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Table 8.6: Summary of PGA values<br />
LOCATION<br />
EARTHQUAKE SCENARIOS<br />
M w = 6.2 M w = 7.0 M w = 8.5 M w = 9.0<br />
Soil (Crest of Levee) 0.16g 0.18g 0.11g 0.12g<br />
Bedrock (Sandy River Sandstone) 0.29g 0.38g 0.12g 0.14g<br />
8.6 LIQUEFACTION ANALYSIS<br />
The liquefaction analyses performed in this study consisted of: (1) computing the cyclic shear<br />
stresses in the soil deposits for each scenario earthquake (CSR EQ ), (2) calculating the cyclic shear<br />
stress required to initiate liquefaction in the cohesionless soils (CRR), (3) comparing the results<br />
of steps 1 and 2 to assess the liquefaction susceptibility of the soil, and (4) utilizing the results of<br />
step 3 to estimate the cyclic shear strength of the soil.<br />
8.6.1 Determination of the Cyclic Stress Ratio<br />
The determination of earthquake induced cyclic shear stresses can be estimated in two ways: (1)<br />
by performing a simple empirical analysis developed by Seed and Idriss (1971, 1982, updated<br />
summary by Youd and Idriss, 1997), or (2) by performing a more in-depth, site-specific dynamic<br />
ground response analysis (SHAKE91). The cyclic shear stresses computed from the SHAKE91<br />
analyses were used for this example problem. The computed cyclic shear stresses used in the<br />
liquefaction analyses are the “equivalent uniform” ( eq. uniform ) shear stresses. The maximum shear<br />
stress ( max ) is reduced by the reduction factor (n given in Equation 8-1) using Equation 8-2 to<br />
account for the irregular and transient nature of the shear stress time history. The eq. uniform is then<br />
normalized by the effective overburden stress ( vo ′) to produce the CSR induced by the<br />
earthquake as given in Equation 8-3. Figure 8.17 shows the CSR versus depth for the magnitude<br />
6.2 earthquake motions employed in this study.<br />
τ<br />
<br />
n *<br />
eq.uniform<br />
τ max<br />
(8-2)<br />
CSR<br />
<br />
τ<br />
eq.uniform<br />
σ<br />
vo<br />
'<br />
(8-3)<br />
8.6.2 Determination of the Cyclic Resistance Ratio<br />
As defined in Chapter 3, the CRR describes the ability of the soil to resist the cyclic loading<br />
induced by the earthquake. The CRR can be determined through empirical relationships based<br />
largely on SPT and/or CPT penetration resistance, or laboratory tests. Both methods were used in<br />
this project and they are discussed in the following sections.<br />
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