Report - Oregon State Library: State Employee Information Center ...
Report - Oregon State Library: State Employee Information Center ...
Report - Oregon State Library: State Employee Information Center ...
You also want an ePaper? Increase the reach of your titles
YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.
1.0 INTRODUCTION<br />
1.1 BACKGROUND<br />
Experience worldwide has demonstrated that bridges and ancillary components (abutments,<br />
approach fills and embankments, pile foundations) located at sites of shallow groundwater and/or<br />
adjacent to bodies of water are highly susceptible to earthquake-induced damage. Liquefaction of<br />
adjacent soils causes a significant amount of the damage. Susceptible soils consist of loose,<br />
saturated, non-cohesive soils that are frequently found in marine and river environments.<br />
Earthquake damage to bridge abutments and embankments is commonly manifested as ground<br />
failures, excessive lateral displacements, and/or settlements. There are many cases of widespread<br />
damage to bridge foundations and approach structures resulting from the lateral displacements<br />
and settlements of surrounding soil.<br />
Earthquake damage to bridges severely impedes response and recovery efforts following the<br />
event. Highways serve as primary lifelines following natural disasters and communities rely on<br />
their access. From a practical perspective, the seismic performance of a bridge is related to its<br />
serviceability following an earthquake. Numerous cases have been documented in postearthquake<br />
reconnaissance reports of bridges that performed well from a structural perspective,<br />
yet were inaccessible due to excessive deformations of approach fills and adjacent foundation<br />
soils. Additionally, the magnitude and pattern of soil deformation around bridges often results in<br />
damage to structural elements.<br />
Bridge abutments and deep foundations are particularly vulnerable to seismic damage. Damage<br />
to bridges has been well documented (see the appendix of this report). For most bridges at river<br />
crossings subjected to medium- to high-intensity earthquake motions, liquefaction occurred and<br />
was likely the primary cause of the reported damage. Contributing factors include reduced<br />
stability of earth structures due to the transient inertial loads, increased active pressures on<br />
abutments due to the loss of soil strength and the seismic inertia of the backfill, and the loss of<br />
passive soil resistance adjacent to the toe of abutments and slopes. All of these factors are<br />
exacerbated by the presence of liquefiable soils. The substantial reduction of strength and<br />
stiffness of the soil leads to possible geotechnical failures including catastrophic ground failures,<br />
limited, yet damaging lateral ground deformations, and/or excessive vertical deformations that<br />
result in uneven and often impassable grades.<br />
Limiting soil deformations adjacent to bridges is a primary seismic design issue throughout<br />
much of the western United <strong>State</strong>s. Several transportation departments are in the initial stages of<br />
adopting deformation-based seismic performance requirements. This method of design also is<br />
becoming more routine in the marine transportation and port communities. The criteria are often<br />
specified in general terms of an allowable limit state (i.e., deformation, load, moment, curvature)<br />
and the exposure time, as follows.<br />
1