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CASE STUDY OF SAND DRAINS-KANSAI INTERNATIONAL
AIRPORT
1.INTRODUCTION
Kansai International Airport (KIX) is an international airport located on an artificial
island in the middle of Osaka Bay, 38 km (24 mi) southwest of Osaka Station, located within
three municipalities, including Izumisano (north), Sennan (south), and Tajiri (central), in
Osaka prefecture, Japan. It is the first 24-hour operational airport in Japan and constructed 5km
offshore in Osaka bay as a man-made island in order to avoid the impact of aircraft noise on
residential areas (Figure 1.1). Kansai opened 4 September 1994 to relieve overcrowding
at Osaka International Airport. An artificial island, 4 km (2.5 mi) long and 2.5 km (1.6 mi)
wide, was proposed.Kansai International airport features 24-hour operability, convenience of
transfer between international and domestic flights, and diverse accesses by highway, railways
and high-speed ferry.
Figure 1.1. Location of Kansai International Airport
(Furudoi,2006)
In 1990, a three kilometer bridge was completed to connect the island to the mainland at Rinku
Town. In the Kansai International Airport, the number of aircraft take-offs and landings is
already close to its handling capacity (30 per hour) during peak hours. Based on pressure from
both home and abroad to further increase its capacity as an international hub airport, the second
phase of the construction project was started in 1999.The 4,000 m × 60 m second runway was
opened on 2 August 2007.
Figure 1.2. Kansai International Airport
(Furudoi,2006)
2.Natural condition
The water depth of the construction site is about 18m to 20m. The Figure 1.3 shows a general
overview below the seabed at the construction site. The layers below the seabed consist of a
soft layer of Holocene clay immediately below the seabed surface and alternative layers of
Pleistocene clay and sand/gravel. Pleistocene clay deposited from 2 million to 10 thousand
years ago during repeated glacial and interglacial periods. The depth andthickness of each clay
layer gently become greater as it goes towards offshore side, as shown in Figure 2.1.
Figure 2.1 General overview of seabed under airport islands
(Furudoi,2006)
Large settlement as a result of reclamation work was expected because of these compressible
clay layers of great thickness. Holocene clay layer was particularly thick and weak. Therefore,
Holocene clay layer should be improved so as to minimize the residual and uneven settlement
which will occur after the airport open its operation and to ensure the stability during the
construction of the island. The ground improvement was carried out by driving many sand
piles into the Holocene clay layer. Sand piles squeeze water from Holocene clay layer, thus
promoting settlement by consolidation of the layer. As a result, it was estimated that the
settlement of Holocene clay layer will be completed during the construction. On the other hand,
it was difficult to improve the Pleistocene clay layers technologically. For this reason, the
natural Pleistocene clay layers continue to subside after the airport was opened. Thus, based
on the results of large depth borings and laboratory tests, long-term settlement of the
Pleistocene clay layerswere predicted and reflected in the design of thickness of reclamation.
3.The first phase of the project
In the first phase project, an airport island of about 510ha was reclaimed, on which one 3,500m
runway, takeoff/landing facilities and terminal facilities were built. To swiftly carry out
largescale reclamation works in deep water was an extremely difficult and unprecedented task.
Various improvements in operation and technological innovations made it possible.
The first phase of the construction project at Kansai International Airport started in 1987.
Holocene clay layer was improved mainly by sand drain method in order to promote settlement
and to increase soil strength at an early stage. In the first phase construction, 1 million sand
columns were driven. This was followed by construction of an 11km long seawall around the
island. Then reclamation inside the seawall was carried out. In the first phase construction,
about 180 million m3 of soil was required for development of the island.
After reclamation work, airport facilities including the run-way and the passenger terminal
were built, and in September 1994, a little over seven years since the start of the construction,
the airport opened its operation.
3.1 The second phase of the project
In order to meet the growing demand for air transportation, the airport functions should be
expanded. Kansai International Air-port launched its second phase construction in July of 1999
to complement its current facilities with an additional 4000m run-way. The second phase of
the project involved development of another man-made island of 545ha land 200m off the
existing air-port island. Thus the natural conditions were more unfavorable than for the first
phase construction. The thickness of compressible clay layers and the water depth of the second
phase construction site were greater than those of the first phase. The second phase island was
expected to settle more than the first phase. In the second phase construction, extraordinary
large-scale construction was conducted in a limited period of time, overcoming these severe
conditions. To complete the airport island, the latest technologies were introduced as well as
the experience accumulated during the first phase construction.
Figure 3.1 Overview of the first and second airport island of KIA(Furudoi,2006)
4.CONSTRUCTION
An artificial island, 4 km long and 2.5 km wide, was proposed. Construction was started in
1987. First, ground improvement works for Holocene clay layer mainly using a sand drain
method were carried out. After that, the seawall was built all round the island site to start
execution of the reclamation. The reclamation work consists of three stages: soil dumping by
hopper barges, soil heaping by re-claimer barges and multi-layered construction by
bulldozers and rollers. Figure 4.1 shows procedure of construction
Figure 4.1 Procedure of construction (Multi-layered construction is in progress.)
(Furudoi,2006)
4.1 Ground improvement work
The subsoil immediately below the seabed surface consists of a thick, weak Holocene clay
layer, which should be improved so as to minimize the residual or uneven settlement after the
airport open its operation and to ensure the stability during the seawall construction and
reclamation. The ground improvement work was carried out throughout the entire seawall and
reclamation area.
5. Spreading of sand blanket
In the ground improvement work, first, a 1.5m thick layer of sea sand was carefully laid and
spread evenly over the seabed as a blanket. The sand blanket allows the water discharged from
Holocene clay layer to pass out and disperses the load caused by the seawall construction and
reclamation. In the spreading sand blanket, two methods were available, the pump method and
the tremie pipe method (Figure 5.1). The sand blanket was created in 2 or 3 layers by sand
spreading barges.
(a) Pump method (b) Tremie pipe method
Figure 5.1. Methods of sand spreading(Furudoi,2006)
Because of depletion of sea sand in the Seto Inland Sea, which was a source of sea sand close
to the construction site, substitutes were used in some part of sand blanket. One of the
substitutes was graded aggregate of nonstandard crushed stone. Because the grain size of
graded aggregate was larger than that of other materials, it was used for upper part of sand
blanket as a cushion to reclamation. Another substitute was and imported sand from China
Korea. The imported sand was directly carried into the construction site by large vessels after
checking the influence on the natural environment since it was the first case in Japan.
To secure the high quality material for permeable layer, grain size distribution of sand was
checked at each source in advance. Furthermore, the fine fraction content of materials was also
checked to be less than 10% by simple method with coagulant on all barges.
6.Ground improvement
The ground improvement was carried out, following the spreading sand blanket. In the
construction site, the sand drain method (SD), the sand compaction pile method (SCP), the
deep mixing method (DM) and the marine plastic drain method (MPD) wers adopted. Figure
2.3 shows the location of each method of ground improvement. The outlines of the ground
improvement methods are described below.
SD : Sand drain method SCP : Sand compaction pile method
DM : Deep mixing method MPD: Marine plastic drain method
Figure 6.1. Ground improvement applied in the construction(Furudoi,2006)
7.Sanddrain method
In the second phase construction as well as in the first phase, a sand drain method was applied
to most parts of the seawall construction area and all of the reclamation area. Sand piles of
40cm diameter were driven into Holocene clay with average thickness of 25m by sand piling
barges (Figure 7.1). The domestic sea sand was used for sand piles and its quality was checked
in the same manner as sand blanket. Spacing of the sand piles was set at 2.5m × 2.5msquare
grid, excluding the area beneath the seawall with spacing of 1.6m × 2.5m rectangular grid
(Figure7.2). The two spacing distances were determined by consolidation analysis solution by
Baron. The narrower spacing for the seawall area was set in order to achieve early strengthening
of Holocene clay with a more accelerated degree of consolidation, because seawall construction
preceded reclamation.
Figure 7.1 Sand-piling barge
According to a finite element consolidation analysis, the spacing of 1.6m × 2.5m is equivalent
to a spacing of 2.0m × 2.0m in terms of degree of consolidation (Kobayashi, 1976). The spacing
of 1.6m × 2.5m was set for efficient construction, since intervals of pile drivers of sand piling
barges were 2.5m. Furthermore, for continuous and seamless placing of sandpiles between
reclamation area and seawall area, the rectangular spacing is applied for the seawall area
(Maeda, 1989). Because thickness of Holocene clay layer becomes greater towards offshore
side, the sand piles in the second construction site were longer than those in the first.
Furthermore, it was apprehended that large settlement of Holocene clay layer might induce
discontinuity or large deformation of the sand piles. Therefore, in order to ensure the effect of
promoting consolidation, the sand piles were driven to the sand layer beneath Holocene clay
layer so that the water could be squeezed through the sand layer as well as the sand blanket.
The pile drivers were confirmed to reach the sand layer, based on penetration resistance
evaluated by rate or load of penetration.
Figure7.2 Spacing of sand drain piles
The criterion of the penetration resistance of each sand piling barge was determined by
penetration test carried out at the site where the thickness of Holocene claylayer was obtained
by boring. The sand piles were driven into the prescribed points precisely by positioning control
system of sand piling barge linked with RTK-GPS. The sand piles were simultaneously driven
in the area of 30m width because the sand piling barges were equipped with 12 pile drivers
with interval of 2.5m. The sand piling barges carried out driving sand piles by unit area of
100m × 90m (30m × 3) where the sand piling barges could drive sand piles without weighing
anchors by controlling length of four anchoring cables. About 1.2 million sand piles were
driven in 16 months from August 1999 by 8 sand piling barges.

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Case study

  • 1. CASE STUDY OF SAND DRAINS-KANSAI INTERNATIONAL AIRPORT 1.INTRODUCTION Kansai International Airport (KIX) is an international airport located on an artificial island in the middle of Osaka Bay, 38 km (24 mi) southwest of Osaka Station, located within three municipalities, including Izumisano (north), Sennan (south), and Tajiri (central), in Osaka prefecture, Japan. It is the first 24-hour operational airport in Japan and constructed 5km offshore in Osaka bay as a man-made island in order to avoid the impact of aircraft noise on residential areas (Figure 1.1). Kansai opened 4 September 1994 to relieve overcrowding at Osaka International Airport. An artificial island, 4 km (2.5 mi) long and 2.5 km (1.6 mi) wide, was proposed.Kansai International airport features 24-hour operability, convenience of transfer between international and domestic flights, and diverse accesses by highway, railways and high-speed ferry. Figure 1.1. Location of Kansai International Airport (Furudoi,2006) In 1990, a three kilometer bridge was completed to connect the island to the mainland at Rinku Town. In the Kansai International Airport, the number of aircraft take-offs and landings is already close to its handling capacity (30 per hour) during peak hours. Based on pressure from both home and abroad to further increase its capacity as an international hub airport, the second phase of the construction project was started in 1999.The 4,000 m × 60 m second runway was opened on 2 August 2007.
  • 2. Figure 1.2. Kansai International Airport (Furudoi,2006) 2.Natural condition The water depth of the construction site is about 18m to 20m. The Figure 1.3 shows a general overview below the seabed at the construction site. The layers below the seabed consist of a soft layer of Holocene clay immediately below the seabed surface and alternative layers of Pleistocene clay and sand/gravel. Pleistocene clay deposited from 2 million to 10 thousand years ago during repeated glacial and interglacial periods. The depth andthickness of each clay layer gently become greater as it goes towards offshore side, as shown in Figure 2.1.
  • 3. Figure 2.1 General overview of seabed under airport islands (Furudoi,2006) Large settlement as a result of reclamation work was expected because of these compressible clay layers of great thickness. Holocene clay layer was particularly thick and weak. Therefore, Holocene clay layer should be improved so as to minimize the residual and uneven settlement which will occur after the airport open its operation and to ensure the stability during the construction of the island. The ground improvement was carried out by driving many sand piles into the Holocene clay layer. Sand piles squeeze water from Holocene clay layer, thus promoting settlement by consolidation of the layer. As a result, it was estimated that the settlement of Holocene clay layer will be completed during the construction. On the other hand, it was difficult to improve the Pleistocene clay layers technologically. For this reason, the natural Pleistocene clay layers continue to subside after the airport was opened. Thus, based on the results of large depth borings and laboratory tests, long-term settlement of the Pleistocene clay layerswere predicted and reflected in the design of thickness of reclamation. 3.The first phase of the project In the first phase project, an airport island of about 510ha was reclaimed, on which one 3,500m runway, takeoff/landing facilities and terminal facilities were built. To swiftly carry out
  • 4. largescale reclamation works in deep water was an extremely difficult and unprecedented task. Various improvements in operation and technological innovations made it possible. The first phase of the construction project at Kansai International Airport started in 1987. Holocene clay layer was improved mainly by sand drain method in order to promote settlement and to increase soil strength at an early stage. In the first phase construction, 1 million sand columns were driven. This was followed by construction of an 11km long seawall around the island. Then reclamation inside the seawall was carried out. In the first phase construction, about 180 million m3 of soil was required for development of the island. After reclamation work, airport facilities including the run-way and the passenger terminal were built, and in September 1994, a little over seven years since the start of the construction, the airport opened its operation. 3.1 The second phase of the project In order to meet the growing demand for air transportation, the airport functions should be expanded. Kansai International Air-port launched its second phase construction in July of 1999 to complement its current facilities with an additional 4000m run-way. The second phase of the project involved development of another man-made island of 545ha land 200m off the existing air-port island. Thus the natural conditions were more unfavorable than for the first phase construction. The thickness of compressible clay layers and the water depth of the second phase construction site were greater than those of the first phase. The second phase island was expected to settle more than the first phase. In the second phase construction, extraordinary large-scale construction was conducted in a limited period of time, overcoming these severe conditions. To complete the airport island, the latest technologies were introduced as well as the experience accumulated during the first phase construction.
  • 5. Figure 3.1 Overview of the first and second airport island of KIA(Furudoi,2006) 4.CONSTRUCTION An artificial island, 4 km long and 2.5 km wide, was proposed. Construction was started in 1987. First, ground improvement works for Holocene clay layer mainly using a sand drain method were carried out. After that, the seawall was built all round the island site to start execution of the reclamation. The reclamation work consists of three stages: soil dumping by hopper barges, soil heaping by re-claimer barges and multi-layered construction by bulldozers and rollers. Figure 4.1 shows procedure of construction Figure 4.1 Procedure of construction (Multi-layered construction is in progress.) (Furudoi,2006)
  • 6. 4.1 Ground improvement work The subsoil immediately below the seabed surface consists of a thick, weak Holocene clay layer, which should be improved so as to minimize the residual or uneven settlement after the airport open its operation and to ensure the stability during the seawall construction and reclamation. The ground improvement work was carried out throughout the entire seawall and reclamation area. 5. Spreading of sand blanket In the ground improvement work, first, a 1.5m thick layer of sea sand was carefully laid and spread evenly over the seabed as a blanket. The sand blanket allows the water discharged from Holocene clay layer to pass out and disperses the load caused by the seawall construction and reclamation. In the spreading sand blanket, two methods were available, the pump method and the tremie pipe method (Figure 5.1). The sand blanket was created in 2 or 3 layers by sand spreading barges. (a) Pump method (b) Tremie pipe method Figure 5.1. Methods of sand spreading(Furudoi,2006) Because of depletion of sea sand in the Seto Inland Sea, which was a source of sea sand close to the construction site, substitutes were used in some part of sand blanket. One of the
  • 7. substitutes was graded aggregate of nonstandard crushed stone. Because the grain size of graded aggregate was larger than that of other materials, it was used for upper part of sand blanket as a cushion to reclamation. Another substitute was and imported sand from China Korea. The imported sand was directly carried into the construction site by large vessels after checking the influence on the natural environment since it was the first case in Japan. To secure the high quality material for permeable layer, grain size distribution of sand was checked at each source in advance. Furthermore, the fine fraction content of materials was also checked to be less than 10% by simple method with coagulant on all barges. 6.Ground improvement The ground improvement was carried out, following the spreading sand blanket. In the construction site, the sand drain method (SD), the sand compaction pile method (SCP), the deep mixing method (DM) and the marine plastic drain method (MPD) wers adopted. Figure 2.3 shows the location of each method of ground improvement. The outlines of the ground improvement methods are described below. SD : Sand drain method SCP : Sand compaction pile method DM : Deep mixing method MPD: Marine plastic drain method Figure 6.1. Ground improvement applied in the construction(Furudoi,2006) 7.Sanddrain method In the second phase construction as well as in the first phase, a sand drain method was applied to most parts of the seawall construction area and all of the reclamation area. Sand piles of 40cm diameter were driven into Holocene clay with average thickness of 25m by sand piling barges (Figure 7.1). The domestic sea sand was used for sand piles and its quality was checked in the same manner as sand blanket. Spacing of the sand piles was set at 2.5m × 2.5msquare grid, excluding the area beneath the seawall with spacing of 1.6m × 2.5m rectangular grid (Figure7.2). The two spacing distances were determined by consolidation analysis solution by
  • 8. Baron. The narrower spacing for the seawall area was set in order to achieve early strengthening of Holocene clay with a more accelerated degree of consolidation, because seawall construction preceded reclamation. Figure 7.1 Sand-piling barge According to a finite element consolidation analysis, the spacing of 1.6m × 2.5m is equivalent to a spacing of 2.0m × 2.0m in terms of degree of consolidation (Kobayashi, 1976). The spacing of 1.6m × 2.5m was set for efficient construction, since intervals of pile drivers of sand piling barges were 2.5m. Furthermore, for continuous and seamless placing of sandpiles between reclamation area and seawall area, the rectangular spacing is applied for the seawall area (Maeda, 1989). Because thickness of Holocene clay layer becomes greater towards offshore side, the sand piles in the second construction site were longer than those in the first. Furthermore, it was apprehended that large settlement of Holocene clay layer might induce discontinuity or large deformation of the sand piles. Therefore, in order to ensure the effect of promoting consolidation, the sand piles were driven to the sand layer beneath Holocene clay layer so that the water could be squeezed through the sand layer as well as the sand blanket. The pile drivers were confirmed to reach the sand layer, based on penetration resistance evaluated by rate or load of penetration.
  • 9. Figure7.2 Spacing of sand drain piles The criterion of the penetration resistance of each sand piling barge was determined by penetration test carried out at the site where the thickness of Holocene claylayer was obtained by boring. The sand piles were driven into the prescribed points precisely by positioning control system of sand piling barge linked with RTK-GPS. The sand piles were simultaneously driven in the area of 30m width because the sand piling barges were equipped with 12 pile drivers with interval of 2.5m. The sand piling barges carried out driving sand piles by unit area of 100m × 90m (30m × 3) where the sand piling barges could drive sand piles without weighing anchors by controlling length of four anchoring cables. About 1.2 million sand piles were driven in 16 months from August 1999 by 8 sand piling barges.