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Report - Oregon State Library: State Employee Information Center ...

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Table 8.20: Riverward Deformation Results Comparison for the Earthquake Magnitude 8.5 Analyses.<br />

METHOD OF<br />

CALCULATION<br />

RIVERWARD DISPLACEMENT: NORTH LEVEE CREST (cm)<br />

Low river stage<br />

Elev. NGVD 2.1 m<br />

100 yr flood river stage<br />

Elev. NGVD 8.8 m<br />

Newmark 17 7 0<br />

Makdisi and Seed 300 100 0<br />

Bracketed Intensity 4 1 0<br />

Results of the Parametric Study 40 30 1<br />

Numerical Model 0 16 48<br />

Levee crest river stage<br />

Elev. NGVD 13.0 m<br />

The direct comparison of the results of rigid-body, sliding block analyses with the results of the<br />

numerical model is complicated by two important issues; (1) the former methods focus only on<br />

the displacement of the slope along a single failure plane, and (2) benched slopes, like the<br />

riverside slope of the levee, should be evaluated for three different modes of failure (shallow<br />

crest, shallow bench, and deep-seated failure) when using limit equilibrium methods. In this<br />

example, the displacement values calculated from the rigid body analyses are only for failure<br />

wedges or circular slip planes associated with what was estimated to be a “critical” deep-seated<br />

riverward failure (Figure 8.24). The location and shape of the potential deep slip surface was<br />

established for the 100 year flood condition and this “critical circle” was used for the other two<br />

river stages. In slopes of cohesionless soils the critical circles are usually associated with shallow<br />

face and/or toe circles.<br />

The shallow failure modes were excluded from consideration in this example, as they were<br />

interpreted as indicating shallow sloughing. The displacements reported here did not take into<br />

account movement by other potential failure masses within the levee. The results of the<br />

Newmark and Bracketed Intensity methods show very little movement of the levee toward the<br />

river. This is in contrast to the results of the Makdisi and Seed method, which is considered to be<br />

very conservative for large magnitude earthquakes. Again, the critical failure surface indicated<br />

by the slope stability analysis for deep-seated riverward failures was used as the basis for the<br />

comparison.<br />

20<br />

Shallow Failure Surface<br />

50<br />

10<br />

Elevation, NGVD (m)<br />

0<br />

-10<br />

Deep Failure Surface<br />

0<br />

-50<br />

Elevation, NGVD (ft)<br />

-20<br />

-30<br />

-100<br />

Figure 8.24: Schematic Illustration of Shallow and Deep-seated Failure Surfaces.<br />

182

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