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Quantitative Classification of Rock Mass - IITKhome.iitk.ac.in/~sarv/New Folder/Presentation...

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Quantitative Classification of Rock M Mass Description of Joints: Description of Joints: Orientation, Persistence, Roughness, Wall Strength Aperture Filling Seepage Strength, Aperture, Filling, Seepage, Number of sets, Block size, spacing. ISRM i i t ISRM commissions report Classification of Rock Material Based on Uniaxial Compressive Strength
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Quantitative Classification of Rock MMass

• Description of Joints:Description of Joints:Orientation, Persistence, Roughness, Wall Strength Aperture Filling SeepageStrength, Aperture, Filling, Seepage, Number of sets, Block size, spacing.ISRM i i ’ tISRM commission’s reportClassification of Rock MaterialBased on Uniaxial Compressive Strength

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Point Load Index• Quick evaluation for uniaxial strength

(field or lab setup)(field or lab setup)• ASTM D 5731 procedures• Little sample preparation (cores,

pieces)• Measure force (P) to crunch intact rock

specimen• Point Load Index: Is = P/de

2 where de= equivalent core diameter equivalent core diameter

Fig.8-1

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Point Load Index

GCTS Device Roctest Equipment

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Uniaxial Compressive Ranges for someUniaxial Compressive Strength

Ranges for some Common Rock Material

Term Kg/cm2 Schist, Silt stone VW-W, Sand Very Weak- VW < 70Stone, Lime stone –VW-M,Granite, Basalt Gneiss

yWeak- WMedium Strong-MS

70-200200-700 Basalt, Gneiss,

Quartzite, Marble –MS-VS

Medium Strong MSStrong- SVery Strong- VS

200 700700-1400> 1400 MS VS

|

Very Strong VS > 1400

|

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Classification for Rock Material StrengthStrength

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Rock Quality Designation (RQD)M difi d C Ror Modified Core Recovery

xRQD iΣ=

LQ

xi = lengths of individual pieces of core ≥ 10 cm i g p

L is the total length of the drill run

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Indirect Methods of determination f RQFof RQF

Seismic Method -Seismic Method RQD= (Vf / Vl )2 * 100

R ti f l it i th fi ld t th t i th l bRatio of velocity in the field to that in the labVolumetric Count -RQD = 115- 3.3* Jv

where J is a measure of number of jointswhere Jv is a measure of number of joints within a unit volume of rock mass

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RQDRQD

RQDA. Very poor 0 – 25B. Poor 25 – 50C.Fair 50 – 75D.Good 75 – 90E Excellent 90 100E. Excellent 90 - 100

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ROCK STRUCTURE RATING (RSR)(RSR)

• Wickham et. al. (1972) suggested this based on ( ) ggobservation of small tunnels supported by steel ribs.

• RSR = A + B + CParameter A Geology: General appraisal of geologicalParameter A, Geology: General appraisal of geological structure on the basis of:

• a. Rock type origin (igneous, metamorphic, di t )sedimentary).

• b. Rock hardness (hard, medium, soft, decomposed).• c. Geologic structure (massive, slightly faulted/folded,c. Geologic structure (massive, slightly faulted/folded,

moderately faulted/folded,• intensely faulted/folded).

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• Parameter B, Geometry: Effect of discontinuity pattern ith t t th di ti f th t l d i thwith respect to the direction of the tunnel drive on the

basis of:a. Joint spacing.b. Joint orientation (strike and dip).c. Direction of tunnel drive

• Parameter C: Effect of groundwater inflow and jointParameter C: Effect of groundwater inflow and joint condition on the basis of:a. Overall rock mass quality on the basis of A and B combined.b. Joint condition (good, fair, poor).c. Amount of water inflow (in gallons per minute per 1000 feet of tunnel)..feet of tunnel)..

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RMR or ‘Geomechanics Cl ifi i ’Classification’

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Guideline properties of Rock Mass ClClasses

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Evaluation of Tunnels b d RMR

Example: 10 m spanRMR = 80Stand up time > 4 yearsbased on RMR Stand up time > 4 yearsRMR = 50Stand up time ≈ 2 days

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RMR modified for slopes or tunnelsRMR modified for slopes or tunnels

Additional factors applied to RMRbasic

• Accounts for excavation method• Accounts for excavation method

BUT moreover,

• Accounts for joint orientation wrt the excavation

– Unfavourable conditions, deduct points from , pRMRbasic

– refer section F of Tablerefer section F of Table

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Slopes - unfavourableSlopes unfavourable

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Slopes - favourable

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Tunnels - unfavourable

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Tunnels - favourable• Widely spaced joints?Widely spaced joints?

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RMR & TunnelsRMR & Tunnels

• “Stand up time” for various tunnel spans based on RMR

• Unreinforced tunnels

─ no advice re support e.g. shotcrete or rockbolts/anchors

Shotcrete = sprayed concrete, lightly reinforcedp y , g y

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NGI Q-System Rating for Rock Masses (Barton, Lien, & Lunde, 1974) Norwegian Classif ication for Rock Masses

⎟⎠⎞

⎜⎝⎛⎟⎟⎠

⎞⎜⎜⎝

⎛⎟⎟⎠

⎞⎜⎜⎝

⎛=

SRFJ

JJ

JRQDQ w

a

r

n

Q - Value Quality of Rock Mass < 0.01 Exceptionally Poor 4. Discontinuity Condition & Infilling = Ja

0.01 to 0.1 Extremely Poor 4.1 Unfilled Cases 0.1 to 1 Very Poor Healed 0.75 1 to 4 Poor Stained, no alteration 1 4 to 10 Fair Silty or Sandy Coating 3

10 t 40 G d Cl ti 4 10 to 40 Good Clay coating 4 40 to 100 Very Good 4.2 Filled Discontinuities 100 to 400 Extremely Good Sand or crushed rock inf ill 4 < 400 Exceptionally Good Stif f clay inf illing < 5 mm 6

Sof t clay inf ill < 5 mm thick 8 PARAMETERS FOR THE Q-Rating of Rock Masses Swelling clay < 5 mm 12

Stif f clay inf ill > 5 mm thick 10 Stif f clay inf ill > 5 mm thick 10 1. RQD = Rock Quality Designation = sum of cored pieces Sof t clay inf ill > 5 mm thick 15 > 100 mm long, divided by total core run length Swelling clay > 5 mm 20

2. Number of Sets of Discontinuities (joint sets) = Jn 5. Water Conditions Massive 0.5 Dry 1

One set 2 Medium Water Inf low 0 66 One set 2 Medium Water Inf low 0.66 Two sets 4 Large inf low in unf illed joints 0.5 Three sets 9 Large inf low with f illed joints Four or more sets 15 that wash out 0.33 Crushed rock 20 High transient f low 0.2 to 0.1

High continuous f low 0.1 to 0.05 3. Roughness of Discontinuities* = Jrg r

Noncontinuous joints 4 6. Stress Reduction Factor** = SRF Rough, wavy 3 Loose rock with clay inf ill 10 Smooth, wavy 2 Loose rock with open joints 5 Rough, planar 1.5 Shallow rock with clay inf ill 2.5 Smooth, planar 1 Rock with unf illed joints 1 Slick and planar 0.5 Filled discontinuities 1 **Note: Additional SRF values given*Note: add +1 if mean joint spacing > 3 m for rocks prone to bursting, squeezing

and swelling by Barton et al. (1974)

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Rock Tunnelling Quality Index, Q( N i Q t ) B t t l 1974(or Norwegian Q system), Barton et al., 1974

⎟⎠⎞

⎜⎝⎛×⎟

⎠⎞

⎜⎝⎛×⎟

⎠⎞

⎜⎝⎛=

SRFJw

JJr

JRQDQ ⎟

⎠⎜⎝

⎟⎠

⎜⎝

⎟⎠

⎜⎝ SRFJaJn

Q

RQD = Rock Quality Designation 100 - 10Jn = Joint set number 1 – 20Jr = Joint roughness factor 4 -1Ja = Joint alteration and clay fillings 1 – 20Jw = Joint water inflow or pressure 1 – 0 1Jw Joint water inflow or pressure 1 0.1SRF = stress reduction factor 1 – 20

Typically: 0.01 < Q <100

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Q systemQ system

⎟⎠⎞

⎜⎝⎛×⎟

⎠⎞

⎜⎝⎛×⎟

⎠⎞

⎜⎝⎛=

SRFJw

JJr

JRQDQ

⎠⎝⎠⎝⎠⎝ SRFJaJn

• (RQD/Jn) = crude measure of block size• (Jr/Ja) = roughness/friction of surfaces

( /S ) f ( )• (Jw/SRF) = ratio of two stress parameters (active stress)

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Geological Strength Index, GSIGSI

• Developed by Hoek, Kaiser, & Bawden (1995) H k & B (1997)(1995), Hoek & Brown (1997).

• GSI from Q-system: 44log9 +⎥⎤

⎢⎡

⎟⎟⎞

⎜⎜⎛⎟⎟⎞

⎜⎜⎛

= rJRQDGSI

• GSI from Geomechanics system where

og9 ⎥⎦

⎢⎣

⎟⎟⎠

⎜⎜⎝⎟⎟⎠

⎜⎜⎝ an JJ

GS

GSI from Geomechanics system where RMR > 25: ( )∑+=

4

10 iRGSI

• Chart approach based on structure & f lit

∑=1i

surface quality

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Slope Mass Rating (SMR)Slope Mass Rating (SMR)

• SMR = RMRb i – ( F1 F2 F3 ) + F4SMR = RMRbasic ( F1.F2.F3 ) + F4

• F1, F2 and F3 are adjustment factors related to joint orientation with respect torelated to joint orientation with respect to slope orientation. F4 is the correction factor for method of excavationfactor for method of excavation.

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Suggested Supports for Various SMR lSMR classes

SMR Classes SMR Values Suggested SupportsSMR Classes SMR Values Suggested Supports

I a 91-100 NoneI b 81-90 None, scaling is required

II a 71-80 Spot BoltingII b 61-70 Spot or systematic bolting

III a 51-60 Spot or systematic bolting, spot shotcrete

III b 41-50 Systematic bolting and shotcrete, toe wall

IV a 31-40 Anchors, systematic shotcrete, toe wallIV b 21 30 S t ti i f d h t t t llIV b 21-30 Systematic reinforced shotcrete, toe wall,

re-exacavationV 11-20 Gravity or anchored wall, re-excavation

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Rock Strength: mi parameter

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Strength of Rock Massesmmi↓

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Strength of Rock Massesc'/qu

mi

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Equivalent Modulus of Rock Masses (Table 10 7)(Table 10-7)

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Allowable Bearing Stresses on Rock Masses

Foundations on Fractured Rock Formation30

MPa

) Note: Use maximum qa < q u

where qu = compressive strength

20

25

ress

qa (M

where qu compressive strengthof intact rock specimens

15

earing

Str

)130/(1)16/(1)(

RQDRQDMPaq ALLOWABLE −

+≈

NOTE: 1 MPa = 10 tsf

5

10

owab

le B

e

Peck, et al. (1974)

NOTE: 1 MPa = 10 tsf

00 10 20 30 40 50 60 70 80 90 100

Allo

( )Approximation

Rock Quality Designation, RQD

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