Internal stability of granular materials in triaxial tests · Internal stability of granular...
Transcript of Internal stability of granular materials in triaxial tests · Internal stability of granular...
Internal stability of granular
materials in triaxial tests
Livah ANDRIANATREHINA (1), Hanène SOULI (1),
Jean-Jacques FRY (2), QuocTuan PHAN (3), Jean-Marie FLEUREAU (3)
(1)-Laboratoire de Tribologie et Dynamique des Systèmes CNRS/UMR 5513, ENISE 58 Rue Jean Parot, 42023 Saint Etienne cedex 02
(2)- Électricité de France, Centre Ingénierie Hydraulique ,
73073 Le Bourget du Lac cedex
(3) Laboratoire de Mécanique (Sols, Structures & matériaux) CNRS/UMR 8579 ,ECP
Grande voie des vignes 92290 Châtenay-Malabry cedex
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability;
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability;
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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I. INTRODUCTION
OVERVIEW OF THE MIGRATION OF FINES:
Migration of
fines
Heterogeneity
of the material
in dam
Differential
settlement Loss of
performance
Phenomenon of
piping
Instability of
the dam
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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II. PRESENTATION OF THE MATERIALS
0
20
40
60
80
100
100 1000 10000 100000
C5
C10
C20
C30
C7
Pa
ssin
g (
%)
Grain diameter (µm)
Continuous grain size distribution
0
20
40
60
80
100
100 1000 10000 100000
D5
D10
D20
D30
Pa
ssin
g (
%)
Grain diameter (µm)
Discontinuous grain size distribution
Name < 0.315
[mm] CU
C5
continuous
5 13,7
C7 7 9,4
C10 10 20,7
C20 20 19,1
C30 30 8,5
D5
discontinuous
5 2,6
D10 10 2,9 - 29
D20 20 35,7
D30 30 35,5
All materials have
Cu =d60/d10>2, then : widely graded
Fine = Φ < 0.315 mm
Cx or Dx = material having respectively
continuous or discontinuous grain size
distribution, containing x% of fines
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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III. EXPERIMENTAL PROCEDURE OF THE TESTS
Equipment:
Triaxial cell;
the loading frame Pressure controller
Saturating;
B check = Δu/Δσ3;
Consolidating;
Shearing.
The triaxial test is consists in:
2 Relative densities:Dr = 50, 90%;
3 effective confining stresses:
σ’3 = 50, 100, 200kPa;
Initial water content: 0 to 4 %.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability;
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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IV. INTERNAL STABILITY OF THE MATERIAL
1)Terzaghi (1953);
2)Kezdi (1979);
3)Kenney and Lau (1985; 1986);
4)Burenkova (1993).
CRITERIA TO EVALUATE INTERNAL STABILITY
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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IV. INTERNAL STABILITY OF THE MATERIAL
Kenney and Lau (1985; 1986)+ Kezdi (1979):
C5 C7 C10 C20 C30 D5 D10 D20 D30
Kenney & Lau (1985,
1986) S S S S S U U U U
Continuous grain size distribution Discontinuous grain size distribution
0
20
40
60
80
100
0 20 40 60 80 100
C5
C10
C20
C30
C7
H=F
H:
mass f
racti
on
betw
een
D a
nd
4D
F: mass fraction smaller than
Unstable
K&L
Stable
K&L
0
20
40
60
80
100
0 20 40 60 80 100
H:
mass f
racti
on
betw
een
D a
nd
4D
D5
D10
D20
D30
H=F
F: mas fraction smaller than
Stable
K&L
Unstable
K&L
Narrowly Graded Narrowly Graded Widely Graded Widely Graded
Kenney & Lau
(1985,1986) + Kezdi
(1979)
U U U S S U U U U
Stable Kezdi
Unstable Kezdi
Stable Kezdi
Unstable Kezdi
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability;
V. Results;
VI. Conclusions.
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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V. RESULTS
DIRECT MEASUREMENT OF THE STABILITY OF THE STUDIED SOILS
AFTER TRIAXIAL TESTS
0
20
40
60
80
100
0.1 1 10 100
initial
triax_upper
triax_medium
triax_lower
Pa
ssin
g (
%)
Grain diameter (mm)
D20
Size analysis tests
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
ΔPmoy
- ΔP≤10%: Stable;
- ΔP>10%: Unstable.
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CONTENTS
I. Introduction;
II. Presentation of materials;
III. Experimental procedure of the tests;
IV. Internal stability;
V. Results;
VI. Conclusions.
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VI. CONCLUSION
C5 C7 C10 C20 C30 D5 D10 D20 D30
Direct measurement U U S S S U U U S
Summary table
analysis of internal stability of soils must take into account several parameters.
None of the criteria gives a correct answer for all the soils (this can be caused
by differences in test conditions); In the present test, the combination of Kenney & Lau (1985, 1986) and Kezdi (1979)
gives the best assessment of the internal stability of soils;
Kenney & Lau (1985,
1986) S S S S S U U U U
Kenney & Lau
(1985,1986) + Kezdi (1979) U U U S S U U U U
Terzaghi, USACE (1953) S LS٭ S S S U U U U
Burenkova (1993) LS٭ U LS٭ S U LS٭ LS٭ U U
Limite Stable٭
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012
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Thank you for your attention!
6th International Conference on Scour and Erosion, Paris Aug. 27-31, 2012