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In situ rock stress measurements
from existing tunnels with LVDT-cell
LVDT-cell version II
Eight radial
LVDT sensors
Rock and cell
temperature sensors
Electronics
O-ring based
mounting system
Mounting
tool
Batteries & USB-memory
Online cable
Measurement location and hole layout
Mine niche
-400 m
Raisebored shaft
-310 m
OC
-12 cm
- 63 cm
SC 80 cm
- 10 cm
- 50 cm
SC 90 cm
- 66 cm
- 10 cm
SC 75 cm
- 46 cm
-15 cm
OC
- 50 cm
- 10 cm
R1
R2
R3
R4
R6
R5
S-tunnel
TBM
Measurement location and hole layout
TBM-tunnel
-450
Drill and blast
S-tunnel
-450 m
LVDT measurement
Measurement holes
Selecting measurement location
- sparcely fractures
- middle of blast round
Overcoring to by pass EDZ
- raise bore or TBM: 0 cm
- drill and blast: 25-50cm
Pilot / installation hole
- Ø 126 mm
- min free length 35 cm
Overcoring
- Ø ≥ 200 mm
min 5 cm
Min OC length 35 cm
EDZ
LVDT-probe
Hole dimensions
Calibration of the cell
Measurement phases
Drilling the 126 mm pilot hole
Overcoring
Cooling
Biaxial testing
Measurement phases
Biaxial testing
3D photogrammetry
3D-photogrammetry
Profiles
Defining the measurement hole
Locations and orientations
Y=North
R1
R3
R4
R5
Building the 3D-model
Building the 3D-model for inversion
Calculation of in situ state of stress
- best fit inverse solution between measured and simulated convergences
- requires 3D-numerical simulations of geometries ( BEM, FEM, DEM )
- assumes linear elastic isotropy or known transverse isotropy
- analytical solution for surface measurements on circular excavation
( considered as gigantic overcoring measurement )
For 3D-model
- 3D-photogrammetric model
- all holes can be in the same model if
far enough from each other
Interpretation
For the inversion
To get orthogonal displacements components
at each LVDT sensor head
- i.e., 6 × 3 displacements for each head location
Six runs:
1) sEE = 1MPa
2) sNN = 1MPa
3) sUU = 1MPa
4) sEN = 1MPa
5) sNU = 1MPa
6) sUE = 1MPa
- other five components are set to zero
- measured mean E and n
u1
N,sij
u1
E,sij
u1
U,sij
Interpretation
Inversion
In the case of linear elasticity the LVDT sensor head displacements caused
by any in situ stress state, ie. ( k×sEE, l×sNN, m×sUU, n×sEN, o×sNU, p×sUE ),
can be constructed by superimposing the multiplied displacement components
caused by each unit stress tensor:
ui(ksEE, lsNN, msUU, nsEN, osNU, psUE ) = k×ui(sEE=1) + l×ui(sNN=1) + m×ui(sUU=1) +
n×ui(sEN=1) + o×ui(sNU=1) + p×ui(sUE=1),
i=E,N,U
-> Best fit between measured and calculated convergence can be found
using a focused iterative search
Interpretation
-> side coring can be used
- to prevent ring disking
4.98e-002
9.10e-002
1.21e-001
9.10e-002
4.98e-002
2.82e-002
2.17e-002
2.82e-002
126.700
200.000
36.650
0
3
2
2
2
2
2
2
2
2
2
2
1
1
1
1
-300 -250 -200 -150 -100 -50 0 50 100 150
deformed shapes
orignal shapes
Solution method does not require full stress release,
because solution uses displacement differences
between the phases before and after coring
Side coring
Side coring
CASE 1
Äspö Hard rock laboratory
Äspö Hard Rock Laboratory
measurements in well known stress state (-450m level)
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
TBM
- bearing 248°, plunge 8°
TASS
- bearing 218°, plunge 0.6° (up)
- drill and blast
TBM
TASS
TBM
TASS
Sidecoring responce
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
Stability of LVDT probe readings
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
LVDTs looking from tunnel
to the measurement hole
Measurement
location
OC_Start
OC_End, 35 cm
0
5
10
15
20
25
30
35
40
45
50
-0.02
0
0.02
0.04
0.06
0.08
0.1
0.12
18:00 19:30 21:00 22:30 0:00 1:30 3:00 4:30 6:00 7:30 9:00
Temperature
(C)
Diametric
deformation
(mm)
R1-50 - 90 (1+5)
R1-50 - 135 (2+6)
R1-50 - 00 (3+7)
R1-50 - 45 (4+8)
OC_Start
OC_End, 35 cm
Values for calc.
Measured convergences
LVDT pair dL at OC-stop (µm) dL/1 h (µm) dL/12 h (µm)
(1+5) 41 2 0
(2+6) 63 0 -2
(3+7) 19 2 2
(4+8) -2 3 3
Results - TASS biaxial tests
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
0
20
40
60
80
100
R1 R2 R3 R4 R6
Young's
Modulus
(GPa)
Sample
SurfaceA
SurfaceB
Deep A
Deep B
0
0.05
0.1
0.15
0.2
0.25
0.3
0.35
0.4
R1 R2 R3 R4 R6
Poisson's
ration
()
Sample
SurfaceA
SurfaceB
Deep A
Deep B R1
R2
R3
R4
R6
R5
Elastic parameters from LVDT pilot cores
- no diffrence in mean values
between EDZ and deep samples
- no difference related to location
( stress state )
- EDZ samples have higher variation
Results - in situ stress orientation
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
Sigma_1
Sigma_2
Sigma_3
North
East
Trend 90
dip=60 dip=30 dip=0
Sigma_1
Sigma_2
Sigma_3
North
East
Trend 90
dip=60 dip=30 dip=0
TASS Axis
TASS TBM
TBM Axis
248°
Deep
solid signals
Surface
open signals
Christiansson &
Jansson (2003)
Christiansson &
Jansson (2003)
Constrained
to be H/V
Results - in situ stress magnitude
Note, Vertical bars are for sH, sh and sV according to Christiansson & Jansson (2003)
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
24.6
18.9
13.6
13.4
9.2
9.8
0 10 20 30
Deep,
Final values
Deep,
OC Stop values
Surface,
Final values
Surface,
OC Stop values
Principal stress ( MPa )
Sigma 1 Sigma 2 Sigma 3
TASS, drill and blast
Deep,
Final values
Surface,
Final values
Principal stress (MPa)
TBM
25.6
22.0
14.1
0 10 20 30
Final, All
Final, All, H/V
All, OC-Stop
Principal stress ( MPa )
Sigma 1 Sigma 2 Sigma 3
Final values
OC stop values
Final values,
constrained
to be H/V
Principal stress (MPa)
Deep,
OC stop values
Surface,
OC stop values
Quality of the solution
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
TASS, drill and blast TBM
y = 1.01x
R² = 0.84
y = 0.67x
R² = 0.82
-60
-40
-20
0
20
40
60
80
100
-60 -40 -20 0 20 40 60 80 100
Calculated
Convergence
(microstrain)
Measred Convergence (microstrain)
Deep, final
Surface, final
y = 0.98x
R² = 0.97
-100
-50
0
50
100
150
200
-100 -50 0 50 100 150 200
Measured convergence (microstrain)
Measured convergence (microstrain)
Calculated
convergence
(microstrain)
Calculated
convergence
(microstrain)
Summary
Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
- deep measurements have excellent agreement with traditional borehole
techniques
- the higher internal error and distortion of surface measurement solution
supports the existence of an excavation disturbed zone (EDZ)
-> minimum measurement depth should be 50 cm
- clear advantages of the methodology are the capability to manage with short
boreholes and a compact drill rig, and avoiding the issues associated with
gluing and the time needed for curing
- method also involves large volume, avoids effect of small scale heterogeneity
σH
MPa
σH trend
(RT90)
σh
MPa
σv
MPa
Christiansson &
Jansson (2003) 24 ±5 136° 10 - 13 12
This study
Deep, > 0.5 m 23-24 136°-139° 12-13 10-11
www.smcoy.fi
matti.hakala@smcoy.fi

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LVDT cell stress measurements for insitu rock stress measurement

  • 1. In situ rock stress measurements from existing tunnels with LVDT-cell
  • 2. LVDT-cell version II Eight radial LVDT sensors Rock and cell temperature sensors Electronics O-ring based mounting system Mounting tool Batteries & USB-memory Online cable
  • 3. Measurement location and hole layout Mine niche -400 m Raisebored shaft -310 m
  • 4. OC -12 cm - 63 cm SC 80 cm - 10 cm - 50 cm SC 90 cm - 66 cm - 10 cm SC 75 cm - 46 cm -15 cm OC - 50 cm - 10 cm R1 R2 R3 R4 R6 R5 S-tunnel TBM Measurement location and hole layout TBM-tunnel -450 Drill and blast S-tunnel -450 m
  • 5. LVDT measurement Measurement holes Selecting measurement location - sparcely fractures - middle of blast round
  • 6. Overcoring to by pass EDZ - raise bore or TBM: 0 cm - drill and blast: 25-50cm Pilot / installation hole - Ø 126 mm - min free length 35 cm Overcoring - Ø ≥ 200 mm min 5 cm Min OC length 35 cm EDZ LVDT-probe Hole dimensions
  • 7. Calibration of the cell Measurement phases Drilling the 126 mm pilot hole
  • 10. Defining the measurement hole Locations and orientations Y=North R1 R3 R4 R5 Building the 3D-model Building the 3D-model for inversion
  • 11. Calculation of in situ state of stress - best fit inverse solution between measured and simulated convergences - requires 3D-numerical simulations of geometries ( BEM, FEM, DEM ) - assumes linear elastic isotropy or known transverse isotropy - analytical solution for surface measurements on circular excavation ( considered as gigantic overcoring measurement ) For 3D-model - 3D-photogrammetric model - all holes can be in the same model if far enough from each other Interpretation
  • 12. For the inversion To get orthogonal displacements components at each LVDT sensor head - i.e., 6 × 3 displacements for each head location Six runs: 1) sEE = 1MPa 2) sNN = 1MPa 3) sUU = 1MPa 4) sEN = 1MPa 5) sNU = 1MPa 6) sUE = 1MPa - other five components are set to zero - measured mean E and n u1 N,sij u1 E,sij u1 U,sij Interpretation
  • 13. Inversion In the case of linear elasticity the LVDT sensor head displacements caused by any in situ stress state, ie. ( k×sEE, l×sNN, m×sUU, n×sEN, o×sNU, p×sUE ), can be constructed by superimposing the multiplied displacement components caused by each unit stress tensor: ui(ksEE, lsNN, msUU, nsEN, osNU, psUE ) = k×ui(sEE=1) + l×ui(sNN=1) + m×ui(sUU=1) + n×ui(sEN=1) + o×ui(sNU=1) + p×ui(sUE=1), i=E,N,U -> Best fit between measured and calculated convergence can be found using a focused iterative search Interpretation
  • 14. -> side coring can be used - to prevent ring disking 4.98e-002 9.10e-002 1.21e-001 9.10e-002 4.98e-002 2.82e-002 2.17e-002 2.82e-002 126.700 200.000 36.650 0 3 2 2 2 2 2 2 2 2 2 2 1 1 1 1 -300 -250 -200 -150 -100 -50 0 50 100 150 deformed shapes orignal shapes Solution method does not require full stress release, because solution uses displacement differences between the phases before and after coring Side coring
  • 16. CASE 1 Äspö Hard rock laboratory
  • 17. Äspö Hard Rock Laboratory measurements in well known stress state (-450m level) Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel TBM - bearing 248°, plunge 8° TASS - bearing 218°, plunge 0.6° (up) - drill and blast TBM TASS TBM TASS
  • 18. Sidecoring responce Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel
  • 19. Stability of LVDT probe readings Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel LVDTs looking from tunnel to the measurement hole Measurement location OC_Start OC_End, 35 cm 0 5 10 15 20 25 30 35 40 45 50 -0.02 0 0.02 0.04 0.06 0.08 0.1 0.12 18:00 19:30 21:00 22:30 0:00 1:30 3:00 4:30 6:00 7:30 9:00 Temperature (C) Diametric deformation (mm) R1-50 - 90 (1+5) R1-50 - 135 (2+6) R1-50 - 00 (3+7) R1-50 - 45 (4+8) OC_Start OC_End, 35 cm Values for calc. Measured convergences LVDT pair dL at OC-stop (µm) dL/1 h (µm) dL/12 h (µm) (1+5) 41 2 0 (2+6) 63 0 -2 (3+7) 19 2 2 (4+8) -2 3 3
  • 20. Results - TASS biaxial tests Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel 0 20 40 60 80 100 R1 R2 R3 R4 R6 Young's Modulus (GPa) Sample SurfaceA SurfaceB Deep A Deep B 0 0.05 0.1 0.15 0.2 0.25 0.3 0.35 0.4 R1 R2 R3 R4 R6 Poisson's ration () Sample SurfaceA SurfaceB Deep A Deep B R1 R2 R3 R4 R6 R5 Elastic parameters from LVDT pilot cores - no diffrence in mean values between EDZ and deep samples - no difference related to location ( stress state ) - EDZ samples have higher variation
  • 21. Results - in situ stress orientation Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel Sigma_1 Sigma_2 Sigma_3 North East Trend 90 dip=60 dip=30 dip=0 Sigma_1 Sigma_2 Sigma_3 North East Trend 90 dip=60 dip=30 dip=0 TASS Axis TASS TBM TBM Axis 248° Deep solid signals Surface open signals Christiansson & Jansson (2003) Christiansson & Jansson (2003) Constrained to be H/V
  • 22. Results - in situ stress magnitude Note, Vertical bars are for sH, sh and sV according to Christiansson & Jansson (2003) Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel 24.6 18.9 13.6 13.4 9.2 9.8 0 10 20 30 Deep, Final values Deep, OC Stop values Surface, Final values Surface, OC Stop values Principal stress ( MPa ) Sigma 1 Sigma 2 Sigma 3 TASS, drill and blast Deep, Final values Surface, Final values Principal stress (MPa) TBM 25.6 22.0 14.1 0 10 20 30 Final, All Final, All, H/V All, OC-Stop Principal stress ( MPa ) Sigma 1 Sigma 2 Sigma 3 Final values OC stop values Final values, constrained to be H/V Principal stress (MPa) Deep, OC stop values Surface, OC stop values
  • 23. Quality of the solution Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel TASS, drill and blast TBM y = 1.01x R² = 0.84 y = 0.67x R² = 0.82 -60 -40 -20 0 20 40 60 80 100 -60 -40 -20 0 20 40 60 80 100 Calculated Convergence (microstrain) Measred Convergence (microstrain) Deep, final Surface, final y = 0.98x R² = 0.97 -100 -50 0 50 100 150 200 -100 -50 0 50 100 150 200 Measured convergence (microstrain) Measured convergence (microstrain) Calculated convergence (microstrain) Calculated convergence (microstrain)
  • 24. Summary Experience with a new LVDT-Cell to measure in-situ stress from an existing tunnel - deep measurements have excellent agreement with traditional borehole techniques - the higher internal error and distortion of surface measurement solution supports the existence of an excavation disturbed zone (EDZ) -> minimum measurement depth should be 50 cm - clear advantages of the methodology are the capability to manage with short boreholes and a compact drill rig, and avoiding the issues associated with gluing and the time needed for curing - method also involves large volume, avoids effect of small scale heterogeneity σH MPa σH trend (RT90) σh MPa σv MPa Christiansson & Jansson (2003) 24 ±5 136° 10 - 13 12 This study Deep, > 0.5 m 23-24 136°-139° 12-13 10-11