3,
8,
16,
17]. The comparison between the performance of these two foundation pits and a certain number of cylindrical excavations, basement excavations, and metro station excavations has been conducted in Shanghai soft clay. The central cylindrical shafts of these two skyscrapers were constructed by the bottom-up method by using deep diaphragm walls without bracing struts due to the sufficient spatial arching effect. The Shanghai Center is constructed to be the tallest building in China until 2015 with a topping-out height of 632 m, making it one of the tallest skyscrapers in the world. The excavation provides valuable information regarding the construction of a super foundation pit with an in-plan area of 12,000 m
2 (diameter 123.4 m) and with a depth of 33.7 m. So far, no building which exceeds 600 m in height exists on soft clay except for the Shanghai Center. This project serves as a distinctive case study on the deformation of a super excavation constructed through the top-down method by adopting circular diaphragm walls with six levels of cast-in-situ concrete struts. This information provides a significant guidance for making the performance predictions for similar projects in the future. The ground surface movements and deformations caused by soil type, construction technique, construction sequence, underground water, and retaining structures are emphasized in this paper based on the field measurements.
Project overview
Site conditions
The Shanghai Center was conceived to be a multi-functional and all-around super high-rise building. Fig. 1 presents the site plan view of the foundation pit, and additionally shows the portions of the annexes and surrounding high-rises. It is located at the most congested area, Lujiazui Finance and Trade Zone, in Shanghai and is bounded by the intersections of Central Yincheng, Garden Stone, Circle Lujiazui, and East Tai Streets, with a distance of 96 m away from the central cylindrical shaft of JT on the north side and a distance of 107 m away from the core-tube of SWFC on the east side. In addition, this area is surrounded by complicated underground pipelines and underground facilities, including Metro Line 2 in service and Line 14 in construction on the north side, as well as Metro Line 2 and 9 in service on the east side. As explained by Tan and Wang when the diameter of a cylindrical shaft exceeds 90 m, both the ring stiffness and spatial arching effect would be impaired significantly [
8]; thus, due to the weak spatial arching effect, it is extremely difficult to maintain retaining walls in a circular shape without support. This project involved the construction of a circular foundation pit which was constructed in an open multi-strutted excavation with a diameter of 123.6 m adjacent to several rectangular annex foundation pits. The whole foundation pit was comprised of two parts: the central pit and the peripheral pit. The excavation of the peripheral pit using the bottom-up method would be started after the underground facilities of the central pit completed by using the top-down method. This paper focuses on the observed performance of the central deep foundation with respect to lateral diaphragm wall movements, the ground settlements, and pit basal heave.
The site was previously occupied by Lujiazui Golf Course which contributed negligible net surcharge to the foundation soils. Prior to construction, Shanghai Geotechnical Investigations and Design Institute Company Limited (SGIDI) was appointed to conduct a comprehensive investigation regarding subsurface conditions and soil parameters. Fig. 2 illustrates the stratified soil layers at the site with the dimension of the foundation pit. The site is primarily composed of saturated clay, silty soil, and sandy soil, which are distributed in stratification. The borehole observation indicated that the site mainly consisted of fourteen layers, among which layer 8 was not detected according to unified strata of Shanghai soft clay made by Shanghai Construction and Management Commission (SCMC) [
18,
19]. The cast in place (CIP) concrete piles, with lengths of 52 to 56 m, were evaluated and chosen due to their high strengh and low construction cost. Only nine layers of compressible sands and clays, which alternated to a depth more than 110 m, were illustrated and considered as supporting layers providing frictional resistance. The main excavation portion, above the depth of 24 m, was dominated by cohesive soil characterized by high moisture content, high void ratio, high sensitivity, high compressibility, and low intensity. Both of the field tests (e.g., borehole observation, cone penetration test, vane shear test, dewatering test, and pressure meter test) and laboratory tests (e.g., consolidation test, compression test, and triaxial test) were carried out to obtain the site information. The variations of some important soil properties in average value along the depth are shown in Fig. 3. Granite as the bedrock was embedded 270 m below the ground surface, which was far beyond the reach of practical foundations. Bearing piles of the core tube reached a depth of 80 m where layer 9
2−1 of the dense silty sand was the bearing stratum. The phreatic water table fluctuates seasonally in elevations ranging from 0.75 to 3.9 m. The first and second aquifer (artesian water) was encountered at layer 7 with an average depth 30 m and layer 9 with an average depth 70 m, respectively. These two aquifers were connected with one another for a total thickness around 97 m. Sustainable and stable dewatering on-demand to lower level of the hydraulic pressure is a significant and challenging factor that impacts the safe and smooth construction of the foundation pit due to the complicated underground water conditions.
Construction procedure of the foundation pit
The top-down method was adopted to conduct the excavation of the central foundation pit which was supported by 50 m deep diaphragm wall with six levels of in situ concrete struts that correspond to six levels of excavation. The six-level excavation is based on the principle of the symmetrical, balanced, and layered excavation procedure. The whole excavation was divided into ten stages involving numerous tasks over a span of 14 months. The detailed information of each stage is summarized in Table 1. Except for level one excavation, the soils along the designed circumferential walls were dug out first and placed in the center of the site prior to removal, following the immediate manufacture of walls and strut framework and the casting of walls with struts. The soils at the center of the pit would be removed after the walls’ concrete at each level gained 80% concrete strength, then the next level of excavation would be initiated. Four lift platforms were built separately at north (No. 1), south (No. 2), west (No. 3), and east (No. 4) along the pit circumference for transferring soil, instruments, materials, and workers, which greatly facilitated the construction of the foundation pit. Circular diaphragm walls with high stiffness aiming to waterproof were adopted as the retaining walls, as well as the basement exterior walls. Prior to the first level excavation, a circular capping beam (CB) was built along the top of the diaphragm walls for the purpose of strengthening the vertical stiffness of the retaining structure. The whole circular diaphragm walls consisted of 70 panels, each of which would be constructed synchronously for the same level and connected without crevices except for construction joints. A uniform size of 176 m (length) × 1.20 m (thickness) was adopted, and a distance of 61.77 m between the turning place (connection between two panels) and the circle center of the pit was implemented for each panel. The six lateral levels of struts were concatenated by vertical columns for the purpose of making them perform together as well as fortifying the retaining system. The size of the struts is presented in Table 2. To accommodate the hazard of pit collapse caused by the inrushing of artesian water, pumping wells were installed along the pit circumference to reduce the water pressure by the dewatering that spanned from November 22, 2009 to April 5, 2010. The field recorded data demonstrates that smooth and fitting ground surface movements and ground deformations caused by symmetrical, balanced, and layered excavation procedure for deep circle pits could produce minimal adverse impact on retaining system.
Instrumentation
An extensive instrumentation program was undertaken alongside the foundation pit as well as the internal/peripheral soils to monitor the performance of the retaining systems, ground movements, and underground water. The monitoring system consisted of two categories based on different properties: one involves monitoring points where the monitoring facilities were anchored to structure parts, the other one refers to boreholes where monitoring facilities were placed in polyvinyl chloride (PVC) pipes or tubes. Fig. 4 shows the instrumentation layout of the boreholes and the monitoring points in the plan. The location and quantity of the monitoring facilities/items were determined by a series of factors (e.g., construction technology, the excavation depth, sequence, and observation objects), which attempt to arrange different monitoring facilities/items on the nearby locations or in the same soil profiles in consideration of facilitating the comparisons between different field measurements. The instrumentation used to monitor the ground surface movements and deformations for the foundation pit included:
1) Lateral movements of the diaphragm walls were measured by sixteen inclinometers (P01~P16) that were anchored to the reinforcement cages at an elevation of 45 m below the ground surface, among which inclinometer tubes P13 and P15 were damaged during the concreting.
2) Lateral movements of the peripheral soil were measured by fifteen inclinometers (T01~T15) that were placed in boreholes with an average depth of 60 m, and these boreholes were approximately 1.5 m behind the diaphragm walls.
3) Standpipes were installed inside (NS1~NS4) and outside (WS1~WS8) of the pit to observe phreatic water table, and observation wells were drilled inside (NY1~NY3) and outside (WY1~WY4) of the pit to observe the artesian water levels.
4) Subsurface settlement outside of the pit was measured by a settlement magnetic system (RI~R8) individually placed in boreholes with an interval of 5 m from the elevation –2.0 m along the depth.
5) Pit basal heave was recorded by four arrowhead magnets (C1~C4) at four platforms and two arrowhead magnets (C5 and C6) at the center of the pit from the elevation –32.0 m with an interval of 5 m.
Field performance
Walls and circumferential soil lateral movements
The walls’ lateral movements at P01 and P05, which are selected as typical measured sections, are summarized in Fig. 5. P01 was located at the north side and P5 at the east side. The lateral movement variations of the walls both along the depth and the excavation progress are separately illustrated. It is noticed that the lateral movements of the walls at these two points from stage 1 to stage 10 developed into a bulged profile moving toward the excavation side. However, during the casting of the base slab, both the retaining walls and the soils began to change the moving direction from inward (excavation side) to outward (ground side). Subtle outward displacement was found for the walls during stage 10. This reverse implies that the underground structures (e.g. base slab, basement) could play a role on restraining both retaining walls and ground moving inward. Such a phenomenon was also reported by Moormann and Tan and Wang [
3,
12]. The maximum lateral movement of the walls at P9 was 73.48 mm, the smallest one among all observation boreholes, while the maximum lateral movement of the walls at P11 was 97.2 mm. This discrepancy can be attributed to several factors: (1) P09 was near the lift platform No.2, and the deflection was suppressed to a certain extent due to the strengthened vertical stiffness of the walls because of the existence of the CIP piles that were used to support the platform; (2) P11 located at the driving zone of heavy trucks, which could increase the lateral load imposed on the walls; and (3) the joint between the wall panel W43 and T05 was designed as a casing connection, which is usually perceived as low integrality.
The characteristics of the lateral movements of the walls at different depths could be examined by placing monitoring instruments in the vertical walls along the depth. By averaging all observation boreholes, the walls’ maximum lateral movement (
) was 78.3 mm, which occurred at a depth (
, where
occurred) of 18 m below the ground surface that is equivalent to the excavation depth 33.7 m (
H) of this foundation pit. Many researchers have statistically analyzed the relationship between the maximum lateral movement of the walls and the excavation depth. Compared with the behaviors of the retaining walls for the deep excavations in soft soils worldwide,
this study is far below the upper boundary
[
25] and also below
[
20] or
[
21]. Liu and Lee et al. reported that the maximum wall deflections of some excavations occurred below the excavation bottom due to the thick layer of soft soils embedded below the excavation bottom [
22,
23]. Their conclusions were based on shallow excavations and cannot explain the changes of location of the walls’ maximum movement for deep excavations. In this case,
(18 m) was examined above the excavation bottom (33.7 m). Regarding deep excavations in soft soils, the highly-strengthened support system and/or the shorter distance from excavation bottom to stiffer bearing strata may make the maximum wall deflection occur above the excavation bottom. This study
matches well with the rule that most
ranged from
to
for cylindrical excavations in Shanghai soft clay by using the top-down method [
3].
Tan and Wang proposed a linear equation (
) to describe the relationship between the maximum lateral movement of the walls (
) and central pit diameter (
D) [
8]. The calculated
by using this equation for this study is 62.4 mm, which is smaller than the actual observed value 78.3 mm. This discrepancy might arise from several reasons: (1) this equation is a linear regression based on some cases that the shaft diameters are less than 90 m, while the diameter in this study is 123.4 m; (2) most cases that were used to infer this equation are less than 20 m in excavation depth; and (3) circular deep excavations with smaller diameter usually tend to deform less due to the spatial arching effect.
No toe movement of the retaining walls was found by screening the inclinometers in the walls. Liu et al. considered the ratio of embedded length of retaining walls (
) to the excavation depth (
H) as a significant fator that may contribute to toe deformation, and a large embedment ratio between 0.7 and 0.94 could help to impede the formation of toe deflection [
24]. However, Wang et al. concluded that no necessary correlation exists between embedment ratio and wall maximum lateral deflection by conducting a statistical analysis regarding the recent excavations in Shanghai soft soils [
14]. The embedment ratio of Shanghai Center is consistent with the conclusion of Wang et al. that an increase in the embedment ratio would not produce a corresponding decrease in maximum wall movement if the stability of the excavation had been ensured. The embedment ratio for Shanghai Center was 0.49, which was much smaller than the lower boundary 0.7 or the average value 0.96 for diaphragm walls in Shanghai soft soils [
14]. The lack of toe deflection detected with this irregular ratio might be ascribed to the high stiffness of the retaining walls supported by six level struts to guarantee the stability of the excavation.
The lateral movements of the circumferential soil behind walls were also monitored. By examining the recorded data, the soil lateral movements showed a deflection pattern similar to the lateral movements of the walls. Due to the similar variation trend, the measurements of the circumferential soil movements will not be presented here. The maximum lateral movement of the circumferential soil, , was 79.4 mm in average, which occurred at 17 m below the ground surface. The development of the walls and circumferential soil lateral movements mainly took place from stage 2 to 7 with the average accumulative lateral movement of 73.2 mm (93% of the maximum) and 72.4 mm (91% of the maximum) for the diaphragm walls and the circumferential soil, respectively. From stage 8 to stage 10, the wall and the soil lateral movements tended to decrease, and the location where the maximum lateral movements were measured moved gradually downward.
Peripheral soil vertical movements in layers and ground settlements
The magnetic system used to monitor the layered vertical settlements of peripheral soil at different depths was comprised of eight sections (RI~R8), each of which was located, respectively, at an elevation from −6 m to−56 m with an interval of 5 m. Hence, the whole site was divided into eleven layers. These eleven monitoring spots were installed 3 m behind the walls. Table 3 summarizes the accumulative vertical movements and the average vertical movements of each section at the end of the excavation. R1 and R5 are selected to illustrate the variations of layered vertical movements in different excavation stages and at different depths, which are presented in Fig. 6 (a) and Fig. 6 (b), respectively.
The layered vertical movements of the soils outside of the pit are affected by stress relief (soil removal), ground lateral movements, and dewatering. The monitoring spots at different depths displayed different vertical movements; the soils above-30.0 m tended to settle, and the settlement decreased with the increase of the depth, while the soils below-30.0 m presented a heave tendency, and the heave increased with the depth. The maximum layered soil settlement (
) was 58 mm, observed by R5 at a depth of-6 m. The extreme trend line between the maximum soil settlement and the excavation depth is
for this study, which falls into the range suggested by Clough and O’Rourke: the upper line
and the lower line
[
20]. The average trend line of this study
is also within the range between
and
proposed by Hashash et al. based on the medium stiff Blue Clay of Boston [
7]. Large settlements over 40 mm were found at the depth of−6 m and−11 m, while the monitoring spot at−26 m showed 10 mm settlement. The faster growth in heave was recorded between−31m and−46 m, but the heave growth slowed down below−46 m. On the other hand, the monitoring spots at the same section also exhibited different vertical movements in different stages. Similar deflection pattern was found for section R1 and R5: (1) heave changed slightly for monitoring spots below−16 m from stage 2 to stage 5, but increased rapidly during stage 6 to stage 8, and then stabilized to a fixed value after stage 9; (2) slight vertical movements occurred throughout the excavation for monitoring spots between−16 m and−41 m; and (3) settlement increased from stage 2 to stage 8 for monitoring spots above−16 m, and then reached a steady state in the construction of underground structures and facilities during stage 9 and 10. By examining the monitoring spots which showed settlements, the maximum settlement 60 mm was detected at−21 m of section R5. This result is in agreement with the maximum lateral movement of the retaining walls.
During stages 2, 3, and 4, the peripheral soil vertical movements were mainly controlled by stress relief (soil removal) and lateral movements of the ground. After the dewatering began in stage 5, the vertical movements of the soils above−21 m can be classified as settlement, but soils behaved as heave below−21 m. During stages 6 and 7, the peripheral soil below−31 m rebounded obviously. During stages 8, 9, and 10, soil deflections (settlement/heave) gradually stabilized, but little heave took place after the end of the dewatering on April 5, 2010. The recorded layered vertical movements of the peripheral soil indicate that the excavation exerted an influence on the heave of soils below the excavation bottom (−33.7 m).
The ground vertical movements of the four surrounding streets (Central Yincheng, Graden Stone, Circle Lujiazui, and East Tai Streets) were monitored and the results are shown in Fig. 7. In general, the ground vertical movements presented settlements that were dually affected by the soil removal and dewatering. The rate of settlements varied in different stages. During stages 2, 3, and 4, the rate decreased with the increase of the distance between the street and the central pit. The ground near the annexes settled more than the aforementioned streets, and small settlements were perceived on the surface of these four streets. With the growth of the excavation depth and initiation of the dewatering from stage 5 to 7, the ground settle rate significantly increased. The influence scope of the excavation expanded and a funnel-shape was developed in the settlement profile. The maximum ground settlement was found at a distance of 20 m from the annex. In stage 8, the ground vertical movements of these four streets were hardly affected by the excavation. Due to the end of the dewatering and the construction of base slab during stage 9 and 10, the ground tended to rebound while the heave rate was smaller than the settle rate.
Pit basal heave
Soil removal during excavation would directly cause the basal soils to rebound. Six groups of arrowhead magnets were used to monitor the basal heave. In each group, six arrowhead magnets were placed at depths of −31 m, −36 m, −41 m, −46 m, −51 m, and −56 m to measure the different heave amounts. Fig. 8 shows the recorded data of the heave amounts along the depth for all arrowhead magnets.
Before stage 4, the basal heave increased obviously due to the soil removal. After the dewatering began (stage 5), the soils above the artesian water level started to consolidate. The heave increased slowly, and sometimes behaved as settlement (i.e. C1 at the depth of-46.0 m) caused by consolidation which was larger than the heave. At the end of the excavation (stage 9), the heave gradually stabilized. In stage 10, the heave measurements did not take into account the settlement caused by the construction of the base slab and other underground structures.
The heave changed consistently with the excavation levels: the heave amounts increased when the soils were removed while decreased when the diaphragm walls and the struts were completed in each level. This corresponds to the conclusion that the stress relief would cause the basal soil to rebound while the retaining walls would suppress the soils moving toward the pit behind the walls. The vast subsurface beneath the excavation bottom was involved to generate a heave amount which was characterized by a decreasing tendency along the depth. For the arrowhead magnets at the center pit (C5 and C6), the measured heave amounts at−56 m of the both boreholes were higher than 35 mm, thus assuming that a great thick subsurface below the excavation bottom would rebound. The maximum basal heave amounts,
, that were measured at C5 and C6 are used to identify the relationship between the maximum basal heave and the excavation depth,
H. The range of the measured maximum basal heave in this excavation between
and
is much lower than the range between
and
that was proposed by Tan and Wang based on a certain amount of basement excavations in Shanghai soft clays [
8]. In addition, the relationship between the maximum basal heave,
, and the excavation diameter, D, was described as
.
Fig. 9 describes the relationship between the heave amount and the distance from the center of the pit to the measured points. It can be seen that the heave amounts at the center were higher than the periphery because the weight of the diaphragm walls and the struts could partially compensate the soil removal. In general, the basal heave might result from a comprehensive function of multiple factors: (1) rebounding due to soil removal; (2) consolidation induced by discharging of artesian water; (3) suppression from soils outside of the pit; and (4) squeezing by retaining walls.
Comparison with previous deep excavations in Shanghai
A database comprising 21 individual cylindrical excavations in top-down method was collected through Chinese journals, conference proceedings, master and doctor theses, and monographs to identify the relationship between excavation depth H (or foundation pit diameter D) and maximum lateral wall movement , maximum layered soil settlement , and maximum basal heave , respectively, as well as to compare this case to the previous deep excavations in Shanghai. In order to see the variation tendency between the embedded depth ratio () and, , and individually, charts of scatter with smooth lines were established. The observed values of , and for Shanghai Center are generally below the average values of the given database. The value of for this care is 0.49, which is almost the same with another three cylindrical excavations whose the values of excavation depth are around 30 m.The analysis in Fig. 10 and Fig. 11 exhibits the following features:
• There is a clear tendency that the embedded depth ratio () decreases with increasing the excavation depth for cylindrical excavations in top-down method. This case can be used to verify the fact that the stiffness of support system for deep excavations would be greatly enhanced that could mitigate the overturn risk caused by inadequate embedded depth. Therefore, further increase of the embedment length of the walls has a limited influence on the performance of the excavation. This result can provide design engineers an economical relevance for the design of deep excavations in soft clays.
• The depth where the maximum lateral wall movement () occurred would increase as the excavation depth increases. Values of generally range from to with an average value of for this database.
• From Fig. 10c, these results including maximum lateral wall movement (), maximum layered soil settlement (), and maximum basal heave () would increase as the excavation depth increases. The average values of , and are 0.28%H, 0.21%H , and 0.16%H , respectively. These three values for this case are in close proximity to the results of the database.
• No obvious relationship exists between embedded depth ratio () and foundation pit diameter (D). It seems that the foundation pit diameter is independent of the embedded depth ratio. A relationship reflects that the depth where occurred increases with increasing the foundation pit diameter.
• For all maximum lateral wall movement, maximum layered soil settlement, and maximum basal heave tend to increase as foundation pit diameter increases. The average values of , and are 0.057%D, 0.049%D , and 0.036%D , respectively.
• For less than 0.7, no evidence can be shown to demonstrate that relationships exist between and, , and individually. However, for more than 0.7, values of , , and tend to decrease slightly. There is an evidence of a trend for increasing the embedment length, more soils under the excavation surface are strengthened disregarding the excavations with less than 0.7. Consequently, less values of , , and will occur.
Analysis of FE models
A three-dimensional finite element (FE) model was made practical through recent advances in computational capabilities, including the formulation of tieback-soil interaction and iterative solvers in the MSC.Marc 3D program. A range of factors may be influencing the ground surface movements and deformations, including approximations in the representation of stratigraphy, initial ground surface, top of the wall elevations, and estimation of the wall bending stiffness or rotation stiffness in the FE models. Several idealizations and simplifications were made to reduce the complexity of the 3D program without affecting the accuracy of the output. The FE models are depicted in Fig. 12. The results in Fig. 13 show the predictive values of , , and seem to increase as the construction proceeded. The predictive values of , , and are 66 mm, 52 mm, and 30mm, respectively, which are smaller than the observed values of 97 mm, 58mm, and 35mm, respectively. It can be seen that the numerical analyses are capable of describing accurately the measured , , and variations throughout the construction process (six levels of struts) although the accuracy of the values may not be guaranteed. However, this simulation could be improved by considering some other complex factors. For example, analysis using a more complex soil model and accounting for partial drainage that spanned from November 22, 2009 to April 5, 2010 can be proposed as a further research.
Conclusions
To date, there is a scarcity of field data associated with deep excavations (≥30 m) in soft soils for super high-rise buildings. The deep excavation for the foundation pit of the Shanghai Center provides a good opportunity to obtain valuable information related to observed ground surface movements and ground deformations during construction. On the basis of results of the ground monitoring and analysis presented herein, the major conclusions with regard to the performance of the Shanghai Center excavation are enumerated as follows:
1) The measured maximum lateral movement of the walls occurred at –18 m with a value
that is far below the upper boundary
[
25],
[
20], and
[
21]. The maximum lateral movement of the circumferential soils,
, occurred at-17 m, which deformed consistently with the walls. The locations of both
and
fall in the range between
and
that were proposed by Tan and Wang based on cylindrical excavations in Shanghai soft clay [
3]. Contrary to the previous case studies, low embedment ratio 0.49 was adopted while no toe deflection emerged, which might be ascribed to the high stiffness of the retaining walls that were supported by six level struts to guarantee the stability of the excavation.
2) The layered settlement of the soils behind the walls is a common product of soil removal, ground lateral movements, and dewatering. The maximum soil settlement
is within the range between
and
suggested by Hashash et al. based on the medium stiff Blue Clay of Boston [
7]. The farther the distance between the street and the central pit, the lower ground settlement, thereby creating a funnel-shaped settlement profile for the ground settlement of the four surrounding streets. The maximum ground settlement was found at a distance of 20 m from the annex.
3) A great thick subsurface below the excavation bottom was involved to generate a heave for this deep excavation that was characterized by a decreasing tendency along the depth. The measured data indicated that the basal heave extended farther away from the excavation bottom than previously reported. The recorded maximum basal heave range between
and
, which is much lower than that ranging between
and
[
8]. A correlation between the maximum basal heave and the excavation diameter
is acquired. The heave generally decreased with the increase of the distance between the center of the pit and the measured point. Multiple factors (e.g., rebounding due to soil removal, consolidation induced by discharging of artesian water, suppression from soils outside of pit, and squeezing by retaining walls) may contribute to the heave development.
4) The results of the database analysis indicate that the average values of , and increase with increasing the excavation depth and/or excavation diameter. There appears to be no discernible relationship between embedded depth ratio () and foundation pit diameter (D). For more than 0.7, values of, , and tend to decrease slightly due to the fact that more soils under the excavation surface would be strengthened by prolonging the embedded length of retaining walls.
5) FE models were established for estimating the ground surface movements and deformations throughout the construction process. The predictive values of , , and are 66 mm, 52 mm, and 30mm, respectively, which are smaller than the observed values due the fact that some complex factor are simplified. However, the numerical analyses are capable of describing accurately the measured variations of , , and .
6) A retaining system was formed by combining the diaphragm walls and the circular struts in order to achieve an arching effect and bring compression resistance of concrete into full play. During the whole excavation, no big ground deflections that might lead to damage to the stability of the foundation pit were detected. This demonstrates that the construction sequence and excavation procedure (symmetrical, balanced, and layered) for this super foundation pit could guarantee the retaining system received minimal influence from the ground deformations.
Higher Education Press and Springer-Verlag Berlin Heidelberg