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1 EXPLICIT CHARACTERISATION AND INTERACTIVE ANALYSIS FOR ENGINEERING DESIGN OF ROCK CAVERNS S C Bandis, J C Sharp, R A MacKean, E A Bacasis GEO-DESIGN United Kingdom and Greece HKIE-HKIP Conference on Planning and Development of Underground Space HONG KONG, 23-24 SEPTEMBER 2011 The principal elements for the design of caverns are : Geological interpretation Engineering characterisation of the rock mass Rock mass model development Design analyses Engineering assessment

EXPLICIT CHARACTERISATION AND INTERACTIVE ANALYSIS FOR ENGINEERING DESIGN OF ROCK CAVERNS

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EXPLICIT CHARACTERISATION AND INTERACTIVE ANALYSIS FOR ENGINEERING DESIGN OF ROCK CAVERNS

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  • 1EXPLICIT CHARACTERISATION AND

    INTERACTIVE ANALYSIS

    FOR ENGINEERING DESIGN OF ROCK CAVERNS

    S C Bandis, J C Sharp, R A MacKean, E A Bacasis

    GEO-DESIGN

    United Kingdom and Greece

    HKIE-HKIP Conference on Planning and Development of Underground Space

    HONG KONG, 23-24 SEPTEMBER 2011

    The principal elements for the designof caverns are :

    Geological interpretation

    Engineering characterisation of the rock mass

    Rock mass model development

    Design analyses

    Engineering assessment

  • 2The discontinuous nature of rock masses predicates the use of comprehensive, explicit methods for engineering characterisation and analysis

    aiming to provide a realistic model of the intrinsic load bearingresponse and hence the degree of stabilisation required for safeand economic cavern development.

    The Distinct Element Method (DEM) provides the most appropriate approach for analysis of discontinuous rock mass behaviour.

    The DEM in rock engineering is implemented by the state-of-art software UDEC and 3DEC, developed by Dr Peter Cundall

    R

    v-

    v+

    n

    t

    Simulation of Rock Mass as a Discontinuum

  • 3The rock mass is simulated as an assembly of relatively rigid (rock) blocks in contact across interfaces representing the geological discontinuities.

    Residual soil

    Weathered

    granitic rock

    Fresh granitic

    rock

  • 4The discontinuum approachis appropriate when the geological structure controls anisotropy and deformation modes of the rock mass.

    IT IS APPLICABLE TO MORE THAN 80% OF ROCK MASSES.

    The equivalent-continuum approach is appropriate where the density and orientation of jointing are such, that no preferential paths of stress strain responses are present.

    IT IS APPLICABLE TO LESS THAN 20% OF ROCK MASSES.

    Simulation as equivalent continuum Discontinuum analysis

    18m cavern inbedded rock

    Pseudo-Continuum vs. Discontinuum

  • 5Comparison between the Ground Reaction Curves derived from theUDEC-BB, FLAC (M-C material behaviour) and FLAC-Ubiquitous Joint analyses.

    Pseudo-Continuum vs. Discontinuum

    EXPLICIT ROCK MASS MODEL DEVELOPMENT REQUIREMENTS

    ROCK MASS

    ROCK MATERIALS

    ROCK DISCONTINUITIES

    Lithological Variability

    Structure Geometry

    Weathering

    (Sets, Orientation)

    Types of Discontinuites

    Index Properties

    Stress-Strain Behaviour

    Shear Strength Stiffness Behaviour

    Engineering

    Characterisation

  • 6EXPLICIT ROCK MASS MODEL DEVELOPMENT

    12

    Weathering

    Zone

    Typical

    Subhorizontal

    Joint Type2

    Associated Characteristics

    Typical Constituent

    Material Grade

    Distribution1

    Typical Core

    Loss (per core

    run)

    Typical

    RQD

    range

    D SH4 &5I,II & III >85%

    IV & V

  • 7ROCK MASS ASSESSMENT

    SITE SPECIFIC ROCK MASS CLASSIFICATION

    RM03 RM06

    RM 07RM02 RM05

    RM01 RM04

    14

  • 8ROCK MASS CLASS O4

    Weathering zone BTypical RQD 90-100%

    Typical core loss

  • 9Q 1Q 10

  • 10

    Most common strength criteria for rock discontinuities

    Barton - Bandis

    BARTON BANDIS CONSTITUTIVE MODEL OF COUPLED BEHAVIOUR OF ROCK DISCONTINUITIES

    The model enables stress-and scale-dependent coupling of shear stress with shear displacement and dilation, and of normal stress with closure.

    The model input data comprise the following joint characterization indices:

    JRC=Joint Roughness Coefficient

    JCS=Joint Wall Compressive Strength

    Lo, Ln=Block size or length of joint

    Eo =Mechanical (true) joint aperture or opening

    r=Angle of residual friction

  • 11

    The rock mass is simulated as an assembly of relatively rigid (rock) blocks in contact across interfaces representing the geological discontinuities.

    vj

    Kn

    Ks

    u

    UDEC

    B-B MODEL

    +

    =

    UDEC - BB

  • 12

    Explicit (Discontinuum) Analyses in Cavern Engineering Practice

    Design prediction Construction reality

    Ideally, the requirements from design analyses are to establish if a rock mass will fail under applied loadings or calculate the displacements required for a system in order to attain a new equilibrium either at the intrinsic or the engineered states.

    Example of excavation sequence Intrinsic performance

  • 13

    SV2 (major) joint

    Extended rotational shearing of the bedded rock due to formation of a large destressed haunch wedge.

    Block detachment under rotational shear at the haunch due to shear overstressing of the bedded rock.

    Contiguous zones of tensile yielding are evident forming the outer boundaries of the collapsing crown block. The distributions of tensile yield points at the fixities and the centers of the rock layers indicate typical failure mechanism of a laminate composed of simply supported beams

    Zone of tensile yield at the rock beam fixities

    Example of collapse mechanism of an unsupported 18m span cavern

    Material yield intension

    INTRINSIC (UNSUPPORTED) CAVERN RESPONSE

    EFFECT OF ROCK MASS QUALITY

    (Fully Drained State)

    GOOD QUALITY RM 01 POOR QUALITY RM 05

    25 mm

    55 mm

    OVERALL STABLE CONDITIONS (EXCLUDING DETACHED WEDGES)

  • 14

    Example of groundwater modelling

    The inferred patterns represent partial drainage with zero pressure at 1m from theexcavation periphery, gradually reverting to full hydrostatic pressure throughinferred intermediate regimes according to the permeability profile.

    Zero groundwater pressure Under groundwater pressure

    Extensive shearing along both the SH and SV discontinuities diminishes the flexural stiffness of the rock slabs COLLAPSE STATE

    EFFECTS OF GROUNDWATER PRESSURE

    POOR QUALITY RM 05

    OVERALL STABLE STATE(EXCLUDING DETACHED WEDGES)

    INTRINSIC (UNSUPPORTED) CAVERN RESPONSE

  • 15

    INTRINSIC (UNSUPPORTED) CAVERN RESPONSE

    INFLUENCE OF HORIZONTAL STRESSES GOOD ROCK MASS QUALITY

    Ko=4.0Ko=0.7

    Enhanced normal stresses across the SV structure mobilize their dilatant shear strength, radial destressing is minimised, normal stresses/shear stiffness across theSH structure maintained de-lamination / slab deflections minimal

    12 mm45 mm

    Simulation of Excavation Support Sequence

    Derivation of induced loadings on rock reinforcementand shotcrete lining support systems

  • 16

    Intrinsic vs. Supported excavation

    Detailed engineering evaluation of the numerical analyses is an extremely important stage of developing comprehensive detailed designs.

    Such an evaluation should also involve a realistic appreciation of the limitations inherent in all computational schemes.

    Engineering Evaluation of Numerical Analyses Resultsin Cavern Engineering Practice

  • 17

    Temporary Support

    Rock Reinforcement

    Modelling details of the reinforcement units (notably the typeof bonding and allowable axial strain) are significant.

    Typically Safety Factors of 1.5 against tensile failure of bar for temporary units and 2.0 for permanent units are usually considered.

    Interaction Diagram

    for Reinforced Concrete DesignAccording to BS 8110, Part 1:1997 & Part 3:1985

    Input Data: TABLE BAL - Concept I - 20m - K=0.7

    SHOTCRETE 350mm - PILLAR (30mm Relaxation)

    h = 350 mm Intrados: cover 50 mmb = 1000 mm diameter 10 mm

    fcu = 25 N/mm2

    spacing 150 mm

    fy = 460 N/mm2

    As1 = 524 524 mm2

    Es = 210000 kN/mm2

    Extrados: cover 20 mmdiameter 10 mm

    Partial material factors: spacing 150 mmmc = 1,5 concrete As2 = 524 524 mm

    2

    ms = 1,05 reinforcement

    M N d1 = 55 mm169,770 2279 0,260 0,055 d2 = 25 mm144,520 2212 0,253 0,047 d = 295 mm119,290 2205 0,252 0,03975,000 2150 0,246 0,02440,420 2101 0,240 0,01314,390 2086 0,238 0,0050,310 2075 0,237 0,000

    18,520 2056 0,235 0,0062,940 2039 0,233 0,0017,690 2002 0,229 0,003

    47,280 2008 0,230 0,01560,000 1989 0,227 0,020

    0,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,000

    Interactive Diagram

    -0,1

    0

    0,1

    0,2

    0,3

    0,4

    0,5

    0,6

    -0,02 -0,01 0,00 0,01 0,02 0,03 0,04 0,05 0,06 0,07 0,08 0,09

    = [M/fcu.b.h2]

    =

    [N

    /fcu.b

    .h]

    Concrete Capacity

    Including tension reinforcement

    Capacity: tension +compression reinforcementSection Forces

    Interaction Diagram

    for Reinforced Concrete DesignAccording to BS 8110, Part 1:1997 & Part 3:1985

    Input Data: TABLE BAL - DESIGN MODEL 20m - K=0.7

    SHOTCRETE 350mm + LAG D2 (Ixx=773,45cm4, H=160mm, 2No32mm + 1No25mm) @ 1000mm

    HALF TOP HEADING (at Relaxation 30mm)

    h = 350 mm Intrados: cover 95 95 mmb = 1000 mm diameter 25 0 mm

    fcu = 25 N/mm2

    spacing 500 100 mm

    fy = 460 N/mm2

    As1 = 982 0 982 mm2

    Es = 210000 kN/mm2

    Extrados: cover 95 95 mmdiameter 32 0 mm

    Partial material factors: spacing 1000 100 mmmc = 1,5 concrete As2 = 1608 0 1608 mm

    2

    ms = 1,05 reinforcement

    M N d1 = 95 mm0,000 0,000 d2 = 95 mm0,000 0,000 d = 255 mm0,000 0,0000,000 0,000

    66,000 2554 0,292 0,02271,810 2667 0,305 0,02353,880 2343 0,268 0,01830,400 2128 0,243 0,01013,040 2173 0,248 0,00413,530 2088 0,239 0,0045,670 1925 0,220 0,002

    12,230 1818 0,208 0,00425,970 1680 0,192 0,0085,680 1588 0,181 0,002

    20,300 1507 0,172 0,00746,740 1426 0,163 0,01575,650 1364 0,156 0,02596,970 1233 0,141 0,032

    116,630 1176 0,134 0,038136,700 1126 0,129 0,045136,010 952 0,109 0,04498,860 1132 0,129 0,03299,340 1085 0,124 0,032

    0,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,0000,000 0,000

    Interactive Diagram

    -0,2

    -0,1

    0

    0,1

    0,2

    0,3

    0,4

    0,5

    0,6

    -0,02 -0,01 0,00 0,01 0,02 0,03 0,04 0,05 0,06 0,07 0,08 0,09

    = [M/fcu.b.h2]

    =

    [N

    /fcu.b

    .h]

    Concrete Capacity

    Including tension reinforcement

    Capacity: tension +compression reinforcementSection Forces

    N-M interaction diagrams for shotcrete line based on UDEC derived data

    Temporary Support

    Shotcrete Capacity

  • 18

    Degree of Rock Mass Stabilization

    Cavern profile deformation Discontinuity shear overstress

    mob

    peak

    SSR = mobilised shear strength / peak shear strength

    dV

    S

    dV = S /250

    for temporary support

    dV = S /500

    for permanent support

  • 19

    Ground loading on shotcrete / concrete linings

    Rock load estimates are usually based on empirical approaches (andrelated classification schemes) and analytically derived (equivalentcontinuum) ground reaction curves and.

    Numerical modelling enables derivations of ground loadings in aninteractive fashion, incorporating the effects of actual deformationsassociated with the prevailing stability mechanisms.

    FIGURE 2- K=0,7 : WIL - FINAL LINING 600mm (GWP 2) - DISTRIB. LOADS

    UNIVERSITY CAVERN

    -100,0

    0,0

    100,0

    200,0

    300,0

    400,0

    30 40 50 60 70 80 90 100 110 120 130 140 150 160 170 180 190 200 210 220

    Nodes

    kP

    a

    NORMALSHEARWATER PRESSURE

    ROCK LOADING Of CONCRETE LININGS

  • 20

    CONCLUSIONS

    Using comprehensive explicit geological and rock mass characterisation and design analysis methods the following is achievable:

    Safely engineered, low risk, design for a range of rock mass conditions and cavern geometries

    Optimised engineering design in terms of excavation sequencing, type and quantum of support.

    Inappropriate design methods for discontinuous rock massesIncluding those in Hong Kong (re equivalent continuum methods), whilst attractive in terms of simplicity may lead to over- or under- dimensioned (and unsafe) designs.

    Due to inevitable uncertainties in geological prediction, a planned

    design implementation process, that includes designer

    involvement and appropriate expertise, should be treated as an

    essential component of a design methodology.

    The key elements of the process should include:

    Specialist evaluation of geological conditions as excavated.

    In-line performance monitoring of key indicators (deformation, stress change, groundwater etc) in order to validate design

    predictions.

    Design model assessment and review (confirmation) for each construction stage.

  • 21

    Particular rock engineering challenges facing Hong Kongcavern developments involve the excavation of cavernsbeneath existing high rise structures and the increasinglycomplex architecture of three dimensional space to producemore acceptable underground layouts and environments.

    Thank you