8_chapter 8 types of rock slope failures- kinematic feasibility

21
CHAPTER EIGHT Types of rock slope failures: kinematic feasibility Modes of failure Overview A rock mass may display one or more modes of failure depending on the following factors: . presence or absence of discontinuity sets . orientation of discontinuity sets in relation to that of the natural or excavated face . discontinuity spacing in one and three dimensions . shear strength of discontinuity walls . persistence of discontinuities. Table 8.1 describes the individual modes of failure that can occur in fractured rock masses. Plane, wedge and toppling failure modes depend on the interaction of discontinuity orientation, face orientation and shear strength. This high degree of geometric control allows potential failure modes to be identi®ed using kinematics. Kinematics is a branch of mechanics that deals with motion without reference to force or mass. Hence in a rock slope, blocks that have the freedom to move based on geometry alone may be regarded as kinematically feasible blocks. A block may only be regarded as unstable however, if it is capable of being removed from the rock mass without disturbing the adjacent rock and the disturbing forces are greater than the restoring forces. A particular mode of failure in a given face may be recognized by identifying the kinematically feasible block for that mode based on the relative orientation of the discontinuities and the face and the stability of the block by considering the shear strength char- acteristics of the discontinuities. By constructing a series of overlays that are used with the contoured plot of pole concentrations, potentially unstable blocks relating to different modes of failure can be readily identi®ed. In constructing the overlays a very simplistic approach is taken to de®ne the shear strength of the dis- continuities. The presence of water in the discontinuities and external loading (both static and dynamic) are ignored. 241

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Page 1: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Lateral release surfaces

Unstable block

Direction ofmovementcontrolled by lateral release surfaces

Basal slip plane

Trace of the discontinuityrepresenting the basal slip plane in the face

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Dip directionof slope face

Angle offriction

Dip of slope face

Poles falling in this zone represent potentialplane slip surfaces

Limits on dipdirectionfor slip plane

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Page 9: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Dip directionof slope face

Angle offriction

Dip of slope face

Intersections falling in thiszone represent potentialplane slip surfaces

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45G

Page 10: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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"/,"/(/.3+.2 34/ -'3/"'- "/-/'(/ (1"0'$/( '.* 34/ (-+, (1"0'$/ 5+-- ',,/'"

5+34+. 34/ $"/($/.3 #0 34/ 5/*2/ 0'+-1"/ #9/"-'): G3 +( ./$/(('") 34/"/0#"/

3# $-'((+0) ,#3/.3+'--) 1.(3'7-/ 5/*2/( +.3# (+.2-/ ,-'./ (-+*+.2 7-#$%(

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! '.* F 5+34 *+, *+"/$3+#.( (4#5. +. J+2: <:]: G0 *+, *+"/$3+#. #0 ,-'./ !

N

Plane B

Plane A

Intersection ofA and B

Cut slope

N

Plane B

Plane A

Intersection ofA and B

Cut slope

(a)

(b)

6.7' &'J K 5%39*+ -*0 +%3%05.1.17 D9%39%0 " <*3%13."$$> /1,3"#$% D%+7%

D.$$ ,$.+% *1 *1% *0 3D* <$"1%, ?-0*5 L*24.17@ (AHJC' ?"C M$.+.17 *1 <$"1%

K' ?#C M$.+.17 *1 .13%0,%23.*1 *- K "1+ N

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Page 11: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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34/ 5/*2/ 0'+-1"/ #9/"-'):

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'.2-/ #0 SU" 5+-- 7/ '((1&/*:

N

AB

A

AB

C

D

B

C

C

B

D

CA

DA

BA

DBDC

CB

D

6.7' &'H ;*1,30/23.*1 *- .13%0,%23.*1 <$*3 #",%+ *1 +"3" 7.=%1 .1 6.7' H':(

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4D6

Page 12: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Dip direction

of slope

30˚Frictioncone

Slope angle, !

50˚60˚

70˚ 80˚

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Page 13: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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$'.3+-/9/" 7/'&(: ;4+( +( $#&&#. +. 34+.-) 7/**/* #" 0#-+'3/* "#$%( (1$4

'( (4'-/? (-'3/ #" ($4+(3 #" $-#(/-) C#+.3/* "#$% 54/"/ 34/ 0"'$31"/( *+,

(3//,-) +.3# 34/ 0'$/ '( (4#5. +. ;'7-/ <:=: ['$4 -')/" 3/.*( 3# 7/.*

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N

A B

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B B

D

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CBDB

6.7' &'A G,% *- *=%0$"> D.39 .13%0,%23.*1 <$*3

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4DC

Page 14: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Page 15: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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#1

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$

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Pole

Horizontal

Discontinuity

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Page 16: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Dip of slope face

Poles falling in these zones provide the potential for flexural toppling providedthe joint spacing is sufficiently close

0

15

–15

–30

30

Angle offriction

Dip directionof slope face

Limits on dipdirection

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789:! ;9<:7= >? /,01 234 5,67 /1,89 93:0399503:

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Page 17: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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Dip of slope face

Angle offriction

Dip directionof slope face A

B

B

60˚ approx.for intersections

Limits on dipdirection

Intersections that fallinto zones A and Brepresent potentiallyunstable blocks whencombined with polesin zone A (basal planes)

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Page 18: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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4DB

Page 19: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

*/,/.* ,"+.$+,'--) #. 34/ (,'$+.2 #0 (/3 L: G0 (/3 L +( 5+*/-) (,'$/*

34/. 34/ 4'D'"* 5+-- 7/ "/*1$/*:

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Use with poles

Zone 4use with intersections

Zone 3use with poles andintersections

Zone 2

Zone 2

High flexural toppling hazard if joints are closely spaced

Low to intermediate flexural toppling hazard if joints are closely spaced

+High block toppling but requires a 3rd joint set to form blocks.Look for intersection in

6.7' &'(F ;*1,30/23.*1 *- 2*5#.1%+ R%E/0"$ "1+ #$*24 3*<<$.17 *=%0$"> -*0 D*04%+

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4DG

Page 20: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

34/ 4+24/(3 $#.$/.3"'3+#. #0 ,#-/( '((#$+'3/* 5+34 *+($#.3+.1+3) (/3 !

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N

B

D

B

C

A

CA

DA

CB

DBDC

BA

180˚

High risk of flexural toppling is high if set D is closely or very closely spaced

D dips @ 60˚A dips @10˚

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4EH

Page 21: 8_Chapter 8 Types of Rock Slope Failures- Kinematic Feasibility

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N

B

D

B

C

A

CA

DA

CB

DBDC

BA

280˚

High risk of flexural toppling from set B if spacing is close enough.High risk of block toppling on basal planes formed by set A. Sets B and D will form unstable blocks if spacing of sets B and D is much less than set A

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4E6