2.1 Definition of the model
The implemented numerical model (Figure 1) intends to represent the most generic conditions with a Finite Difference code (FLAC v8, Itasca, 2016), exploiting the flexibility and available library of advanced constitutive models provided by this tool. The calculation setup has been validated assigning specific seismic, subsoil and building conditions of a known case study where liquefaction was carefully surveyed. The adopted two-dimensional layout consists of three horizontal layers developed on a width of 40 meters and a total depth of 20 meters, with an upper low-permeability cap (Layer #1), an intermediate liquefiable layer (Layer #2) and a lower base clay (Layer #3). The typical calculation mesh consists of 13,980 rectangular elements of 0.8m width and variable heights (0.5 m for the above and below layers, 0.4 for the liquefiable layer), these dimensions chosen after the suggestion of Kuhleimeyer & Lysmer (1973), who found that propagation of seismic waves in continuum media can be simulated with sufficient accuracy if the element’s dimension is smaller than 1/10 of the minimum propagating wavelength. The stress-strain response of the liquefiable soil has been simulated with PM4Sand Version 3.1 (Boulanger and Ziotopoulou, 2017) chosen thanks to its capability to capture the cyclic behavior of saturated sand. It represents an evolution of the Dafalias and Manzari (2004) formulation, being a stress-ratio controlled, critical state compatible, bounding surface plasticity model developed primarily for earthquake engineering applications (Boulanger and Ziotopoulou, 2015). The stress-strain response of the shallow and deepest layers is simulated using Mohr-Coulomb hysteretic model, considering the stress state induced into the subsoil by the above building. Luque and Bray (2015) and Luque and Bray (2017) showed that the primary aspects of the dynamic response of a 3D system in terms of liquefaction-induced building settlement can be captured in 2D analyses by using tributary mass and stiffness with the primary goals being to capture the mass and stiffness. The superstructure is modeled with an equivalent beam characterized with a flexural stiffness (EI) and a contact pressure (q). The EI modulus summarizes the bending stiffness of the building-foundation system. For framed buildings it can be computed dividing the sum of stiffnesses of all parallel longitudinal frames by the transversal extension of the building. A lower bound stiffness of frames can be computed neglecting the upper decks and considering the transverse section of the foundation element only (Mazzolani, 1967), nil in case of isolated footings. Alternatively, a more realistic estimate can be obtained adding the bending moments of the upper decks, computing the moments of inertia of transverse sections with reference to the center axis of each deck (Sherif and Koenig, 1975).
The contact pressure q summarizes the contribution of all building floors and can be computed multiplying the number of floors times the overall unit load, i.e. the load per unit area including the self-weight of structural and non-structural elements and the accidental loads.
2.2 Calibration and validation
The prototype model has been firstly validated with the back-analysis of a building located in the Municipality of Terre del Reno, whose data are extracted from the Emilia-Romagna Regional database. The building consists of a two storeys masonry building with a rectangular layout (length 13.10 m, width 11.10 m) founded on a shallow slab of poor structural characteristics. The liquefaction induced by the May 20th earthquake (Mw=6.1) caused significant differential settlements in the East-West direction, with an absolute settlement of 35 cm on the West side and 5 cm on the East side (Figure 2.b). Being the epicenter located about 15 km far from the building, at a depth approximately equal to 10 km below the ground level (Luzi et al., 2019), the acceleration time history assigned for the back analysis (Figure 2.c) has been computed transferring to the considered site the signal recorded at the nearest seismic station (Mirandola, from the ITACA seismic catalogue) with the procedure suggested by Sinatra & Foti (2015). These authors propose to deconvolve the acceleration time history recorded at the station to recover the signal the seismic bedrock, then apply the attenuation law proposed by Bindi et al. (2011) to move from the station to the studied site, then perform a local seismic response analysis to obtain the input at the model’s base. In the analysis, the deeper subsoil model has been taken from Fioravante et al. (2013), while the top subsoil stratigraphy has been reconstructed considering various CPTU tests performed in the closest area around the building (Figure 2.a).
The physical properties for the three strata have been derived from Fioravante et al. (2013), while permeability, friction angle (ϕ), cohesion (c) and undrained shear strength (cu) of the fine-grained soils are taken from Sinatra and Foti (2015). For the upper and lower layers, the experimental stiffness decay and damping curves have been derived from Fioravante et al. (2013) and their calibration has been performed simulating the cyclic simple shear tests with the adopted numerical model (Figure 3). Finally, the effective strength values and the large strain stiffness parameters have been taken from the literature (Itasca Consulting Group, Inc., 2016).
The PM4Sand model for the intermediate layer (#2) has been calibrated setting twenty one parameters with the default values recommended by Boulanger and Ziotopoulou (2017) and finding the remaining three (i.e. sand’s apparent relative density Dr, shear modulus coefficient Go, and contraction rate parameter hpo) reproducing with the numerical code (FLAC v8, Itasca, 2016) the cyclic undrained behavior of the liquefiable sandy layer seen on four triaxial undrained cyclic tests performed by Facciorusso et al. (2016) Figure 4.a, 4.b and 4.c. The complete list of models and parameters for the three layers is given in (Table 1).
The building has been simulated with an elastic body of given width (B=12m), flexural stiffness (EI=60 MN*m) and contact pressure (q=50 kPa). The performed analysis returned a significant rotation of the building with a final vertical displacement at the west corner of 37 cm and at the east side corner of about 4 cm. The similarity between computed and observed settlements confirms that the adopted numerical tool can be reliably adopted for simulating the effects of liquefaction upon general conditions as accomplished in the following parametric study.
Table 1. Subsoil parameters assigned in the calculation.
Stratum
|
Model
|
n
|
γnat (kN/m3)
|
Permeability
|
φ' (°)
|
C' (kPa)
|
Cu (kPa)
|
K (Mpa)
|
G (Mpa)
|
c0
|
c1
|
Dr
|
G0
|
hp0
|
nb
|
Nd
|
Silty cap
|
Mohr-Coulomb
|
0.5
|
16.5
|
1.00E-07
|
28
|
2
|
34
|
2.67
|
1.6
|
-3
|
0.2
|
/
|
/
|
/
|
/
|
/
|
Sands
|
PM4Sand
|
0.5
|
18.5
|
7.00E-06
|
33
|
0
|
/
|
16.7
|
10
|
/
|
/
|
0.4
|
507
|
20
|
0.5
|
0.1
|
Clays
|
Mohr-Coulomb
|
0.4
|
18
|
6.00E-08
|
20
|
8
|
45
|
0.67
|
0.4
|
-2
|
0.2
|
/
|
/
|
/
|
/
|
/
|
2.3 Parametric study
The physical, mechanical and geometrical factors varied in the parametric analysis have been chosen following Karimi et al. (2018) who observed the mean permanent settlement of the building is affected by respectively contact pressure, seismic input, thickness, relative density and depth of the liquefiable layer, but also by the presence of a low-permeability cap. These parameters have thus been varied in the model as summarized in Table 2, positioning the water table at the ground level for all calculations. The structure-foundation system has been modeled with an equivalent plate characterized by width (B) and flexural stiffness modulus (EI). (see Table 2). In addition a set of six numerical analysis has been performed to evaluate relevance of the structure's inertial mass, simulating height/width ratio (H/B) ranging between 0.5 and 1.5.
Finally, considering the fundamental role played by the earthquake magnitude, four waveforms have been applied in the analysis, extracting them from the PEER Strong Ground Motion Databases. The velocity time history of these events, chosen thanks to their largely different Arias intensity (Table 3), have been scaled by three amplitude factors, respectively 0.7, 1.0 and 1.6 in order to introduce the role of earthquake intensity in the analysis. Combining the seismic input with the parameters reported in Table 2, about 320 analyses have been carried out.
The typical output of calculation consists of the displacements profile below the foundation (Figure 5) from which the following characteristic variables are extracted:
- maximum, minimum and mean settlement: wMax, wmin and wav;
- angular distortion: β;
- horizontal deformation: eh.
Table 2. Parameters for sensitivity analyses
Parameter
|
Description
|
Range of variation
|
Hc
|
Layer #1 (non-liquefiable crust) thickness (m)
|
2 to 6 m
|
HL
|
Layer #2 (liquefiable layer) thickness (m)
|
4 to 12 m
|
Hb
|
Layer #3 (lower clay) thickness (m)
|
20 m-HL-Hc
|
Dr
|
Relative density of the liquefiable layer (%)
|
20 to 60%
|
su
|
Undrained shear strength of crust and lower clay (kPa)
|
25 to 100 kPa
|
B
|
Foundation base width (m)
|
10 to 30 m
|
Q
|
Contact pressure at the building foundation (kPa)
|
25 to 100 kPa
|
EI
|
Equivalent stiffness of the building foundation system (MN*m)
|
0 to 260 MN*m
|
PGV
|
Peak ground velocity (m/s)
|
0.23 to 0.63 m/s
|
Table 3. Selected seismic input.
Earthquake
|
PGV (m/s)
|
Ia (m/s)
|
Emilia-Romagna
|
0.33
|
0.64
|
Northridge
|
0.42
|
4.5
|
Imperial Valley
|
0.47
|
1.6
|
Northridge
|
0.63
|
2.8
|
2.3 Sensitivity study
A sensitivity study has been initially performed to understand the relative influence of the varied parameters on the kinematic variables defined in Figure 5. Firstly, the relation between mean and maximum settlements (wav and wMAX) has been investigated (Figure 6) as their equivalence is needed for the following analyses where their outputs are alternatively related to the angular distortion of the building-foundation system. Figure 6 shows a proportionality between these two variables, being the ratio wav/wmax equal on average to 0.84, with minimum and maximum values equal to respectively 0.73 and 0.98.
The results of calculation are then summarized looking at the dependency of maximum, differential settlement, and angular distortion (respectively wMAX, δ and β) on each of the parameters varied in the analysis. Figures 7 to 12 show sample results obtained assigning the seismic input of Emilia Romagna scaled for the different amplifying factors. Figures 7 and 8 point out the influence of the upper impervious crust characterized with thickness (HC) and undrained shear strength (su). All curves show the positive role of both parameters on all the considered components of the foundation movement, attenuation rates being more remarkable for the stronger seismic events. Settlements reduce almost linearly within the considered thickness range (Hc≤6 m) for the higher seismic intensities (f=1.0 and 1.6), while reduction is smoother for the lower intensity earthquake (f=0.7) (Figure 7); attenuation rate is very high for undrained shear strength su increasing up to 50 kPa, then drops progressively for increasing su (up to 100 kPa and more) (Figure 8). The two plot sets reveal that, despite preventing the excess pore pressure exhaust, the impervious crust contributes significantly with its strength to limit the liquefaction effects on buildings.
Figures 9 and 10 show the influence of the liquefiable layer. The settlements and deformation increase rather continuously with thickness (HL), being rates dependent on the earthquake intensity (Figure 9). On the contrary, variation with soil density is sharper, effects being critical for low density material (Dr=20%) where wMAX reaches values as high as 2.5m (for f=1.6), then reduces rapidly for Dr=40%, moreover for Dr=60%.
Finally, Figures 11 and 12 summarize the effect of the building-foundation system, characterized by length B and flexural stiffness EI. Width produces a noticeable reduction on the absolute settlements throughout the considered variation (Figure 11.a), less evident on the differential component (Figure 11.b and c). On the other hand, flexural stiffness EI produces a continuous reduction on the differential settlements and angular distortion (Figure 12. b and c) but has negligible effects on the absolute settlements (Figure 12.a).
2.3.1 Role of Superstructure Inertia
Considering the limited relevance of the structure's inertial mass and of the height/width ratio seen by Karimi et al. (2018) and willing to limit the analysis to low-rise buildings, the structure-foundation system has been modeled with an equivalent plate so that inertia effects from the superstructure were avoided. In order to investigate the consistency of this assumption, six numerical simulations have been performed modelling the framed superstructure, considering several height/width ratios (H/B). The equivalent-linear-perfectly-plastic response of structural components has been reproduced through beam elements that can sustain axial force, shear force, and bending moment. The effect of this simplification is presented in terms of ratio between foundation movements computed with the basic analysis and the corresponding results of the parametric analyses with superstructure inertia (ρ). In particular, Figure 13 shows a negligible effect of the superstructure inertia on the predicted response, characterized by a variation ranging between -4% and +7%, for the examined cases. This finding is comparable with Karamitros et al. (2013), who observed a deviation of predictions less than ±5% and confirmed by field evidence. For instance, Yoshida et al. (2001) examined building behavior in Adapazari during the 1999 Kocaeli earthquake in Turkey and noted that buildings with a liquefaction induced settlements and tilts, did not suffer severe inertia-induced structural damage, as opposed to numerous buildings in the non-liquefied areas of the city, which totally or partially collapsed because of structural system failure. Karamitros et al. (2013) ascertained that these results are justifiable by two mechanisms acting as natural seismic isolation and minimizing the inertial forces developing on the superstructure as well as the associated horizontal shear forces and overturning moments applied to the foundation. The first mechanism is related to the sand stiffness degradation and its considerable decrease of the system’s natural frequency, thus deamplifying the applied dynamic excitation. Furthermore, liquefaction also activates a failure mechanism, which further inhibits the input motion from propagating to the footing.