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![Page 1: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/1.jpg)
Introduction to the Task A Task Force Meeting
B. Garitte and A. Gens
2nd DECOVALEX 2011 workshop, 20th of October 2008, Wakkanai , Japan
Dept. of Geotechnical Engineering and GeosciencesTECHNICAL UNIVERSITY OF CATALONIA (UPC)
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Data from VE test (NF-PRO)
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Schedule of Task A
Background of Task A
Description of step 0
Participants
Index
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Schedule of Task A
Step 0: Identification of relevant processes and of Opalinus Clay parameters. Modelling of the
laboratory drying test.
Step 1: Hydromechanical modelling up to the end of Phase 1.
Step 2: Hydromechanical modelling up to the end of Phase 2 using parameters
backcalculated from step 1. Advanced features as permeability anisotropy, rock damage and
permeability increase in the damaged zone may be considered.
Step 3: Hydromechanical and geochemical modelling of the full test. Conservative transport
and one species considered.
Step 4: Hydromechanical and geochemical modelling of the full test. Reactive transport and
full geochemical model (optional).
![Page 5: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/5.jpg)
Schedule of Task A
Step 0: Identification of relevant processes and of Opalinus Clay parameters. Modelling of the
laboratory drying test.
Step 1: Hydromechanical modelling up to the end of Phase 1.
Step 2: Hydromechanical modelling up to the end of Phase 2 using parameters
backcalculated from step 1. Advanced features as permeability anisotropy, rock damage and
permeability increase in the damaged zone may be considered.
Step 3: Hydromechanical and geochemical modelling of the full test. Conservative transport
and one species considered.
Step 4: Hydromechanical and geochemical modelling of the full test. Reactive transport and
full geochemical model (optional).
![Page 6: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/6.jpg)
Schedule of Task A
Step 0: Identification of relevant processes and of Opalinus Clay parameters. Modelling of the
laboratory drying test.
Step 1: Hydromechanical modelling up to the end of Phase 1.
Step 2: Hydromechanical modelling up to the end of Phase 2 using parameters
backcalculated from step 1. Advanced features as permeability anisotropy, rock damage and
permeability increase in the damaged zone may be considered.
Step 3: Hydromechanical and geochemical modelling of the full test. Conservative transport
and one species considered.
Step 4: Hydromechanical and geochemical modelling of the full test. Reactive transport and
full geochemical model (optional).
![Page 7: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/7.jpg)
Granite200m – 450 m deepGeneric, purpose-built
Opalinus (hard) clay400m deepGeneric, not purpose-built
C-O argillite (hard clay)450m – 520 m deep Site-specific
Boom clay (plastic)230m deepGeneric, purpose-built
Rock salt490m – 800m deepGeneric, not purpose-built
Granite450m deepGeneric, not purpose-built
Background of Task A
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Mont Terri Project
• Located in Northern Switzerland
• Opalinus clay (shale)
• 400 m deep
• Operating since 1995
• Generic, not purpose - built
1: Mont Terri rock laboratory, 400 m beneath the hill2: Southern entrance of the motorway tunnelSource: Mont Terri website
Background of Task A
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Background of Task A
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• Overconsolidated clay
• Low porosity (±15%)
• Water content (±6%)
• Density (2.45 g/cm3)
• Low permeability (±10-13m/s)
• Variation of stiffness (2 to 10 GPa)
• UCS (10 to 20 MPa)
• Anisotropic material Temperature Mechanical (Strength and
stiffness) Hydraulic (?: selfhealing)
Stiff layered Mesozoic clay of marine origin
Background of Task A
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Background of Task A
Location of the ventilation test
Raise bored horizontal microtunnel
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Background of Task A
Ventilation test section
Section SA3
In flow
RH-out
Water pan 1SA1
SB1 SC1SA2 SD1 SE
SC2 SB2SD2 SA4
SA3
Rear doors
Out flow
RH-outRH-in RH-1 RH-2
Water Pan 2
RH-in
Instru m ented section:SA : M in i P ie zo m e tersSB : H um id ity se ns orsSC : T D RsSD : Exten so m e te rsSE : G e oe le ctric
Forward doors
Le gend :
R H-n : hyg ro m e te rRH-rRH-l
10 m
7 m
1,50 m
1,00 m
0,65 m
0,65 m
0,60 m
0,60 m
0,60 m
0,60 m
1,00 m
0,65 m
0,65 m
1,50 m
MI niche1.3m
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0
10
20
30
40
50
60
70
80
90
100
11/03/1997
24/07/1998
06/12/1999
19/04/2001
01/09/2002
14/01/2004
28/05/2005
10/10/2006
22/02/2008
06/07/2009
18/11/2010
Time
Re
lati
ve h
um
idit
y o
f in
co
min
g a
ir
[%]
9/4
/98:
Exc
. NG
1/2
/99:
Exc
. MT
8/7
/02:
Sea
ling
ve
ntil
ate
d s
ect
ion
24/9/06
8/7/02
28/5/03 29/1/04 11/7/05
Background of Task A
Section SA3
In flow
RH-out
Water pan 1SA1
SB1 SC1SA2 SD1 SE
SC2 SB2SD2 SA4
SA3
Rear doors
Out flow
RH-outRH-in RH-1 RH-2
Water Pan 2
RH-in
Instru m ented section:SA : M in i P ie zo m e tersSB : H um id ity se ns orsSC : T D RsSD : Exten so m e te rsSE : G e oe le ctric
Forward doors
Le gend :
R H-n : hyg ro m e te rRH-rRH-l
10 m
7 m
1,50 m
1,00 m
0,65 m
0,65 m
0,60 m
0,60 m
0,60 m
0,60 m
1,00 m
0,65 m
0,65 m
1,50 m
Saturation 1: 11 months
Desaturation 1: 8 months
Saturation 2: 11.5 months
Desaturation 2: 20.5 months
Continuous water mass
balance
Water content profiles
Relative humidity
Water pressure
Displacements
Geochemical
characterization
Ventilation test
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Objective of Task A
The main objective of the task is to examine the hydromechanical
and chemical changes that may occur in argillaceous host rocks,
especially in relation to the ventilation of drifts.
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Description of step 0
Objectives:
Brainstorming about theoretical formulations to be used in Task A
Determination of a set of parameters for Opalinus Clay
Reproduction of a laboratory drying experiment (Floria et al, 2002)
Material provided:
Physical prop. All (project data), water content prof.
Hydraulic prop. Floria (2002), Muñoz (2003), Solexperts (2003)
Mechanical prop. Bock (2001)
Hydro-Mech. coupling Various
Hydro-Mechanical info from chemical reports.
Traber ( 2003, 2004), Fernandez (2007), Noy (2003)
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Description of step 0
Drying test: lay out
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Description of step 0
Impermeable lateral boundaries
10cm
28cm
Tem
per
atu
re 30ºC
Rel
ativ
e h
um
idit
y [%
]
20%
50%
142 days
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Description of step 0
Impermeable lateral boundaries
10cm
28cm
Air
vel
oci
ty [
cm/s
]
30 [cm/s]
70 [cm/s]
9000gr.
Mas
s [g
ram
s]
Water pan: = 9.2cm
![Page 19: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/19.jpg)
Description of step 0
0
0.05
0.1
0.15
0.2
0.25
0 2 4 6 8water content [%]
dis
tan
ce t
o b
ase
[m]
Initial water content
Measurements at 21 days
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0 50 100 150Time [days]
Wat
er l
oss
[kg
]
Sample C
Water content profiles
Water lost during drying
Initial water content (porosity = 16%), = 7%. Amount to 352gr. water
59gr. water
60gr. water
![Page 20: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/20.jpg)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0 50 100 150Time [days]
Wat
er l
oss
[kg
]
Sample B Sample C
0
0.05
0.1
0.15
0.2
0.25
0 2 4 6 8water content [%]
dis
tan
ce t
o b
ase
[m]
Initial water content
Measurements at 21 days
Measurements at 99 days
Description of step 0
Water content profiles
Water lost during drying
Initial water content (porosity = 16%), = 7%. Amount to 352gr. water
121gr. water
130gr. water
![Page 21: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/21.jpg)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0 50 100 150Time [days]
Wat
er l
oss
[kg
]
Sample A Sample B Sample C
0
0.05
0.1
0.15
0.2
0.25
0 2 4 6 8water content [%]
dis
tan
ce t
o b
ase
[m]
Initial water content
Measurements at 21 days
Measurements at 99 days
Measurements at 142 days
Description of step 0
Water content profiles
Water lost during drying
Initial water content (porosity = 16%), = 7%. Amount to 352gr. water
![Page 22: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/22.jpg)
0.00
0.02
0.04
0.06
0.08
0.10
0.12
0.14
0.16
0.18
0.20
0 50 100 150Time [days]
Wat
er l
oss
[kg
]
Sample A Sample B Sample C
0
0.05
0.1
0.15
0.2
0.25
0 2 4 6 8water content [%]
dis
tan
ce t
o b
ase
[m]
Initial water content
Measurements at 21 days
Measurements at 99 days
Measurements at 142 days
Description of step 0
Water content profiles
Water lost during drying
Initial water content (porosity = 16%), = 7%. Amount to 352gr. water
151gr. water
156gr. water
![Page 23: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/23.jpg)
Participants
Modelling team CAS CEA JAEA Quintessa UoE
Person Liu Xiaoyan/Jing Lanru Alain Millard Shigeo Nakama Alex Bond Chris McDermott
On behalf of WHU IRSN JAEA NDA NDA
Country China France Japan UK UK
Comparison issues between different teams:
(T)H(M) formulation
Parameter set for Opalinus Clay
Model setup (top boundary condition)
Model results
![Page 24: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/24.jpg)
Participants
CAS CEA JAEA Quintessa UoE
Physical
Solid grain density ρs [kg/m3]
Porosity φ
Hydraulic
Intrinsic permeability k [m2]
Dynamic viscosity μ [Pa.s]
Liquid relative permeability λ’
Vapour diffusion coefficient
Mechanical
Young modulus E [GPa]
Poisson coefficient ν
Friction angle φ [º]
Cohesion c [MPa]
Hydro-Mech. coupling
Suction bulk modulus Ks [GPa]
Air entry value (retention curve) P0 [MPa]
Shape parameter (retention curve) λ
Maximum suction (retention curve)* Ps [MPa]
Second shape parameter (retention curve)* λs
Residual and maximum saturation (retention curve) Srl – Srs
2 /wgD m s
* Modified Van Genuchten
![Page 25: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/25.jpg)
Participants
CAS CEA JAEA Quintessa UoE
Physical
Solid grain density ρs [kg/m3]
Porosity φ
Hydraulic
Intrinsic permeability k [m2]
Dynamic viscosity μ [Pa.s]
Liquid relative permeability λ’
Vapour diffusion coefficient
Mechanical
Young modulus E [GPa]
Poisson coefficient ν
Friction angle φ [º]
Cohesion c [MPa]
Hydro-Mech. coupling
Suction bulk modulus Ks [GPa]
Air entry value (retention curve) P0 [MPa]
Shape parameter (retention curve) λ
Maximum suction (retention curve)* Ps [MPa]
Second shape parameter (retention curve)* λs
Residual and maximum saturation (retention curve) Srl – Srs
2 /wgD m s
* Modified Van Genuchten
![Page 26: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/26.jpg)
Participants
CAS CEA JAEA Quintessa UoE
Physical
Solid grain density ρs [kg/m3]
Porosity φ
Hydraulic
Intrinsic permeability k [m2]
Dynamic viscosity μ [Pa.s]
Liquid relative permeability λ’
Vapour diffusion coefficient
Mechanical
Young modulus E [GPa]
Poisson coefficient ν
Friction angle φ [º]
Cohesion c [MPa]
Hydro-Mech. coupling
Suction bulk modulus Ks [GPa]
Air entry value (retention curve) P0 [MPa]
Shape parameter (retention curve) λ
Maximum suction (retention curve)* Ps [MPa]
Second shape parameter (retention curve)* λs
Residual and maximum saturation (retention curve) Srl – Srs
2 /wgD m s
* Modified Van Genuchten
![Page 27: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/27.jpg)
Participants
CAS CEA JAEA Quintessa UoE
Physical
Solid grain density ρs [kg/m3]
Porosity φ
Hydraulic
Intrinsic permeability k [m2]
Dynamic viscosity μ [Pa.s]
Liquid relative permeability λ’
Vapour diffusion coefficient
Mechanical
Young modulus E [GPa]
Poisson coefficient ν
Friction angle φ [º]
Cohesion c [MPa]
Hydro-Mech. coupling
Suction bulk modulus Ks [GPa]
Air entry value (retention curve) P0 [MPa]
Shape parameter (retention curve) λ
Maximum suction (retention curve)* Ps [MPa]
Second shape parameter (retention curve)* λs
Residual and maximum saturation (retention curve) Srl – Srs
2 /wgD m s
* Modified Van Genuchten
![Page 28: Introduction to the Task A Task Force Meeting B. Garitte and A. Gens 2nd DECOVALEX 2011 workshop, 20 th of October 2008, Wakkanai, Japan Dept. of Geotechnical.](https://reader035.fdocuments.us/reader035/viewer/2022081519/56649d4c5503460f94a2a16e/html5/thumbnails/28.jpg)
Participants
CAS CEA JAEA Quintessa UoE
Physical
Solid grain density ρs [kg/m3]
Porosity φ
Hydraulic
Intrinsic permeability k [m2]
Dynamic viscosity μ [Pa.s]
Liquid relative permeability λ’
Vapour diffusion coefficient
Mechanical
Young modulus E [GPa]
Poisson coefficient ν
Friction angle φ [º]
Cohesion c [MPa]
Hydro-Mech. coupling
Suction bulk modulus Ks [GPa]
Air entry value (retention curve) P0 [MPa]
Shape parameter (retention curve) λ
Maximum suction (retention curve)* Ps [MPa]
Second shape parameter (retention curve)* λs
Residual and maximum saturation (retention curve) Srl – Srs
2 /wgD m s
* Modified Van Genuchten
0.1
1
10
100
1000
0 0.2 0.4 0.6 0.8 1Degree of saturation
Pg
-Pl [
MP
a]
Drying Path (Muñoz, 2003)
Wetting Path (Muñoz, 2003)
Gens (2000)
Drying path (Zhang, 2005)
Wetting path (Zhang, 2005)
Drying path (Villar, 2007)