DETAILED INVESTIGATION OF PILES DAMAGED BY HYOGOKEN NAMBU EARTHQUAKE

Similar documents
STUDIES ON SEVARAL COUNTERMEASURES AGAINST LIQUEFACTION-INDUCED FLOW AND AN APPLIVATION OF A MEASURE TO EXISTING BRIDGES IN TOKYO

EFFECTS OF LIQUEFACTION-INDUCED GROUND DISPLACEMENTS ON PILE PERFORMANCE IN THE 1995 HYOGOKEN-NAMBU EARTHQUAKE

A STUDY ON DAMAGE TO STEEL PIPE PILE FOUNDATION ON RECLAIMED LAND DURING HYOGO-KEN-NANBU EARTHQUAKE

RESIDUAL DEFORMATION OF CAISSON, SHEET PILE AND GROUND BY SIMPLIFIED ANALYSIS

PILE FOUNDATION RESPONSE DUE TO SOIL LATERAL SPREADING DURING HYOGO-KEN NANBU EARTHQUAKE

Effective stress analysis of pile foundations in liquefiable soil

DYNAMIC RESPONSE AND FAILURE MECHANISMS OF A PILE FOUNDATION DURING SOIL LIQUEFACTION BY SHAKING TABLE TEST WITH A LARGE- SCALE LAMINAR SHEAR BOX

PILE DESIGN IN LIQUEFYING SOIL

SEISMIC PERFORMANCE OF URBAN, RECLAIMED AND PORT AREAS -FULL SCALE EXPERIMENT USING BLAST TECHNIQUE. Takahiro SUGANO 1) and Eiji KOHAMA 2)

EFFECTIVE STRESS ANALYSES OF TWO SITES WITH DIFFERENT EXTENT OF LIQUEFACTION DURING EAST JAPAN EARTHQUAKE

Field Investigation and Dynamic Analysis of Damaged Structure on Pile Foundation during the 2011 off the Pacific Coast of Tohoku Earthquake

RELATIONSHIP BETWEEN AGE OF GROUND AND LIQUEFACTION OCCURRENCE IN THE 2011 GREAT EAST JAPAN EARTHQUAKE

Tsukuba, Japan International Institute of Seismology and Earthquake Engineering Building Research Institute STUDY TRIP TO ITAKO CITY

HORIZONTAL LOAD DISTRIBUTION WITHIN PILE GROUP IN LIQUEFIED GROUND

Centrifuge Shaking Table Tests and FEM Analyses of RC Pile Foundation and Underground Structure

RELIQUEFACTION POTENTIAL OF CEMENT-TREATED SANDY SOILS

Residual Deformation Analyses to Demonstrate the Effect of Thin Steel Sheet Piles on Liquefaction-Induced Penetration Settlement of Wooden Houses

Study of the liquefaction phenomenon due to an earthquake: case study of Urayasu city

Experimental Study on Damage Morphology and Critical State of Three-Hinge Precast Arch Culvert through Shaking Table Tests

SIMPLIFIED ANALYSIS OF PILES SUBJECTED TO LATERAL SPREADING: PARAMETERS AND UNCERTAINTIES

AMPLIFICATION OF GROUND STRAIN IN IRREGULAR SURFACE LAYERS DURING STRONG GROUND MOTION

DAMAGE ANALYSIS OF WATER SUPPLY PIPES DUE TO THE 2004 NIIGATA-KEN CHUETSU, JAPAN EARTHQUAKE ABSTRACT

Liquefaction and Foundations

PROBABILISTIC LIQUEFACTION HAZARD ANALYSIS IN JAPAN

LIQUEFACTION STRENGTH OF COARSE WELL GRADED FILL UNDER TORSIONAL SIMPLE SHEAR

EARTHQUAKE OBSERVATION OF A LOW-RISE BUILDING

REPRODUCTION OF A LARGE-SCALE 1G TEST ON UNSATURATED SAND DEPOSITS AND PILE FOUNDATIONS USING CENTRIFUGE MODELING

EVALUATION OF STRENGTH OF SOILS AGAINST LIQUEFACTION USING PIEZO DRIVE CONE

CORRELATION BETWEEN INERTIAL FORCE AND SUBGRADE REACTION OF PILE IN LIQUEFIED SOIL

Comparison between predicted liquefaction induced settlement and ground damage observed from the Canterbury earthquake sequence

SIMPLIFIED METHOD IN EVALUATING LIQUEFACTION OCCURRENCE AGAINST HUGE OCEAN TRENCH EARTHQUAKE

MEDAT-2: Some Geotechnical Opportunities. Site Characterization -- Opportunities. Down-hole CPT & vane (Fugro)

DEVELOPMENT AND PERFORMANCE OF AN ACTIVE TYPE SHEAR BOX IN A CENTRIFUGE

Numerical Modelling of Dynamic Earth Force Transmission to Underground Structures

PREDICTION METHOD OF LIQUEFACTION AT FISHING VILLAGE IN KOCHI PREFECTURE BY NANKAI EARTHQUAKE

Experimental Study on The Seismic Assessment of Pile Foundation in Volcanic Ash Ground

COEFFICIENT OF DYNAMIC HORIZONTAL SUBGRADE REACTION OF PILE FOUNDATIONS ON PROBLEMATIC GROUND IN HOKKAIDO Hirofumi Fukushima 1

Study of Sand Boiling Characteristics Along Tokyo Bay During The 2011 Tohoku-Pacific Ocean Earthquake

ROAD BRIDGE DAMAGE DUE TO LIQUEFACTION DURING LEVEL-2 EARTHQUAKE IN KOBE

Model tests and FE-modelling of dynamic soil-structure interaction

ASIAN JOURNAL OF CIVIL ENGINEERING (BUILDING AND HOUSING) VOL. 10, NO. 5 (2009) PAGES **-**

DYNAMIC PROPERTIES OF STRUCTURE-PILE SYSTEM USING MOCK-UP MODEL

Author(s) Sawamura, Yasuo; Kishida, Kiyoshi;

EXPERIMENTAL AND NUMERICAL MODELING OF THE LATERAL RESPONSE OF A PILE BURIED IN LIQUEFIED SAND

THE STRUCTURAL DESIGN OF PILE FOUNDATIONS BASED ON LRFD FOR JAPANESE HIGHWAYS

Investigation of Liquefaction-induced Damage to Wooden Houses in Urayasu City Caused by the Great East Japan Earthquake

Estimation of Multi-Directional Cyclic Shear-Induced Pore Water Pressure on Clays with a Wide Range of Plasticity Indices

Y. Shioi 1, Y. Hashizume 2 and H. Fukada 3

Geo-Database Development in Kansai Area of Japan and Its Application in Assessing Liquefaction Potential

1368. Seismic behavior of pile in liquefiable soil ground by centrifuge shaking table tests

3-D Numerical simulation of shake-table tests on piles subjected to lateral spreading

NUMERICAL STUDY ON LATERAL SPREADING OF LIQUEFIED GROUND BEHIND A SHEET PILE MODEL IN A LARGE SCALE SHAKE TABLE TEST

STUDY OF THE BEHAVIOR OF PILE GROUPS IN LIQUEFIED SOILS

Seismic Response Analysis of Structure Supported by Piles Subjected to Very Large Earthquake Based on 3D-FEM

EFFECTS OF EARTHQUAKE-INDUCED SETTLEMENT OF CLAY LAYER ON THE GROUND SUBSIDENCE

Cyclic Behavior of Sand and Cyclic Triaxial Tests. Hsin-yu Shan Dept. of Civil Engineering National Chiao Tung University

ENCE 3610 Soil Mechanics. Site Exploration and Characterisation Field Exploration Methods

DAMAGE TO PILES DUE TO OSCILLATION OF LIQUEFYING GROUND

Investigation of Liquefaction Behaviour for Cohesive Soils

Seismic Responses of Liquefiable Sandy Ground with Silt Layers

Earthquake record from down-hole array observation in Tokyo bay area during the 2011 off the pacific coast of Tohoku earthquake

NUMERICAL ANALYSIS OF DAMAGE OF RIVER EMBANKMENT ON SOFT SOIL DEPOSIT DUE TO EARTHQUAKES WITH LONG DURATION TIME

Piles in Lateral Spreading due to Liquefaction: A Physically Simplified Method Versus Centrifuge Experiments

Damage of Houses and Residential Areas by Niigata Prefecture Earthquakes (Part 1)

Seismic Performance of a River Dike Improved by Sand Compaction Piles

Module 6 LIQUEFACTION (Lectures 27 to 32)

LATERAL SPREADING DURING CENTRIFUGE MODEL EARTHQUAKES

Comparison of different methods for evaluating the liquefaction potential of sandy soils in Bandar Abbas

Mitigation of Liquefaction Potential Using Rammed Aggregate Piers

ON-LINE PSEUDO-DYNAMIC RESPONSE TEST EVALUATION OF MULTILAYER SOIL IMPROVEMENT OF LIQUEFIABLE SOILS

Foundations on Deep Alluvial Soils

DYNAMIC CENTRIFUGE TEST OF PILE FOUNDATION STRUCTURE PART TWO : BEHAVIOR OF STRUCTURE AND GROUND DURING EXTREME EARTHQUAKE CONDITIONS

LIQUEFACTION INDUCED GROUND FAILURES CAUSED BY STRONG GROUND MOTION

Prediction of pile response to lateral spreading by 3-D soil-water coupled dynamic analysis: shaking in the direction of ground flow

DYNAMIC CENTRIFUGE TEST OF PILE FOUNDATION STRUCTURE PART ONE : BEHAVIOR OF FREE GROUND DURING EXTREME EARTHQUAKE CONDITIONS

AN EXPERIMETAL STUDY ON THE FLUID PROPERTIES OF LIQUEFIED SAND DURING ITS FLOW

CENTRIFUGE MODELING OF PILE FOUNDATIONS SUBJECTED TO LIQUEFACTION-INDUCED LATERAL SPREADING IN SILTY SAND

Effect of lateral load on the pile s buckling instability in liquefied soil

Liquefaction induced ground damage in the Canterbury earthquakes: predictions vs. reality

(THIS IS ONLY A SAMPLE REPORT OR APPENDIX OFFERED TO THE USERS OF THE COMPUTER PROGRAM

The Preliminary Study of the Impact of Liquefaction on Water Pipes

GEOTECHNICAL CRITERION FOR SERVICEABILITY LIMIT STATE OF HORIZONTALLY-LOADED DEEP FOUNDATIONS

Ömer AYDAN. Ismail FEBRIN. Fumihiko IMAMURA KOGAMI (Tsunami Alert Community-NPO)

K. Tokimatsu 1 and H. Arai 2. Professor, Dept. of Architecture and Building Engineering, Tokyo Institute of Technology, Japan 2

Keywords: Tohoku earthquake, Liquefaction, Hot spot, Pipeline damage, Topographic history

Static Pile Head Impedance using 3D Nonlinear FEM Analysis

SOME OBSERVATIONS RELATED TO LIQUEFACTION SUSCEPTIBILITY OF SILTY SOILS

IN SITU TESTING TECHNOLOGY FOR FOUNDATION & EARTHQUAKE ENGINEERING. Wesley Spang, Ph.D., P.E. AGRA Earth & Environmental, Inc.

Liquefaction. Ajanta Sachan. Assistant Professor Civil Engineering IIT Gandhinagar. Why does the Liquefaction occur?

NONLINEARITY IN SITE AMPLIFICATION AND SOIL PROPERTIES DURING THE 1995 HYOGOKEN-NAMBU EARTHQUAKE

Landslide FE Stability Analysis

NON-LINEAR ANALYSIS OF SOIL-PILE-STRUCTURE INTERACTION UNDER SEISMIC LOADS

A NUMERICAL STUDY OF DYNAMIC BEHAVIOR OF A SELF-SUPPORTED SHEET PILE WALL

Ground settlement due to shield tunneling through gravelly soils in Hsinchu

Department of National Defence B-Jetty Reconstruction

EARTHQUAKE SIMULATION TESTS OF BRIDGE COLUMN MODELS DAMAGED DURING 1995 KOBE EARTHQUAKE

Dynamic Response of EPS Blocks /soil Sandwiched Wall/embankment

1 PROJECT BACKGROUND. August 14, Alberta Transportation Central Region #401, Street Red Deer, Alberta T4N 6K8

Response of piles due to lateral slope movement

Evaluation of Geotechnical Hazards

Transcription:

DETAILED INVESTIGATION OF PILES DAMAGED BY HYOGOKEN NAMBU EARTHQUAKE Kenichi HORIKOSHI 1, Akira TATEISHI 2 And Hiroyasu OHTSU 3 SUMMARY Since the 199 Hyogoken Nambu earthquake, a number of detailed investigations have been conducted on damage to piles in the reclaimed islands of Kobe. This paper presents the results of a detailed investigation of 111 piles, which were driven more than years ago on one of the reclaimed islands of Kobe. The diameter of the piles varied from 4 mm to mm, and their lengths were 33 m or 36 m. There were two joints along the length of the piles, the upper segment of the piles was made of concrete covered with a steel pipe (SC pile), while the middle and lower segments were made of high strength pre-stressed concrete (PHC pile). Two things to note which were applicable to all 111 piles were: (1) At the time of the earthquake none of the piles was supporting a superstructure on top. Therefore, the damage to the piles were solely caused by soil during and after the earthquake. (2) All the piles were driven in the reclaimed island, however the distance from the nearest quay wall, which moved towards the sea about 2-4 m, was as far as 3 m. Therefore the effects of such large quay wall displacements were thought to be small. The methods used in the investigation of damage to the piles were (1) low strain integrity test, (2) visual inspection of pile damage from inside by using a water-proof CCD camera, and (3) pile deflection measured by means of a specially made inclinometer. The results of the investigation showed that all the piles were significantly damaged at a depth where a reclaimed soil layer existed. A major crack was found in almost all the piles at a depth of about 8 m, i.e. below the boundary between the reclaimed soil layers of coarse sand with gravel and medium sand with gravel. The horizontal residual displacement of the pile top was about - 4 mm. Interestingly, all the pile tops were inclined in the direction of the soil displacement, which was perpendicular to, and not along, the direction of major shaking. It was considered that differences in the dynamic soil responses between the above-mentioned two reclaimed sand layers caused such damage to the piles. INTRODUCTION Since the 199 Hyogoken Nambu Earthquake which struck Kobe city in Japan, a number of detailed investigations on the foundation damage have been reported such as [3],[4] and [6]. It is also well-known that the earthquake caused widespread liquefaction on almost all reclaimed islands in Kobe. Hamada et al [1] examined the distribution of the residual horizontal displacement of the soil, and found that soil near the waterfront lines moved by as much as 2-4 m towards the sea. 1 2 3 Taisei Research Institute, Taisei Corporation, Yokohama, Japan Email:kenichi.horikoshi@sakura.taisei.co.jp Civil Engineering Design Section, Taisei Corporation, Tokyo, Japan Email: tateishi@ce.taisei.co.jp Civil Engineering Department, Kyoto University, Kyoto, Japan Email: ohtsu@geotech.kuciv.kyoto-u.ac.jp

The investigations revealed that many piles in the liquefied soil suffered significant damages due to the effects of the earthquake. It, also, appears that the damage to piles was more pronounced near the waterfront possibly due to the large residual displacement of the quay walls. This paper presents the results of a detailed investigation of 111 slender piles damaged by the Hyogoken Nambu earthquake on one of the reclaimed islands, Fukae Hama, in the east part of Kobe city. As mentioned earlier there was no superstructure and footing on any of the pile tops at the time of the earthquake. Therefore, the piles were considered to be damaged only due to the effects of soil displacement related to liquefaction. Also, the nearest distance from the quay walls to the piles was as at least 3 m so that the effects of the large quay wall displacements were considered to be small. OUTLINE OF THE INVESTIGATION SITE The reclaimed island where the site was located suffered from significant liquefaction during and after the Hyogoken Nambu earthquake. The authors investigated the distribution of crack width which surfaced on the ground with distance from the waterfront line, as shown in Figure 1. According to the figure, the crack width was large within a distance up to m from the waterfront line. As the piles were at least 3 m from the quay walls it was therefore considered that the effects of the large quay wall displacements on the pile response at this site was small. Hamada et al.[1] reported that the soil at the site moved by about 1 m in the south-west direction based on analyses of aerial photographs before and after the earthquake. Figure 2 shows an overview of the investigation site. In the photograph, the pile tops are below the soil surface at a depth of about 1-2 m in the area where excavated soil can be seen. The excavation was conducted to expose the pile top which was necessary for conducting the investigation. Figure 3 shows a close-up photograph of one of the pile tops. In the photograph, a small hole can be seen close to the pile surface which was thought to be the result of soil liquefaction. The ground at the investigated area settled by about.4 -. m due to the soil liquefaction. Figure 4 illustrates the settlement. GROUND AND PILE CONDITIONS The distribution of the soil profiles with depth was investigated after the earthquake at a point close to pile No. (see Figure 7), and it is summarized in Figure. The soil profiles are shown up to a depth of.3 m below the soil surface. PS-logging was, also, conducted to investigate the shear wave velocity profile. 6 Crack width (mm) 4 3 3 Distance from waterfront lines (m) Figure 1: Distribution of crack width observed at the island Figure 2: Photograph of the investigation site in Kobe. 2

Figure 3: Hole found near pile surface Figure 4: Settlement of the fence near the site In Figure, the ground up to a depth of about 13 m below the surface is reclaimed soil which is called Masado (consisting of decomposed granite). The reclaimed soil at the site consists of three layers, i.e. gravel at the soil surface, medium sand with gravel and coarse sand with gravel, and their SPT N values and the shear wave velocities are slightly different. It should be noted that there was a slight change in SPT values and shear wave velocity at the boundary between the medium sand with gravel and coarse sand with gravel. The ground water level was at about 2.2 m below the soil surface. The F L value, i.e. liquefaction safety factor, was estimated from the soil profiles based on the Japanese Standard for Highway Bridges [2]. In the estimation, the correction factor for area, c z, was assumed to be unity, and the seismic intensity for the ground was set at k hc =.6. The calculated distribution of the F L value is shown in Figure 6 together with other soil profiles such as mean grain size and fine contents. The results show that the F L values were below. throughout most of the reclaimed soil. The total number of investigated piles was as many as 111, all of which were driven more than years ago. SPT N value Gravel Medium sand with gravel SC pile m Shear wave velocity 4 Coarse sand with gravel 1 Silty clay PHC pile 13 m 33 m SPT N FC 4 6 D (mm) 1234 F L. 1 1. 2 3 Clay 3 Sandy gravel PHC pile 1 m 4 4 1 Figure 6: F L value estimated from soil profiles Figure : profiles obtained after the earthquake 3

Figure 7 shows a plan of the pile arrangement at the site. 1 Diameter 4 mm Diameter mm Investigation by CCD camera Investigation by inclinometer Length : 36mm (Others 33 m) 42 m 149 197 Velocity response -1 Reflection from pile tip 3 Pile length (m) N Pile number 21 77 187 16 7 199 Figure 7: Plan of pile arrangements and investigation m (a) Result from undamaged pile of the same type Velocity response 1-1 Reflected wave 3 4 Pile length (m) Pile length = 33 m (b) Typical result obtained from the pile at the site Figure 8: Results obtained from low strain integrity tests The outside diameter of the piles was either 4 mm or mm, and the inside diameter of the piles was mm and 31 mm, respectively. The length of the piles was either 33 m or 36 m (see Figure 7). Each pile had two joints along its length. The upper segment of the pile is the so called SC pile, concrete pile covered by steel pipe and the middle and the lower segments are pre-stressed concrete piles (PHC piles). The tips of the piles were shaped as pencil tops and thud the pile tips were closed. RESULTS OF INVESTIGATION] Pile integrity tests: Firstly, low strain integrity tests were conducted for all 111 piles. In the tests, the response of reflected elastic wave from pile tip or the damaged section is analyzed to evaluate the pile integrity. A small impact was applied to the pile top by using a small plastic hammer. The reflected waves were measured by a small accelerometer with a high resolution. Figure 8(a) shows the result of the integrity test conducted on an undamaged pile which has the same components as the piles examined in this study. In the figure, the horizontal axis corresponds to the pile length, and the depth at which the incident waves are reflected is shown. According to the figure, a clear reflection can be seen at a depth of 24 m, which corresponds to the pile length. On the other hand, Figure 8(b) shows a typical response obtained from the piles at the investigation site. According to the figure, only a reflection from the relatively shallow depth of about m can be obtained, and no reflection from a depth corresponding to the pile length, i.e. 33 m, can be seen. The results obtained from all the piles were essentially the same as shown in Figure 8(b). Therefore, based on the integrity tests it was considered that the majority of the piles at the site might have some damage similar to that depicted in Figure 8(b). Investigation by CCD camera: A small water-proof camera was installed inside the hollow pile to visually investigate the damage. The camera used in the investigation had a capability to rotate around its vertical axis with the help of a remote control. The total number of piles investigated by the CCD camera was 8 (see Figure 7). An effort was made to remove as much water and soil inside each pile as possible by using a vacuum. However, in reality, ground water entered into the pile from the outside immediately after the removal probably through the cracks as shown later. The photographs of major damage taken by the CCD camera are shown in Figure 9 for the piles No. 7 and No. 199. Although it was rather difficult to quantify the crack size accurately from these photographs, it was 4

(a) Pile No 7, depth about 8 m (b) Pile No. 199, depth about 8.-9.m Figure 9: Pile damage observed by a CCD camera from inside No.16 (m) No. 21 (m) No. 7 (m) No. 77 (m) No. 149 No. 187 (m) (m) No. 199 (m) No. (m) Profile (m) Gravel N =7-3 Medium sand with gravel N =6 Coarse sand with grave N = - 14 Coarse sand with gravel 1 1 1 1 1 1 1 1 1? Silty clay Thicker line denotes more serious damage Figure : Summary of pile damage obtained from inspection by CCD camera possible to estimate the size by making comparisons with the size of the scale shown in the photograph. The actual width of the scale shown in the photograph was mm. Figure summarizes the findings of this investigation. In the figure, the thickness of the lines represents the size of the crack and the thicker the line the larger the crack. According to the figure, it can be seen that the integrity tests only found the shallowest damage. Large cracks were found in all the investigated piles indicating the severity of damage caused by the Hyogoken Nambu earthquake. The color of the crack as indicated by the photographs taken by the CCD camera was light gray, indicating that the cracks were created just before the investigation, i.e. at the time of the earthquake. At times the inside diameter of the damaged point was sometimes too narrow for maneuvering the CCD camera. The depth of the largest crack in all of the 8 piles investigated using the CCD camera was about 7-8 m from the soil surface, slightly below the boundary between the reclaimed soil layers of coarse sand with gravel and the medium sand with gravel. Investigation by inclinometer: The depths at which pile damage occurred were estimated from the two tests described above, and in the third series of test the pile deflection was investigated using a specially made inclinometer. The inclinometer used in the investigation is shown in Figure 11, and it is of the same type as the one used by Shamoto et al.[]. The inclinometer has a capability by which it can be installed on the inside of the pile wall by means of plate springs.

West (mm) East -3 - - South (mm) North - - 1 1 Figure 11: Inclinometer used for investigation North Pile No.7 E-W direction West (mm) East -3 - - (a) Pile No. 7 Pile No.7 S-N direction South (mm) North - 3 West 149 199 77 7 197 27 Number in each point denotes pile number. (mm) South East The inclination of the pile was measured at every mm spacing along the length of the pile. A total number of 7 piles were investigated by the inclinometer (see Figure 7). The pile deflections computed using the inclinometer readings have been summarized in Figure 12. Note that the point of zero deflection was taken at the deepest measured point, and that a correction was made to exclude the initial inclination of the piles occurring from the time of the installation. Since the pile tips are pencil shaped and they were driven into the soil, some inclination at the time of the installation was unavoidable. The figures clearly show that the piles deflected at a depth about 8- m from the pile top. Although the deflection patterns are almost the same for the investigated piles, it was also seen that some piles (pile No. 199 & ) deflected at two depths. The lower depth of the large deflection was about 12 m from the pile top as shown in Figure 12 (c). Figure 13 summarizes the direction of the pile deflection. The figure shows that all the piles deflected towards the 3 4 Figure 13: Displacement of each pile top estimated from results of inclinometer 1 Pile No.149 E-W direction West (mm) East -3 - - 1 Pile No. E-W direction 1 (b) Pile No. 149 Pile No.149 S-N direction South (mm) North - 3 1 (c): Pile No. Pile No. S-N direction Figure 12: Pile deflections obtained from inclinometer 6

southwest in the direction of the soil displacement as shown by Hamada et al [1]. The magnitude of the pile top displacement varied from mm to 4 mm and was smaller than the amount shown by Hamada et al. It should, also, be noted that the major direction of the shaking in the Hyogoken Nambu earthquake was from the northwest to the southeast. The direction of the pile deflection was perpendicular to the direction of main shaking. CONCLUSIONS The results of a detailed investigation of 111 piles which were considered to be damaged due to the effects of soil displacement during and after the 199 Hyogoken Nambu earthquake were reported in this paper. The findings of the investigation are: 1. Although not a single pile had a superstructure or footing above the pile at the time of the earthquake, significant damage was found in all the investigated piles. 2. The location of the damage was in all cases below the boundary between the reclaimed layers of coarse sand with gravel and medium sand with gravel. The two types of reclaimed soil are referred to as Masado, i.e. decomposed granite. The differences in the seismic responses of the two soil layers may have been the cause of such significant damage to the slender piles. 3. The displacements of all the pile tops were in the southwest direction, and they were in the same as the direction of the reported residual soil displacement based on an aerial photographic survey. Interestingly, the direction of the displacements was perpendicular to the direction of main shaking which was in direction of the northwest to the southeast. REFERENCES 1. Hamada, M., Isoyama, R., and Wakamatsu, K. (199), The Hyogoken-Nanbu (Kobe) earthquake, liquefaction, ground displacement and soil condition in Hanshin area, Association for development of Earthquake Prediction, The School of Science and Engrg., Waseda Univ. and Japan Engrg. Consultant Co., Ltd. 2. Japan Road Association (1996), Specifications for highway bridges, Vol. (in Japanese). 3. Karube, D., Kimura, M. (1996), Damage to foundations of railway structures, Special Issue of s and Foundations, pp. 1-2. 4. Matsui, T., Oda K. (1996), Foundation damage of structures, Special Issue of s and Foundations, pp. 189-.. Shamoto, Y., Sato M., Futaki, M. and Shimadu, S. (1996), A site investigation of post-liquefaction lateral displacement of pile foundation in reclaimed land, Tsuchi-to-Kiso, Japanese Geotechnical Society, Vol. 44, No.3, Ser. No. 48, pp. 2-27 (in Japanese). 6. Tokimatsu, K., Mizuno, H. and Kakurai, M. (1996), Building damage associated with geotechnical problems, Special Issue of s and Foundations, pp. 291-234. 7