SOIL IMPROVEMENT BY VACUUM PRELOADING FOR A POWER PLANT PROJECT IN VIETNAM

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18 th Southeast Asian Geotechnical & Inaugural AGSSEA Conference 29-31 May 213, Singapore Leung, Goh & Shen (eds) SOIL IMPROVEMENT BY VACUUM PRELOADING FOR A POWER PLANT PROJECT IN VIETNAM GOUW TJIE-LIONG 1 Civil Engineering, Binus Univeristy, Indonesia, gouw3183@binus.ac.id LIU YU 2 PT.Geotekindo, Indonesia, coolriverly@gmail.com ABSTRACT: A power plant project in South Vietnam was to be constructed on 16-3m depth very soft muddy clay layer. The project covered an area of 25.3 hectare. The very soft clay layer had a natural water content of around 58%, initial void ratio 1.594, and compression index.615. Vacuum preloading with an average PVD length of 26m and vacuum pressure of more than 8 kpa, was employed to improve the soft soil. The vacuum degree, surface and subsoil settlement, pore water pressure and lateral displacement were carefully monitored during the preloading period. After the vacuum preloading period of 117-15 days, ground surface settlement of 1.254-1.655 m correspond to a degree of consolidation over 9% was achieved. The maximum lateral displacement was 176mm in the direction towards the improved area. The after treatment Vane Shear Test yields undrained shear strength, Su, is 4 ~ 7 kpa. KEYWORDS: Vacuum preloading; soft muddy clay; vacuum degree; ground surface settlement; pore water pressure; lateral displacement. INTRODUCTION The proposed power plant is located at the entrance between two tributaries of Mekong River flowing into South China Sea. The landform is a typical delta formed by sea-land interaction and flood land at an edge of alluvial plain. Soil investigation result indicated that there is an extremely soft muddy clay layer with a thickness of 16.~3. m. Vacuum preloading method was adopted to improve soft soil in this project which covered an area of 25.3 hectare, divided to 1 zones during construction. The vacuum degree, surface and subsoil settlement, pore water pressure and lateral displacement were carefully monitored during the preloading period. The mechanism of vacuum preloading method and the monitoring data are presented and discussed in this paper. STRATUM CHARACTERISTICS According to the survey result, from 1m depth to the ground surface, all deposits are of Quaternary age. The subsoils where vacuum preloading soil improvement was applied were described below (from top to bottom): Layer 1-Backfill layer: embanked soil and late marine deposits. Light grey, hoar, loose, slightly dense, mainly filled with silty sand, newly formed and untreated, with thickness from.3m to 7.8m. Layer 2-Clay: Swamp and marine deposits. Dark grey, brownish grey, very soft, liquidplastic, contain large amount of organic matter and shell pieces, partially with lenses and pockets

of fine sand, with thickness from 17.5m to 25.m. Initial soil properties of layer 2 are listed in Table 1. Thickness contour of layer 2 is shown in Fig 1. Sub-layer 2a-Fine sand: Marine deposits, dark grey, black, loose, partially slightly dense. This layer is exposed in most boreholes and the distribution is continuous at 6. ~ 1.m depth under the ground. The thickness is normally.5m~3.m and maximum is 13.4m. Layer 3-Fine sand: Marine deposits, light grey, brown yellow, medium dense, partially slightly dense or dense. Below layer 3 is stiff ~ very stiff soil. Table 1. Original soil properties of layer 2. Items Unit Average value Water content w % 57.9 Unit weight γ w g/cm 3 16.3 Void ratio e 1.594 Compressibility Index C c.615 Coefficient of consolidation 1-3 cm 2 /s C v.74 C h.93 Fig 1. Thickness contour of the soft soil. DESIGN & CONSTRUCTION Vacuum preloading method utilizes atmospheric pressure as surcharge load to accelerate soil consolidation. Its principle is presented in Fig 2. Basically, whole vacuum preloading system consists of drainage system, sealing system and vacuum pumps. Vacuum pressure, generated in vacuum pumps, spreads into soils along drainage

system, taking out water and accelerating soil consolidation. The whole system is depicted in Fig. 3. The drainage system is an interconnected network of PVD, horizontal filter pipes and sand layer, forming a complete path for spreading of vacuum pressure and water flow. The sealing system is an airtight isolation system to prevent leakage of water & air below it. It consists of geomembrane, slurry wall and the soft clay itself. Due to its high permeability, the existence of sub-layer 2 which is a-fine sand in this project became a serious threat for the vacuum degree. Slurry wall was employed to cut off the water & air flow in this sub-layer 2a. The improvement area, total 253,83 m 2, was divided into 1 zones as shown in Fig 4. PVD were installed in square pattern of 1. m x 1. m spacing and an average depth of 26 m. The soil improvement target is to achieve 9% average degree of consolidation under vacuum pressure and backfilling loads. The information about backfilling height, preload and preloading time of each zone is listed in Table 2. 1-Total stress line, 2-initial water pressure line, 3-water pressure line after vacuum applied, 4- water pressure line if without head lose Fig 2. Principle of Vacuum Preloading Fig 3. Description of vacuum preloading system.

Fig 4. Layout of zone partition. Table 2. Construction Information of each Zone No. H(m) P(kPa) T(day) Zone 1 2.41 127 15 Zone 2 2.43 129 133 Zone 3 1.48 18 147 Zone 4 1.21 13 147 Zone 5 2.19 12 132 Zone 6 2.41 125 137 Zone 7 1.48 18 143 Zone 8 2.34 124 142 Zone 9 2.5 128 117 Zone 1 1.5 11 134 Note: H -- Backfilling Height P -- Total preload = vacuum pressure + backfilling load T Preloading time. MONITORING Monitoring System In order to control the effect of vacuum progress, the following monitoring schemes were conducted: Vacuum degree -- Vacuum gauges were installed to monitor vacuum degree under the geomembrane, 9 gauges for every zone.

Ground surface settlement -- Surface settlement plates were installed on top geotextile layer to monitor ground surface settlement, at least 9 plates for every zone. Subsoil settlement -- Layered settlement meters (extensometer) were installed at -4 m, -8 m, -12 m, -16 m, -2 m and -24 m in one borehole for every zone. Pore water pressure -- Water pressure meter (piezometer) were installed at -5 m, -1 m, -15 m and -2 m in one borehole, 3 boreholes for every zone. Lateral displacement -- Lateral displacement boreholes (inclinometers) were located at outside of boundary, total 4 boreholes. The monitoring layout and arrangement, taking zone 2 for example, is shown in Fig. 5. Monitoring frequency of each item is shown in Table 3. Monitoring frequency (interval) Fig 5. Monitoring meters arrangement. Table 3. Monitoring Frequency Vacuum Preloading Period First Month Consolidation Period Last Month Vacuum Pressure 1 day 2 days 2 days Surface Settlement 1 day 3 days 1 day Layered Settlement 1 day 3 days 2 days Pore Water Pressure 1 day 3 days 2 days Lateral Displacement 3 days 5 days 7 days Monitoring Data Analysis Vacuum degree is the key-point for vacuum preloading, especially the vacuum increasing in the beginning several weeks. Vacuum degree had been monitored and recorded very carefully and the result is shown in Fig 6. In this project, it takes 8 ~ 33 days for vacuum pressure to reach 8 kpa for different zones. The shortest is 8 days in zone 8 and zone 9 but the longest is 33 days in

zone 6. Basically, after the beginning period, the vacuum pressures were maintained over 8 kpa except some power off accidents which are clearly showed in Fig 6. Asaoka method was used to calculate consolidation degree for each zone based on surface settlement monitoring data. After 117 ~ 15 days preloading, all zones had reached consolidation degree requirement with surface settlement ranging from 1254 mm to 1655 mm. The average consolidation degrees are listed in Table 4. 8 Vacuum pressure(kpa) 6 Zone 1 Zone 2 Power off Zone 3 4 Zone 4 Zone 5 Zone 6 2 Zone 7 Zone 8 Zone 9 Zone 1 3 6 9 12 15 Time (Day) Fig 6. Vacuum degree curves. Fig 7. Contour of surface settlement. Table 4. Average Consolidation Degrees No. T day) P kpa) S con (mm) U Zone 1 15 127 1454 97% Zone 2 133 129 1445 97% Zone 3 147 18 1254 91% Zone 4 147 13 1458 99% Zone 5 132 12 167 99% Zone 6 137 125 1655 99% Zone 7 143 18 1295 99% Zone 8 142 124 1353 99% Zone 9 117 128 1496 96% Zone 1 134 11 1291 99% Notes: S con -- Surface settlement during preloading. U -- Average consolidation degree (by Asaoka method). Among the 1 zones, zone 6, zone 2 and zone 3 are typical zones which represent middle, side and corner zone respectively. Therefore, the monitoring data in these 3 zones will be further analyzed.

Surface settlement of the whole area is shown in Fig 7 which clearly indicates that maximum settlement took place in the middle and decreased from center to boundary. Relationship between load, settlement, pore water pressure and time in zone 2, zone 3 and zone 6 are showed in Fig 8, Fig 9 and Fig 1, respectively. Load (kpa) Settlement (mm) 16 12 8 4 Time (Day) 3 6 9 12 15 4 8 12 16 Suface -4m -8m -12m -16m -2m -24m Time (day) 3 6 9 12 15 2 Zone 2-5 5m 1m 15m 2m Fig 8. Relationship between Load, Settlement, Pore Water Pressure and Time in Zone 2. Pore water pressure (kpa) 15 1 5 Load (mm) Settlement(mm) 16 12 8 4 Time (Day) 3 6 9 12 15 4 8 12 16 Zone 3 Surface -4m -8m -12m -16m -2m -24m Water pore pressure (kpa) Time (day) 3 6 9 12 15 2 15 1 5-5 5m 1m 15m 2m Fig 9. Relationship between Load, Settlement, Pore Water Pressure and Time in Zone 3. Load (kpa) Settlement(mm) 16 12 8 4 4 8 12 16 3 6 9 12 15 Zone 6 Time (Day) Surface -4m -8m -12m -16m -2m -24m Water pore pressure (kpa) Time (day) 3 6 9 12 15 2 15 1 5-5 5m 1m 15m 2m Fig 1. Relationship between Load,Settlement, Pore Water Pressure and Time in Zone 6.

In zone 2, most settlement occurred at -4 ~ -24 m depth and the layered settlement seems nearly homogeneous. On the other hand, the settlement from m to -4 m depth was quite small, this is due to the fact that this 4m is the thickness of the platform, which could had been densified by the movement of trucks and equipment during the course of the site backfilling and preparation. Pore water pressure (u) decreased by 6 ~ 8 kpa rapidly after vacuum applied, especially in ~ - 15 m. However, at -2 m depth, the decreasing rate occurred in 2 stages, 1 st stage in the beginning 15 days and 2 nd stage in the following 3 ~ 9 days. This phenomenon can be found also in zone 3 and zone 6, which indicates that the influence of vacuum pressure could reach - 15m rapidly and tends to extend into deeper soil as time developing. In zone 3, distribution of layered settlement is different with zone 2, ~ -4 m offered 22% of total settlement but below -24m only offered 1%. However, the situation in zone 6 is very similar with zone 2. The distributions of layered settlement in these 3 zones are shown in Fig 11. Layered settlement (mm) 1 2 3 4 1 2 3 4 1 2 3 4 Depth(m) 4 8 12 16 2 24 28 6% 22% 1% 19% 2% 19% 19% 23% 23% 12% 13% 14% 2% 12% 23% 13% 9% 9% 1% 1% 11% Zone 2 Zone 3 Zone 6 Fig 11. Distributions of Layered Settlement. The monitoring data shows that vacuum degree, settlement and pore water pressure monitoring data clearly proved that the consolidation of soft clay had been almost finished due to the application of vacuum preloading method in this project and the influence of vacuum effect could reach -24 m or deeper. Lateral displacement monitoring result near zone 2, showed in Fig 12, clearly showed that the soil movement direction is inward with a maximum lateral movement of 176 mm. Since the vacuum pressure is isotropic, therefore, in the lateral direction an inward force is exerted on the subsoil which is totally different with surcharge preloading where no inward force is exerted. This means, in most cases, the sliding failure mechanism in vacuum method could be eliminated. POST TREATMENT SOIL TEST After vacuum preloading, laboratory test and field vane shear strength test were performed to check the soil property. The lab test result is listed in Table 5. Water content is reduced by 8.9% and compression index has been significantly improved. The vane shear strength test results, shown in Fig 13, indicates that the Su max is larger than 4 kpa and the average sensitivity is 3..

Displacement (mm) -2-15 -1-5 5 5 days 15 days 3 days 6 days 9 days 12 days 15 days 1 5 15 2 25 Depth (m) Note: - represents inward direction, + represents outward direction. Fig 12. Lateral displacement curves near zone 2. Table 5. Soil Parameter Comparison Items Unit Original Improved w % 57.9 49. γ w kn/m 3 16.3 17. e 1.594 1.352 C c.615.37 3 Fig 13. Field Vane Shear Strength Test Result.

DISCUSSION So far, many papers have discussed the mechanism of vacuum preloading method and several theories have been developed to explain the mechanism of this method. Besides, a lot of experiments and practices have been performed which provide precious data and cases to help understanding and applying this method better. In the authors opinion, the basic mechanism of vacuum preloading is the pore water pressure difference between vertical drains and the subsoil forces water to seep from thes subsoil into the vertical drains. For deep soil, although vacuum effect could not reach it by itself, the decreasing of pore water pressure in vertical drains still creates basis for consolidation. That is the reason why vacuum preloading influence can reach deeper soil. Furthermore, the suction forces generated by vacuum pumps keep accelerating water and air flowing, which effectively reduces the resistance in drainages. Therefore, consolidation time for vacuum preloading is usually shorter than conventional soil surcharging method. REFERENCES [1] Technical code for ground treatment of buildings. JGJ 79 22. [2] Technical specification for vacuum preloading technique to improve soft soils. JTS -2-29. [3] Gong Xiao-nan, Soil Improvement Manual, 3rd edition, China Architecture & Building Press, 28. [4] Gong Xiao-nan & Cen Yang-run. Mechanism of vacuum preloading. Journal of Harbin university of C. E. & Architecture, Vol. 35, No. 2, (22), pp 7-1. [5] Li Shi-liang. Analysis of action mechanism of treating soft foundation with vacuum preloading. Rock and soil mechanicals, Vol. 29, No. 2, (28), pp 479-482.