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Evaluation Process

In document Interim Guidelines (Page 65-67)

4. POST-EARTHQUAKE EVALUATION

4.2 Preliminary Evaluation

4.2.1 Evaluation Process

Preliminary evaluation is the process of determining if a building should be subjected to detailed post-earthquake evaluations. Detailed evaluations should be performed for all buildings thought to have experienced strong ground motion, as indicated in Section 4.2.1.1 or for which the other indicators of Section 4.2.1.2 apply. Detailed post-earthquake evaluations include the entire process of determining if a building has experienced significant damage and if damage is found, determining appropriate strategies for occupancy, structural repair and/or modification. Except as indicated in Section 4.2.3, detailed evaluation should include inspections of a

representative sample of moment-resisting (and other type) connections within the building. 4.2.1.1 Ground Motion

Within UBC Seismic Zone 4 {NEHRP Map Area 7}, detailed evaluation is recommended for all WSMF buildings when an earthquake of Magnitude greater than or equal to 6.5 has produced ground motion at the building site in excess of 0.20g, or when any earthquake has produced ground motion at the building site in excess of 0.30g. For buildings located in zones of lower seismicity, refer to Table 4-1, Section 4.2.2 for appropriate ground motion thresholds. Whenever feasible, ground motion estimates should be based on actual instrumental recordings in the vicinity of the building. When such instrumental recordings are not available, ground motion estimates may be based on empirical or analytical techniques. In all cases, ground motion estimates should reflect the site-specific soil conditions.

Commentary: A number of techniques are available for estimating the

distribution of ground motion in an area, following an earthquake. In regions with a large number of strong motion accelerographs present, actual ground motion recordings produce the best method of mapping contours of ground motion. In other regions, empirical techniques, such as the use of standard

ground motion attenuation relationships (e.g. Joyner and Boore - 1994, Campbell and Bazorgnia - 1994) may be required. These can be supplemented with

analytically derived estimates such as those obtained by direct simulation of the fault rupture and ground wave propagation. It should be noted, however, that lacking direct instrumental evidence, site-specific ground motion estimates are at best, uncertain, and subject to wide variations depending on the assumptions made. Therefore, the best indicator of the severity of ground motion at a site is often the performance of adjacent construction. The criteria of Section 4.2.1.2 are provided to help assure that sites which experienced strong ground motion are not overlooked as a result of inaccurate estimates of the ground motion severity.

4.2.1.2 Additional Indicators

Regardless of the magnitude of the earthquake event, detailed evaluation should be considered for a building if any of the following apply:

1) significant structural damage is observed in one or more WSMF structures located within 1 kilometer of the building, on sites with similar, or more firm soil profiles; 2) significant structural damage is observed to one or more modern, apparently well-

designed structures (of any material) within 1 kilometer of the building and on sites with similar, or more firm soil profiles;

3) for an earthquake having a magnitude of 6.5 or greater, the structure is either within 5 kilometers of the trace of a surface rupture or within the vertical projection of the rupture area when no surface rupture has occurred.

4) significant architectural or structural damage is observed in the building; 5) permanent interstory drift greater than 0.5% of story height is observed;

6) unexpected damage, or significant period lengthening of the building are observed in aftershocks; or

7) entry to the building has been limited by the building official because of earthquake damage, regardless of the type or nature of the damage.

Commentary: In the above, the term “significant” has been used without

definition or quantification. The intent is to use known damage as an indicator of the severity of ground motion experienced. Damage is dependent not only on the strength of ground motion, but also on the quality and condition of the affected construction. Relatively moderate damage to buildings having regular

configuration and adequate lateral-force-resisting systems may be a more

in poor condition or having other poor earthquake resisting characteristics. The building official and/or structural engineer should use their own judgment in determining the significance of such damage.

The absence of significant observable damage to WSMF structures on sites believed to have experienced strong ground motion, per Section 4.2.1, should not be used as an indication that detailed evaluations are not required. Many WSMF buildings that were structurally damaged by the Northridge Earthquake had little apparent damage based on casual observation.

The observed behavior of a building in repeated aftershocks may provide some clues as to whether it has experienced significant structural damage. In instrumented buildings it may be possible to observe a period shift in the instrumented response, as successive damage occurs. In buildings without instruments, the observation of unexpectedly large amounts of architectural damage could indicate the presence of structural damage.

In many cases in the past, buildings have initially been posted as unsafe without adequate investigation of their condition. Upon reconsideration and technical evaluation such buildings have subsequently been re-posted to allow occupancy. In such cases and for the purposes of item 7 above, the building need not be considered to have been posted.

In document Interim Guidelines (Page 65-67)