update of the cpt-based liquefaction triggering procedure boulanger & idriss 2014

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Update of the CPT-based liquefaction triggering procedure Boulanger & Idriss 2014 23/10/2014

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Presentation about the updated CPT triggering procedure with Boulanger & Idriss 2014CPT & SPT Based Liquefaction Triggering Procedures, CGM Report No. UCD/CGM-14/01

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  • Update of the CPT-based liquefaction triggering procedureBoulanger & Idriss 2014

    23/10/2014

  • 2

    Existing Liquefaction Analysis Methods

    Since 1970s several liquefaction analysis

    methods have been developed

    Laboratory and Field Methods

    Numerical Methods

    Empirical Methods

    Simplified Empirical Methods:

    Seed and Idriss (1971) was first

    Youd et al. (2001) (NCEER)

    Cetin et al. (2004)

    Idriss and Boulanger (2006, 2008,2014)

  • 3

    Overview of the simplified empirical methods

    Liquefaction is usually evaluated with the estimation of factor of safety against liquefaction,

    FoS or FSL

  • 4

    Idriss & Boulanger 2008 Boulanger & Idriss 2014

  • 5

    Boulanger & Idriss 2014 or B&I 2014

    B&I 2014

    Presented a revised CPT-based liquefaction triggering procedure

    New relationships for the Magnitude Scale Factor (MSF)

    Modified MSF expression to be a function of magnitude, soil type and density of the soil layer at depth

    Update of CPT-based approach

    Changed qc1N as a function of FC

    Changed CRR versus qc1Ncs

    Examination of the CPT-based case histories in terms of soil behaviour type (SBT) index, Ic

    These revisions were based on findings from experimental data

    (eg cyclic triaxial testing), analytical (eg analyses of ground

    motion records) and case history studies (including 50

    Christchurch case histories 25 CPTs summarized in Green

    et al 2014).

  • 6

    CPT-BASED CASE HISTORY DATABASE

    Limited to cases with Ic

  • 7

    CPT-BASED CASE HISTORY DATABASE

  • 8

    Magnitude Scale Factor (MSF)

    The value of Cyclic Stress Ratio (CSR) loading is calculated using the following

    History of the development of MSF

    Seed et al. (1975): proposed a relationship between "Number of Equivalent Uniform Cycles, Neq" &

    Magnitude, M, which led to the initial development of "MSF Values".

    Seed & Idriss (1982): Tabulated "MSF Values" as a function of M; used shaking table test results by

    DeAlba et al. (1976) relating CRR to "Number of Uniform Cycles".

    Idriss (1999): Used results of cyclic tests on frozen samples by Yoshimi et al. (1984) to derive a

    revised relationship between Neq & M, which resulted in a revised MSF relationship.

    Boulanger & Idriss (2014): Modified MSF expression to be a function of magnitude, soil type, and

    density (void ratio) of the soil.

    MSF=f(earthquake & ground motion characteristics; DR; FC)

    and is used to account for duration effects on the triggering of liquefaction

  • 9

    Magnitude Scale Factor (MSF)

  • 10

    Magnitude Scale Factor (MSF)

    Effects of density void ratio on slope b

    looser

    denser

  • 11

    Magnitude Scale Factor (MSF)

    looser

    denser

    The revised MSF relationship shown in Figure 2.6 is believed to provide an improved accounting

    of how this relationship should vary with soil characteristics compared to currently available MSF

    relationships that provide a single relationship for all cohesionless soils.

    MSF is picking up the Mw vs cycles; the link between CRR and Nc (density dependent) less cycles required to liquefy a looser soil than a denser one

    Loose relatively flat (need lower no of Nc to develop liquefaction)

  • 12

    LOADING - Cyclic Stress Ratio

    RESISTANCE - Cyclic Resistance Ratio

    Update of CPT-based approach, B&I 2014

    The deterministic version of the CPT-based

    correlation in terms of qc1N for different values of FC,

    rather than in terms of the equivalent clean sand

    penetration resistance (qc1Ncs)

  • 13

    Update of CPT-based approach, B&I 2014

    No change

    The terms Q and F are used in soil behavior type

    classification charts, such as the chart shown in

    Figure (Robertson 1990, SBT).

    The exponent n varies from 0.5 in sands to 1.0 in

    clays (Robertson and Wride 1998).

    The term Ic represents the radial distance between

    any point on this chart and the point defined by Q =

    2951 and F = 0.06026%.

    Circular arcs defined by constant Ic values are used

    to approximate the boundaries between different soil

    behavior types in this chart

  • 14

    Update of CPT-based approach, B&I 2014

    Large scatter

    Ic=2.6 ranging from 15% to 100% FC

    Correlation of lab estimation with

    representative CPT depth

    Inherent limitations in using Ic to

    predict FC

    Influence of fines - plasticity

    Large uncertainty in the Ic vs FC due

    to:

  • 15

    Update of CPT-based approach, B&I 2014

    CFC

    CFC is a fitting parameter

    based on specific data or in

    the absence set equal to

    0.0 (mean) and check for

    SD=0.29

    Positive CFC for larger

    estimate of FC

    Negative CFC for lower

    estimate of FC

    CFC = 0.07 is approximately

    equal to the relationship

    developed by Robinson et

    al (2013) for liquefiable

    soils along the Avon River

  • 16

    Update of CPT-based approach, B&I 2014

    Equivalent clean sand

    adjustment (qc1Ncs) which are

    considered appropriate for non-

    plastic to low-plasticity silty

    fines M.. due to changes in the

    updated case history dataset

    More FC correction in B&I

    2014

    5.4

    16.0 0.01 0.01

    I&B 2008B&I 2014

  • 17

    B&I 2014 and MBIE Clarifications and updates

    Mw SLS ILS ULS

    PGA

    7.5 0.13 0.20 0.35

    6.0 0.19 0.30 0.48

    CFC=0.07

    B&I 2014 [A]

    B&I 2014 [B]

    Lower Mw higher PGA is more

    critical for B&I 2014 triggering

    method

    Mw=7.5 is critical for I&B 2008

    Mw=6.0 is critical for B&I 2014

  • 18

    Update of CPT-based approach, B&I 2014

    For sites outside of the Canterbury earthquake region, it would only be appropriate to adopt the 2014

    methodology where a seismic hazard de-aggradation plot or other data has been examined to determine

    appropriate representative design events

    Implementation of 2014 liquefaction triggering procedure for mapping of expected damages at SLS, ILS or

    ULS levels of seismic loading REQUIRE use of representative PGA-M values consistent with de-

    aggregation of seismic hazard

    Highlights the importance of PGAs on either back or forth estimation of liquefaction triggering and the use

    of any of existing liquefaction vulnerability parameters (Sv1D, LPI, LSN, LPIc etc)

    Deterministic towards a Performance Based Liquefaction Analysis (Kramer et al, 2008 Performance-

    Based Liquefaction Potential Evaluation), which is another way to characterize liquefaction potential in

    terms of the liquefaction resistance (CRR q or N) required to produce a desired level of performance

    Prudent to perform parametric analyses

    Using CFC=-0.29, 0.0, 0.29 to evaluate the sensitivity to FC estimates

    Ic cut-off shall be repeated for 2.4, 2.6 and 2.8 to evaluate sensitivity to this parameter

    Results can then be used to illustrate the importance of site-specific sampling and testing for a given

    project, while recognizing that some amount of sampling and testing should always be required for

    high risk / high consequence projects

  • 19

    Examples

  • 20

    Examples CBD, Bealey Avenue

    80% clay-like 20% sand-like

  • 21

    Examples Cashmere

    60% clay-like 40% silt-like

  • 22

    Examples Woolston

    80% sand-like 20% silt-like

  • 23

    Examples Beckenham

    20% sand-like 80% silt & clay-like

  • 24

    Examples New Brighton

    100% sand-like

  • 25

    Examples Aranui

    100% sand-like

  • 26

    Examples Parklands

    25% clay-like 75% sand-like

  • 27

    Examples CBD, Bealey Avenue

    80% clay-like 20% sand-like

    2008, 7.5

    0.13 0.20 0.350.19 0.30 0.48

    2014, 6.0

  • 28

    Examples CBD, Bealey Avenue

    80% clay-like 20% sand-like

    2008, 7.5

    0.13 0.19

    2008, 6.0

    2014, 7.5 2014, 6.0

  • 29

    2008, 7.5

    0.13 0.20 0.350.19 0.30 0.48

    2014, 6.0

    Examples New Brighton

    100% sand-like

  • 30

    2008, 7.5

    0.13 0.19

    2008, 6.0

    2014, 7.5 2014, 6.0

    Examples New Brighton

    100% sand-like

  • 31

    Elements that affect site response in order of importance:

    Input motion (Mw PGA)

    Soil profile

    Soil material properties

    Method of analysis