Presentation IQPC Africa

91
Seismic Design Aspects of Underground Structures Asrat Worku (Dr-Ing) Gibb International, Nairobi Kenya (Formerly, Associate Professor at Addis Ababa University, Addis Ababa, Ethiopia)

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Transcript of Presentation IQPC Africa

  • Seismic Design Aspects of Underground Structures

    Asrat Worku (Dr-Ing) Gibb International, Nairobi Kenya (Formerly, Associate Professor at Addis Ababa University, Addis Ababa, Ethiopia)

  • Outline 1. Types of UG Structures Addressed 2. Earthquake Effects on UG Structures 3. Performance of UG Structures to Earthquakes 4. Seismic Design Procedures 5. Seismic Hazard Analysis 6. Seismic Design Load Criteria 7. Ground Motion Parameters 8. Response of UG Structures to Ground Shaking 9. Large Ground Deformations 10. Conclusions

  • 1. Types of UG Structures The presentation focuses on tunnels

    Cut-and-cover tunnels Bored tunnels Immersed tunnels

    Most issues are applicable to other UG structures including Cut-and-cover structures Portal Structures Deep Chambers Waste Repositories (e.g.: nuclear)

  • 2. Earthquake Effects on UG Structures

    Two major effects 1. Ground Shaking (major concern)

    Due to seismic waves 2. Ground Failure

    Liquefaction Slope instability Fault Displacement

  • 2. Earthquake Effects on UG Structures

    Severity in both Effects depends on Structure geometry Depth to structure Soil properties Structural properties Ground motion characteristics

  • 2. Earthquake Effects on UG Structures

    On-ground structures Inertia of the structure and resonance are

    important

    UG structures Inertia of structure (gross11kN/m3) is less than the

    inertia of surrounding soil - mostly disregarded

  • 2. Earthquake Effects on UG Structures

    Misguided conception exists due to the small structural inertia

    However, seismic design of UG structures is governed by Free-field ground motion, and SSI

    (see figures)

  • 2. Earthquake Effects on UG Structures

    (Kawashima 2006)

    Significant inertia effect

  • 2. Earthquake Effects on UG Structures

    (Kawashima 2006)

    Insignificant inertia effect

    Similar frequency content

  • 3. Observed Performance of UG Structures to EQ Documented case histories of EQ damages to UG

    structures exist (ASCE, JSCE, Researchers)

    In western US UG structures built as early as 1927 Measured free-field PGA: 0.1g - 0.25g Observed damages to date are insignificant

    (including during Loma Prieta and Northridge) However, experts warn: maximum anticipated

    seismic events not reached Hashash et al, 2001

  • 3. Observed Performance of UG Structures to EQ Daikai Subway Station, Japan, exhibited

    severest damages so far: Existing Conditions

    Cut-and-fill, box-type construction Central columns at 3.5m interval Box: 17m wide by 7.17m high Columns: 0.4m by 1.0m in section and 3.82m high 4.8m overburden No seismic consideration in its design (1962)

    Kawashima 2000, 2006

  • 3. Observed Performance of UG Structures to EQ Daikai Subway Station: Extent of Damage

    Severe damage occurred during 1995 Kobe EQ 35 center columns damaged (See figure) Roof slab collapsed Road on the surface settled by 2.5m Columns with light shear r. bars failed Columns with additional zigzag r. bars survived Transverse walls provided at change of station width

    were damaged saving the columns

    Hashash et al, 2000; Kawashima, 2000, 2006

  • 3. Observed Performance of UG Structures to EQ Center column failure Mechanism of failure

    Kawashima 2000, 2006

  • 3. Observed Performance of UG Structures in General Less damage than in surface structures

    Damages decrease with depth

    Cut-and-cover tunnels are more vulnerable than deep bored tunnels

    Structures in rocks are safer than in soils

    Stabilization of surrounding soil is more

    effective than increasing liner thickness

    Hashash et al, 2001

  • 3. Observed Performance of UG Structures to EQ - General

    Damage may be related to PGA and PGV

    Strong-motion duration is very important to fatigue and excessive deformation

    Slope stability is important in portal structures

    Damages to lined tunnels are less than in pipelines

    Hashash et al, 2001

  • 4. Seismic Design Procedure

    Step 1: Defining the Seismic Environment

    Step 2: Evaluation of Ground Response to Shaking

    Step 3: Assessment of Structural Behavior

  • 4. Seismic Design Procedure

    Step 1: Defining the Seismic Environment Conducting Seismic Hazard Analysis (SHA)

    Establishing Design Criteria

    Establishing Design Ground Motion Parameters

  • 4. Seismic Design Load Procedure

    Step 2: Evaluation of Ground Response

    It involves evaluating Ground Shaking: the main focus here

    Ground Failure

  • 4. Seismic Design Load Procedure

    Step 3: Assessment of Structural Behavior

    Establishing Seismic Design Loading Criteria

    Determination of Response of UG Structures to Ground Deformation

    Any Special considerations

    Hashash et al, 2001

  • 5. Seismic Hazard Analysis

    Characterizes potential for strong ground motions for a given region by studying Extent of active faulting, Potential for fault motion, and Recurrence rate

    Two approaches available Deterministic seismic hazard analysis (DSHA) probabilistic seismic hazard analysis (PSHA)

  • 5.1. DSHA Aims at a particular seismic scenario to

    summarize hazard at a site and involves 1. Identification of EQ sources: geometry, potential

    (M) 2. Source-to-site distance of each 3. Identification of controlling EQ in terms of a

    ground motion parameter: attenuation Relations are employed for this purpose

    4. Definition of seismic hazard in terms of PGA, PGV, PGD, RS and TH of the design EQ

  • 5.2 PSHA Accounts for uncertainties in the size, location,

    and recurrence rate of EQs probabilistically 1. Identification of EQ sources with probability

    distribution of location for each 2. Characterization of seismicity/temporal

    distribution 3. Determination of ground motion by all sizes of EQs

    with uncertainties considered 4. Combination of uncertainties to establish the

    probability that a given ground motion parameter will be exceeded for a given time period

  • 5.2 PSHA Seismic Hazard Maps (GSHAP)

    PGA up to 0.24g in Africa

    The EARS has possibly the highest hazard

    SA may experience up to 0.16g

    PGA for 475-years return period

  • 5.2 PSHA Seismic Hazard Maps

    PGA up to 0.24g In EARS region

    Many vulnerable populous cities and towns in EARS region

    Capital cities with high hazard: Asmara, Djibouti, Addis Ababa, Juba, Kampala, Bujumbura

  • 5.2 PSHA Seismic Hazard Maps (GSHAP)

    According to SABS 2010, SA may experience up to 0.1g from EQ And up to 0.2g from mining activities

    SABS Standards Division, 2010

  • 5.2 PSHA Generally, site-specific seismic hazard studies are

    recommended for major structures in a specific area

    A lot has yet to be done in Africa regarding seismic hazard assessment, especially in EARS region

    The lack of awareness among policy makers even engineers is quite alarming

    In contrast to its relatively low seismic hazard, SA can be cited as a good example in updating seismic codes (e.g. SABS 2010)

  • 6. Seismic Design Load Criteria

    Dual Criteria: 1. MDE: aims at life safety (corresponds to ULS)

    In PSHA, 3 5% probability of exceedance in the

    life span of the facility (usually 50 years)

    Worst combination of DL, LL, EQ to be considered

  • 6. Seismic Design Load Criteria

    Dual Criteria: 2. ODE: minimizes economic risk (corresponds to

    SLS) Occurrence: at least once in design life In PSHA, 40 50% probability of exceedance Facility should be operational during and after

    event with little or no damage Thus, response must remain elastic

  • 6. Seismic Design Load Criteria

    Load Combinations: 1. MDE

    Cut-and-cover tunnels

    U=DL+LL+E1+E2+EQ

    Bored tunnels U=DL+LL+EX+H+EQ

  • 6. Seismic Design Load Criteria

    Load Combinations: 2. ODE Cut-and-cover tunnels

    U=1.05DL+1.3LL+1.05(E1+E2)+1.3EQ

    Bored tunnels U=1.05DL+1.3LL+1.5EX+H+1.3EQ

  • 7. Design Ground Motion Parameters

    Maximum/effective A, V and D are employed to define MDE or ODE

    Damage to UG structures are better correlated to particle v and u than to a

    Most attenuation relations available for A, but also for V and D

    In the absence of site-specific data, available relations may be used to estimate PGV and PGD from PGA (see Tables)

  • 7. Design Ground Motion Parameters (Power et al. 1996)

    Mw Ratio: PGV(cm/s)/PGA(g)

    Source-to-site distance (km)

    0-20 20-50 50-100

    Rock (vs>750m/s)

    6.5 66 76 86

    7.5 97 109 97

    Stiff soil (200-750m/s)

    6.5 94 102 109

    7.5 140 127 155

    Soft soil (

  • 7. Design Ground Motion Parameters (Power et al. 1996)

    Mw Ratio: PGD(cm)/PGA(g)

    Source-to-site distance (km)

    0-20 20-50 50-100

    Rock (vs>750m/s)

    6.5 18 27 30

    7.5 43 56 69

    Stiff soil (200-750m/s)

    6.5 35 41 48

    7.5 89 99 112

    Soft soil (

  • 8. Response of UG Structures

    Modes of Response (see Figures)

    1. Compression-extension

    2. Longitudinal bending

    3. Ovaling (for circular shapes)

    4. Racking (for rectangular)

  • 8. Response of Ground Shaking

    Hashash et al 2001

  • 8. Response of Ground Shaking

    Hashash et al 2001

  • 8. Response of Ground Shaking

    Hashash et al 2001

  • 8. Response of UG Structures

    MAIN Focus: Response to ground shaking A number of approaches available

    1. Free-field deformation Approach 2. SSI Approach 3. Seismic Deformation Method (for soft ground) 4. Numerical Approaches

  • 8.1 Free-Field Deformation (FFD) Approach FFD describes strains due to elastic plane

    waves in the absence of structures It imposes the free-field deformation on the UG

    structure Does not account for SSI Provides first-order estimate of structural

    response Closed-form relations available FFD is effective tool for small soil deformations

    (low-seismic areas, stiff soils)

  • 8.1 Free-Field Deformation (FFD) Approach Axial and Bending FFD is based on Newmarks (1968) idealization of

    elastic waves (see sketch)

    St. John and Zahrah (1987) used this to calculate axial and curvature strains analytically due to the three wave types shown schematically (see sketch)

    All solutions are available in closed form: longitudinal, normal and shear strains and curvature due to P-, S- and Rayleigh waves

  • 8.1 Free-Field Deformation (FFD) Approach Axial and Bending

    Power et al 1996

  • 8.1 Free-Field Deformation (FFD) Approach Axial and Bending

    Power et al 1996

  • 8.1 Free-Field Deformation (FFD) Approach Axial and Bending Tunnel modeled as an elastic beam, combined

    free-field axial and curvature deformations are obtained as

    For P-waves:

    For S-waves:

    For Rayleigh waves (compression component):

  • 8.1 Free-Field Deformation (FFD) Approach - Axial and Bending

    With increasing r, the curvature contribution increases

    However, this component is generally small

    Note: the apparent wave velocities, VP and VS, fall in

    the range of 4-8km/s and 2-4km/s, respectively These are close to wave velocities in deep rock

    than in the shallow soil

  • 8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation

    Ovaling

    refers to the distortion of circular tunnels (see Figure)

    is caused by waves inducing transverse strains

    Is predominantly due to vertically propagating shear waves

  • 8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation Non-perforated ground Perforated ground

    Wang 1993

  • 8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation

    In non-perforated ground (see Figure):

    In perforated ground (see Figure):

    This is an upper bound

  • 8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation

    The perforated ground scenario

    gives 2 to 3 times larger distortion than the non-perforated case

    gives an upper bound distortion criterion

    Provides a good estimate for thin linings

  • 8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation

    The non-perforated ground scenario gives better estimate for lining stiffness

    comparable with the medium

    For stiffer linings, distortion can even be less than in the non-perforated case

  • 8.1 Free-Field Deformation (FFD) Approach Racking Deformation

    Racking

    refers to the distortion of rectangular tunnels (see Figure)

    Associated deformations can be computed from shear strains available in closed form

    Alternatively, numerical site response analysis can be used

  • 8.1 Free-Field Deformation (FFD) Approach Racking Deformation

  • 8.2 Soil-Structure-Interaction (SSI) Approach

    Accounts for soil-structure interaction

    Tunnels are modeled as beams on elastic foundation (see Figure)

    SSI is accounted for quasi-statically through use of linear springs

    No dynamic inertia interaction is considered

    The internal forces are as shown (see Figure)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Model

    (After Kawashima 2000)

  • 8.2 Soil-Structure-Interaction (SSI) Approach: Internal Forces Sectional forces Circumferential forces

    Hashash et al . 2001

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending

    The maximum axial strain (due to a 45-degrees incident shear wave):

    A= free-field displacement response amplitude of idealized sinusoidal shear wave; Q= frictional force; L=Wave length; Ka= longitudinal spring stif

    Hashash et al . 2001

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending

    The maximum bending strain due to a zero-degree incident shear wave:

    The maximum shear force:

    Kt= transversal spring stiffness; Ic=mom. of inertia

    Hashash et al . 2001

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending

    The spring coefficients:

    The wave length:

    Where, for an assumed uniform soft soil layer over rock:

    Hashash et al . 2001

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending

    The ground displacement amplitude for a sinusoidal wave:

    For free-field axial strains

    For free-field bending strains

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending

    A conservative estimate of the total axial strain is given by

    Finally, the structure is designed to sustain these strains

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    The ovaling response of a tunnel is a function of the compressibility and flexibility ratios, C and F defined as:

    C: a measure of extensional stiffness F: a measure of flexural stiffness

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    Assuming full slip conditions (for soft soils and severe shaking):

    The diametric strain:

    Maximum thrust: (see Figure) The maximum b. moment:

    Where (See Plots)

    K1= Lining response coefficient

  • 8.2 Soil-Structure-Interaction (SSI) Approach Forces due to ovaling

  • 8.2 Soil-Structure-Interaction (SSI) Approach Forces due to ovaling

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    For most tunnels, the interface condition is between the full-slip and no-slip cases

    The full-slip case may cause significant underestimation of Tmax

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    The no-slip condition can give maximum thrust as given by

    Where the lining response coefficient is given by:

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    Variation of K2, and thus of Tmax, against C and F for =0.35 is as plotted (see graph)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    The normalized lining deflection:

    (see Plots)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling

    Observations from the plots: For F1 (softer lining in stiffer soil): The lining deforms more than the free field

    For F: lining deflection equals that of the perforated ground

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking Box-type structures are less efficient to transmit

    static loads Thus,

    the walls and slabs are thicker and the structure stiffer SSI is more important than in circular tunnels

    Besides, ground deformations may be larger due to Site amplification at shallow depth Decreased soil stiffness due to lower overburden

    pressure Different nature of backfill

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking

    The increased rigidity for statics reduces structural strains

    Hence, design based on free-field strains is too conservative

    Closed-form solutions are not available due to variable geometric characteristics

    The stiffness of the soil in simple shear relative to the structure is the most important factor

    (Wang 1993)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking

    It can be easily shown that the soil-to-structure flexibility ratio is given by (see Figure) Where W is the width and S1 is the unit racking

    stiffness of the structure given by (see Figure)

    (Hashash et al 2001)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking

    (Hashash et al 2001)

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking For simple structures the racking stiffness can be

    determined from ordinary frame analysis

    Thus, F for a one-barrel frame with moments of inertia, IR=IS and IW, for the slabs and walls is

    F can similarly be obtained for other common forms

  • 8.2 Soil-Structure-Interaction (SSI) Approach - Racking

    FE studies showed the following F0: structure is rigid; do not rack regardless of

    ground distortion F1: Structure racking is larger than soil F: Nearly Zero stiffness of structure; same

    deformation as the perforated ground

  • 8.2 Seismic Deformation Method

    Emerged out of a 5-year research in Japan (1972-1977) for UG structures in soft ground

    The modeling accounts for SSI Consists of idealizing the UG structure as

    Beam on elastic foundation (for axial and bending deformations) (see Figure)

    Spring-mass modeling 2D FE model for in-plane ovaling/racking

    (After Kawashima 2006)

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    (Kawashima 2006)

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    The governing DE neglecting inertia Axial deformation:

    Bending deformation:

    The idealized ground deformation (see sketch):

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    (Kawashima 2006)

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    The wave length based on Guide Specifications: Where

    VS and VSB: shear wave velocities of soil (average) and

    rock; L1 and L2 are corresponding wave lengths

    TS: fundamental natural period

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    The ground surface displacement amplitude: SV: design velocity response spectrum at bedrock

    level The surface strains are determined by

    differentiating the surface deformation, the amplitudes being

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    The ratio of the strain amplitudes:

    For a uniform soil over rock, it can be easily shown that

    Thus, for a uniform soil:

    The strain ratio varies in the range of

  • 8.2 Seismic Deformation Method Beam on elastic foundation

    The deformation of the structure is determined by solving the DEs

    The internal forces for design easily follow from the constitutive laws

  • 8.2 Seismic Deformation Method Spring-mass system

    (Kawashima 2006)

    Soil mass is included

    3D analysis is possible

  • 8.2 Seismic Deformation Method In-plane 2D FE model

    (Kawashima 2006)

    Suitable for ovaling/ racking

    Analysis is in 2D

  • 9. Large Ground Deformations Large ground deformations during EQ are

    associated with Liquefaction Fault displacement Slope Instability

    Since UG structures are commonly long, They may generally cross soil formations susceptible

    to liquefaction Crossing active faults may not be avoidable Certain structures like portals ca be susceptible to

    slope instability Hence, considerations for these issues are equally

    important as for the ground shaking

  • 10. Conclusions Knowledge is not as well established as in on-

    ground structures

    Measured data and studies are fewer

    A few state-of-the-art reviews are available

    Seismic loadings on UG structures are not as insignificant as commonly perceived

    FFD and SSI are very important considerations

    In contrast, structure inertia plays a minor role

  • 10. Conclusions

    The FFD Approach is sufficient for anticipated small ground deformations (case in point: Africa?)

    The SSI approach and SDM are also easy to use

    For the continent: FFD, SSI and SDM approaches are recommendable Complicated numerical modeling do not appear to be

    necessary, at least currently

  • 10. Conclusions

    Considerations for large ground deformations are equally important

    Adaptation of design guides is not difficult and is recommendable

    Regular follow-up of the global state-of-the-art is helpful for improvement

  • Thank You

    Seismic Design Aspects of Underground StructuresOutline1. Types of UG Structures2. Earthquake Effects on UG Structures2. Earthquake Effects on UG Structures2. Earthquake Effects on UG Structures2. Earthquake Effects on UG Structures2. Earthquake Effects on UG Structures2. Earthquake Effects on UG Structures3. Observed Performance of UG Structures to EQ3. Observed Performance of UG Structures to EQ 3. Observed Performance of UG Structures to EQ3. Observed Performance of UG Structures to EQ3. Observed Performance of UG Structures in General3. Observed Performance of UG Structures to EQ - General4. Seismic Design Procedure4. Seismic Design Procedure4. Seismic Design Load Procedure4. Seismic Design Load Procedure5. Seismic Hazard Analysis5.1. DSHA5.2 PSHA5.2 PSHA Seismic Hazard Maps (GSHAP)5.2 PSHA Seismic Hazard Maps5.2 PSHA Seismic Hazard Maps (GSHAP)5.2 PSHA6. Seismic Design Load Criteria6. Seismic Design Load Criteria6. Seismic Design Load Criteria6. Seismic Design Load Criteria7. Design Ground Motion Parameters7. Design Ground Motion Parameters(Power et al. 1996)7. Design Ground Motion Parameters(Power et al. 1996)8. Response of UG Structures8. Response of Ground Shaking8. Response of Ground Shaking8. Response of Ground Shaking8. Response of UG Structures8.1 Free-Field Deformation (FFD) Approach8.1 Free-Field Deformation (FFD) Approach Axial and Bending8.1 Free-Field Deformation (FFD) Approach Axial and Bending8.1 Free-Field Deformation (FFD) Approach Axial and Bending8.1 Free-Field Deformation (FFD) Approach Axial and Bending8.1 Free-Field Deformation (FFD) Approach - Axial and Bending8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation8.1 Free-Field Deformation (FFD) Approach Ovaling Deformation8.1 Free-Field Deformation (FFD) Approach Racking Deformation8.1 Free-Field Deformation (FFD) Approach Racking Deformation8.2 Soil-Structure-Interaction (SSI) Approach8.2 Soil-Structure-Interaction (SSI) Approach - Model8.2 Soil-Structure-Interaction (SSI) Approach: Internal Forces8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending8.2 Soil-Structure-Interaction (SSI) Approach - Axial and Bending8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach Forces due to ovaling8.2 Soil-Structure-Interaction (SSI) Approach Forces due to ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Ovaling8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Soil-Structure-Interaction (SSI) Approach - Racking8.2 Seismic Deformation Method8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Beam on elastic foundation8.2 Seismic Deformation Method Spring-mass system8.2 Seismic Deformation Method In-plane 2D FE model9. Large Ground Deformations10. Conclusions10. Conclusions10. ConclusionsThank You