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Sanjay GuptaSanjay Gupta Ravi SundaramRavi Sundaram
Anurag GoyalAnurag Goyal
CENGRS GEOTECHNICA PVT. LTD.CENGRS GEOTECHNICA PVT. LTD.
Sanjay GuptaSanjay Gupta Ravi SundaramRavi Sundaram
Anurag GoyalAnurag Goyal
CENGRS GEOTECHNICA PVT. LTD.CENGRS GEOTECHNICA PVT. LTD.
Yamunanagar Power PlantYamunanagar Power Plant
Site on banks of River YamunaSite on banks of River Yamuna
Geotechnical investigations includedGeotechnical investigations included
•• BoreholesBoreholes
•• Static Cone Penetration TestsStatic Cone Penetration Tests
•• Plate Load TestsPlate Load Tests
For dynamic behavior of soilsFor dynamic behavior of soils
•• CrossCross--hole Seismic Testshole Seismic Tests
•• Seismic Refraction TestsSeismic Refraction Tests
Alluvial DepositsAlluvial Deposits
00 -- 3 m3 m : Clayey Silt: Clayey Silt
33 -- 55∼∼7 m7 m : Sand: Sand
55∼∼77 -- 15 m15 m : Boulders/pebbles: Boulders/pebbles
with sandwith sand
1515 -- 2020∼∼21 m21 m : Hard Clayey Silt: Hard Clayey Silt
2020∼∼21 m +21 m + : Very Dense Sand: Very Dense Sand
Typical Borehole ProfilesTypical Borehole Profiles
Static Cone Penetration TestStatic Cone Penetration Test
Tests for Dynamic ParametersTests for Dynamic Parameters
Seismic Refraction Tests along 5Seismic Refraction Tests along 5
lines : For global assessmentlines : For global assessment
•• Each line 250 m long covering theEach line 250 m long covering the
Power Block and CHP areaPower Block and CHP area
CrossCross--hole Seismic Tests in 6hole Seismic Tests in 6
boreholes to 25 m depth : Forboreholes to 25 m depth : For
specific localized profile with depthspecific localized profile with depth
•• at TG, Mill Crusher Houseat TG, Mill Crusher House –– location oflocation of
dynamically loaded foundationsdynamically loaded foundations
Seismic Refraction TestSeismic Refraction Test
Seismic Energy ApplicationSeismic Energy Application
To generate PTo generate P--
Wave, steel plate isWave, steel plate is
struck vertically withstruck vertically with
a 12 lbs hammera 12 lbs hammer
Data acquisitionData acquisition
using 24 geophonesusing 24 geophones
2424--channel signalchannel signal
enhancementenhancement
seismographseismograph
Seismic RefractionSeismic Refraction
Test SchematicTest Schematic
TravelTravel--Time RecordsTime Records
Seismic TravelSeismic Travel--TimeTime
DiagramDiagram
–– Data AnalysisData Analysis
Seismic Refraction TestSeismic Refraction Test
Geophones fixed along LineGeophones fixed along Line Close up View of GeophoneClose up View of Geophone
Embedded in GroundEmbedded in Ground
Seismic Refraction Test inSeismic Refraction Test in
progressprogress
Typical ResultsTypical Results
Lithology interpreted from SRTLithology interpreted from SRT
CrossCross--Hole Seismic TestsHole Seismic Tests
Horizontally traveling P & S WavesHorizontally traveling P & S Waves
are generated in a borehole atare generated in a borehole at
desired depthdesired depth
Arrival times are recorded at twoArrival times are recorded at two
adjacent receiver boreholes spaced 4adjacent receiver boreholes spaced 4
m apartm apart
Test conducted at every 1.5Test conducted at every 1.5--m depthm depth
intervalinterval
DownDown--hole Sensorshole Sensors
Geophone Assembly withGeophone Assembly with
inflatable bladderinflatable bladder
CloseClose--up view of orthogonalup view of orthogonal
Sensors encased in waterSensors encased in water--tighttight
assemblyassembly
CrossCross--hole Seismic Testhole Seismic Test
Geophone being
lowered in
borehole
SchematicSchematic –– CrossCross--holehole
Seismic TestSeismic Test
Source
Borehole
Receiver
Boreholes
Impact Hammer
Geophones
4 m 4 m
SeismographSeismograph
SPT Hammer as Energy SourceSPT Hammer as Energy Source
Data AcquisitionData Acquisition –– SeismicSeismic
TestsTests
Typical CHST ResultsTypical CHST Results
Plot of PPlot of P--WaveWave
velocity and Shearvelocity and Shear
Wave Velocity withWave Velocity with
depthdepth
VVpp and Vand Vss
correlated to E, Gcorrelated to E, G
andand μμ
P & S Wave VelocitiesP & S Wave Velocities
Depth
(m)
Soil
Classi-
fication
SPT
(N)
Value
qc
Value
kg/cm2
P-Wave
Velocity,
m/s
S-Wave
Velocity,
m/s
SRT CHST SRT CHST
0 – 3 Clayey Silt 8-10 10 -20
300-
600
300-
600
120-
250
105-
230
3 – 8 Fine Sand 15-30 40 -60
800-
900
600-
1000
400-
450
275-
450
8 – 13
Pebbles /
Cobbles with
Sand
50-
100+
Refusal
1600-
1800
1400-
2000
850-
1000
700-
975
>13
Hard Clayey
Silt / Dense
Sand
50+ >100
2100-
2600
2000-
2500
1050-
1300
900-
1100
Design ParametersDesign Parameters
Depth,
m
Lithology
Design
Vp
m/s
Design
Vs
m/s
Poisson’s
Ratio
E
MPa
G
MPa
0 – 3 Clayey Silt 450 180 0.40 165 59
3 – 8 Fine Sand 710 350 0.33 595 224
8 – 13
Pebbles /
Cobbles with
Sand
1650 850 0.30 3741 1439
>13
Hard Clayey
Silt / Dense
Sand
2000 1000 0.34 5198 1939
Published CorrelationsPublished Correlations
VVss (m/s) = 91 N(m/s) = 91 N0.3370.337 Imai (1977)Imai (1977)
G (MPa) = 12 NG (MPa) = 12 N0.80.8 Ohasaki &Ohasaki &
IwasakiIwasaki
LayerLayer NN
VVss
m/sm/s
GG
MPaMPa
1 9 191 70
2 25 270 158
3 200 543 831
4 75 390 380
Vs & G from NVs & G from N––valuevalue
correlations showcorrelations show
reasonable agreementreasonable agreement
for N<30for N<30
In hard/dense soils,In hard/dense soils,
NN--value correlationsvalue correlations
underestimate Vs & Gunderestimate Vs & G
Concluding RemarksConcluding Remarks
CrossCross--hole seismic tests and seismichole seismic tests and seismic
refraction tests provide useful datarefraction tests provide useful data
for design of dynamically loadedfor design of dynamically loaded
foundationsfoundations
Data superior to block vibration testData superior to block vibration test
Successfully used at YamunanagarSuccessfully used at Yamunanagar
Power PlantPower Plant
Thank You!Thank You!

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Dynamic characteristics of alluvial deposits a case study

  • 1. Sanjay GuptaSanjay Gupta Ravi SundaramRavi Sundaram Anurag GoyalAnurag Goyal CENGRS GEOTECHNICA PVT. LTD.CENGRS GEOTECHNICA PVT. LTD. Sanjay GuptaSanjay Gupta Ravi SundaramRavi Sundaram Anurag GoyalAnurag Goyal CENGRS GEOTECHNICA PVT. LTD.CENGRS GEOTECHNICA PVT. LTD.
  • 2. Yamunanagar Power PlantYamunanagar Power Plant Site on banks of River YamunaSite on banks of River Yamuna Geotechnical investigations includedGeotechnical investigations included •• BoreholesBoreholes •• Static Cone Penetration TestsStatic Cone Penetration Tests •• Plate Load TestsPlate Load Tests For dynamic behavior of soilsFor dynamic behavior of soils •• CrossCross--hole Seismic Testshole Seismic Tests •• Seismic Refraction TestsSeismic Refraction Tests
  • 3. Alluvial DepositsAlluvial Deposits 00 -- 3 m3 m : Clayey Silt: Clayey Silt 33 -- 55∼∼7 m7 m : Sand: Sand 55∼∼77 -- 15 m15 m : Boulders/pebbles: Boulders/pebbles with sandwith sand 1515 -- 2020∼∼21 m21 m : Hard Clayey Silt: Hard Clayey Silt 2020∼∼21 m +21 m + : Very Dense Sand: Very Dense Sand
  • 5. Static Cone Penetration TestStatic Cone Penetration Test
  • 6. Tests for Dynamic ParametersTests for Dynamic Parameters Seismic Refraction Tests along 5Seismic Refraction Tests along 5 lines : For global assessmentlines : For global assessment •• Each line 250 m long covering theEach line 250 m long covering the Power Block and CHP areaPower Block and CHP area CrossCross--hole Seismic Tests in 6hole Seismic Tests in 6 boreholes to 25 m depth : Forboreholes to 25 m depth : For specific localized profile with depthspecific localized profile with depth •• at TG, Mill Crusher Houseat TG, Mill Crusher House –– location oflocation of dynamically loaded foundationsdynamically loaded foundations
  • 8. Seismic Energy ApplicationSeismic Energy Application To generate PTo generate P-- Wave, steel plate isWave, steel plate is struck vertically withstruck vertically with a 12 lbs hammera 12 lbs hammer Data acquisitionData acquisition using 24 geophonesusing 24 geophones 2424--channel signalchannel signal enhancementenhancement seismographseismograph
  • 9. Seismic RefractionSeismic Refraction Test SchematicTest Schematic TravelTravel--Time RecordsTime Records Seismic TravelSeismic Travel--TimeTime DiagramDiagram –– Data AnalysisData Analysis
  • 10. Seismic Refraction TestSeismic Refraction Test Geophones fixed along LineGeophones fixed along Line Close up View of GeophoneClose up View of Geophone Embedded in GroundEmbedded in Ground
  • 11. Seismic Refraction Test inSeismic Refraction Test in progressprogress
  • 13. Lithology interpreted from SRTLithology interpreted from SRT
  • 14. CrossCross--Hole Seismic TestsHole Seismic Tests Horizontally traveling P & S WavesHorizontally traveling P & S Waves are generated in a borehole atare generated in a borehole at desired depthdesired depth Arrival times are recorded at twoArrival times are recorded at two adjacent receiver boreholes spaced 4adjacent receiver boreholes spaced 4 m apartm apart Test conducted at every 1.5Test conducted at every 1.5--m depthm depth intervalinterval
  • 15. DownDown--hole Sensorshole Sensors Geophone Assembly withGeophone Assembly with inflatable bladderinflatable bladder CloseClose--up view of orthogonalup view of orthogonal Sensors encased in waterSensors encased in water--tighttight assemblyassembly
  • 16. CrossCross--hole Seismic Testhole Seismic Test Geophone being lowered in borehole
  • 17. SchematicSchematic –– CrossCross--holehole Seismic TestSeismic Test Source Borehole Receiver Boreholes Impact Hammer Geophones 4 m 4 m SeismographSeismograph
  • 18. SPT Hammer as Energy SourceSPT Hammer as Energy Source
  • 19. Data AcquisitionData Acquisition –– SeismicSeismic TestsTests
  • 20. Typical CHST ResultsTypical CHST Results Plot of PPlot of P--WaveWave velocity and Shearvelocity and Shear Wave Velocity withWave Velocity with depthdepth VVpp and Vand Vss correlated to E, Gcorrelated to E, G andand μμ
  • 21. P & S Wave VelocitiesP & S Wave Velocities Depth (m) Soil Classi- fication SPT (N) Value qc Value kg/cm2 P-Wave Velocity, m/s S-Wave Velocity, m/s SRT CHST SRT CHST 0 – 3 Clayey Silt 8-10 10 -20 300- 600 300- 600 120- 250 105- 230 3 – 8 Fine Sand 15-30 40 -60 800- 900 600- 1000 400- 450 275- 450 8 – 13 Pebbles / Cobbles with Sand 50- 100+ Refusal 1600- 1800 1400- 2000 850- 1000 700- 975 >13 Hard Clayey Silt / Dense Sand 50+ >100 2100- 2600 2000- 2500 1050- 1300 900- 1100
  • 22. Design ParametersDesign Parameters Depth, m Lithology Design Vp m/s Design Vs m/s Poisson’s Ratio E MPa G MPa 0 – 3 Clayey Silt 450 180 0.40 165 59 3 – 8 Fine Sand 710 350 0.33 595 224 8 – 13 Pebbles / Cobbles with Sand 1650 850 0.30 3741 1439 >13 Hard Clayey Silt / Dense Sand 2000 1000 0.34 5198 1939
  • 23. Published CorrelationsPublished Correlations VVss (m/s) = 91 N(m/s) = 91 N0.3370.337 Imai (1977)Imai (1977) G (MPa) = 12 NG (MPa) = 12 N0.80.8 Ohasaki &Ohasaki & IwasakiIwasaki LayerLayer NN VVss m/sm/s GG MPaMPa 1 9 191 70 2 25 270 158 3 200 543 831 4 75 390 380 Vs & G from NVs & G from N––valuevalue correlations showcorrelations show reasonable agreementreasonable agreement for N<30for N<30 In hard/dense soils,In hard/dense soils, NN--value correlationsvalue correlations underestimate Vs & Gunderestimate Vs & G
  • 24. Concluding RemarksConcluding Remarks CrossCross--hole seismic tests and seismichole seismic tests and seismic refraction tests provide useful datarefraction tests provide useful data for design of dynamically loadedfor design of dynamically loaded foundationsfoundations Data superior to block vibration testData superior to block vibration test Successfully used at YamunanagarSuccessfully used at Yamunanagar Power PlantPower Plant