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Dingee Reservoir Final Seismic Report - East Bay Municipal Utility ...

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Table 8<br />

<strong>Seismic</strong> Slope Stability Analysis Results<br />

Yield Coefficients (FS ~1.0)<br />

Section Downstream, K y Upstream, K y<br />

A-A’ 0.15 g 0.45 g<br />

7.4.2 Earthquake-Induced Newmark Displacements<br />

The seismic slope deformations were evaluated using a simplified Newmark sliding block<br />

analysis (1965). The method is based on the assumption of rigid-perfectly plastic stress-strain<br />

behavior and potential failure surface using a sliding-block type approach. In the sliding-block<br />

approach, a slope is idealized as a rigid mass above a plane of sliding with specified yield<br />

acceleration. If design acceleration levels of the block are lower than the yield acceleration, no<br />

movement will occur along the sliding plane. If the design accelerations are higher than the<br />

yield acceleration, there will be net movement between the block and the base, i.e.<br />

displacements. The horizontal displacements of the sliding block are calculated by double<br />

integrating the difference between the earthquake-induced average acceleration of the slide mass<br />

and its yield acceleration with respect to time.<br />

These time histories were then double integrated using the computer program SHAKE2000 to<br />

develop the displacement time history for a yield coefficient of 0.15g. Plate 25 shows a plot of<br />

the estimated deformation on the downstream slope of the dam for the three time histories<br />

considered for both normal and reverse polarity cases that can be either the maximum or<br />

minimum.<br />

Table 9: Newmark Slope Displacement Estimates<br />

Average of 3 Earthquakes<br />

Yield Accel. Max Average Min<br />

0.10 4.01 3.45 2.90<br />

0.15 2.23 1.82 1.40<br />

0.20 1.28 1.05 0.82<br />

0.25 0.73 0.63 0.52<br />

0.30 0.40 0.37 0.34<br />

The figure below and Table 9 summarize the results of the Newmark slope deformation<br />

estimates for the downstream slope verses different values of yield acceleration. The minimum,<br />

maximum, and arithmetic average values of displacements are shown in Table 9. The maximum<br />

refers to the higher of the normal or reverse polarity values from the site specific time history. A<br />

conservative best estimate for the yield acceleration for the downstream slope from our stability<br />

evaluations was 0.15g. We calculated the range for the average horizontal deformations to be<br />

1.4 to 2.2 feet. We computed the average horizontal displacement to be about 3½ feet and the<br />

corresponding crest settlement to be less than 2 feet for the historic high reservoir storage levels<br />

of 772-feet.<br />

<strong>Seismic</strong> Stability Evaluation <strong>Report</strong><br />

<strong>Dingee</strong> <strong>Reservoir</strong> Dam<br />

19<br />

August 2008

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