update of the cpt-based liquefaction triggering procedure boulanger & idriss 2014
DESCRIPTION
Presentation about the updated CPT triggering procedure with Boulanger & Idriss 2014CPT & SPT Based Liquefaction Triggering Procedures, CGM Report No. UCD/CGM-14/01TRANSCRIPT
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Update of the CPT-based liquefaction triggering procedureBoulanger & Idriss 2014
23/10/2014
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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)
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Overview of the simplified empirical methods
Liquefaction is usually evaluated with the estimation of factor of safety against liquefaction,
FoS or FSL
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Idriss & Boulanger 2008 Boulanger & Idriss 2014
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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).
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CPT-BASED CASE HISTORY DATABASE
Limited to cases with Ic
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CPT-BASED CASE HISTORY DATABASE
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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
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Magnitude Scale Factor (MSF)
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Magnitude Scale Factor (MSF)
Effects of density void ratio on slope b
looser
denser
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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)
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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)
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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
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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:
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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
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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
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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
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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
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Examples
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Examples CBD, Bealey Avenue
80% clay-like 20% sand-like
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Examples Cashmere
60% clay-like 40% silt-like
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Examples Woolston
80% sand-like 20% silt-like
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Examples Beckenham
20% sand-like 80% silt & clay-like
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Examples New Brighton
100% sand-like
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Examples Aranui
100% sand-like
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Examples Parklands
25% clay-like 75% sand-like
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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
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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
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2008, 7.5
0.13 0.20 0.350.19 0.30 0.48
2014, 6.0
Examples New Brighton
100% sand-like
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2008, 7.5
0.13 0.19
2008, 6.0
2014, 7.5 2014, 6.0
Examples New Brighton
100% sand-like
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Elements that affect site response in order of importance:
Input motion (Mw PGA)
Soil profile
Soil material properties
Method of analysis