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Airport Liquefaction Susceptibility Analysis Report - ABAG ...

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Fugro Consultants, Inc.<br />

Project No. 04.79221200<br />

Table 1. Ground Motion Parameters for <strong>Liquefaction</strong> Assessment<br />

Peak Ground Acceleration (PGA) / Moment Magnitude (M)<br />

(PGA 7.5)<br />

<strong>Airport</strong> Location<br />

(V s30) 3 1906 San Hayward-<br />

10% Probability 2% Probability of<br />

Concord-<br />

Francisco Rodgers<br />

of Exceedance in Exceedance in<br />

Green Valley<br />

Earthquake Creek<br />

Scenario 1 Scenario 1 Scenario 1 50-Years<br />

50-Years<br />

Scenario 2 Scenario 2<br />

San Francisco<br />

International<br />

<strong>Airport</strong> (200 m/s)<br />

0.48 / 7.8<br />

(0.53)<br />

0.27 / 7.26<br />

(0.25)<br />

0.15 / 6.71<br />

(0.11)<br />

0.48 / 8.0<br />

(0.57)<br />

0.75 / 8.0<br />

(0.89)<br />

Oakland<br />

International<br />

<strong>Airport</strong> (210 m/s)<br />

0.32 / 7.8<br />

(0.35)<br />

0.35 / 7.26<br />

(0.32)<br />

0.20 / 6.71<br />

(0.15)<br />

0.49 / 6.7<br />

(0.37)<br />

0.73 / 6.7<br />

(0.55)<br />

Buchanan Field<br />

<strong>Airport</strong> (250 m/s)<br />

0.15 / 7.8<br />

(0.17)<br />

0.24 / 7.26<br />

(0.22)<br />

0.53 / 6.71<br />

(0.40)<br />

0.54 / 6.6<br />

(0.39)<br />

0.87 / 6.6<br />

(0.63)<br />

Livermore<br />

Municipal <strong>Airport</strong><br />

(330 m/s)<br />

0.18 / 7.8<br />

(0.20)<br />

0.25 / 7.26<br />

(0.23)<br />

0.17 / 6.71<br />

(0.13)<br />

0.53 / 6.7<br />

(0.40)<br />

0.84 / 6.7<br />

(0.63)<br />

Moffett Federal<br />

Airfield (290 m/s)<br />

0.31 / 7.8<br />

(0.34)<br />

0.32 / 7.26<br />

(0.29)<br />

0.10 / 6.71<br />

(0.07)<br />

0.49 / 6.7<br />

(0.37)<br />

0.75 / 6.7<br />

(0.56)<br />

Notes:<br />

1 Based on the PGA data points provided by USGS<br />

2 Based on USGS deaggregation calculator (2013)<br />

3 Based on USGS V s30 maps (2013)<br />

5.1.2 Groundwater<br />

Depth-to-groundwater (DTW) is an important variable in the assessment of liquefaction<br />

susceptibility since saturated soil conditions are required for liquefaction to occur. Saturation<br />

reduces the effective normal stress of near-surface sediment, increasing the likelihood of<br />

earthquake-induced liquefaction (Youd, 1973). DTW can vary daily, seasonally, and annually,<br />

as well as locally and regionally.<br />

For this assessment, only near-surface groundwater (i.e., groundwater levels at depths less<br />

than 40 feet) was considered and applied. The DTW data was compiled from CPT and borehole<br />

logs, and historical high ground water levels published by the California Geological Survey<br />

(2006 and 2008).<br />

17<br />

May 31, 2013

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