Embargoed until 11 A.M., PST
NSF PR 97-74 - December 10, 1997
This material is available primarily for archival purposes. Telephone
numbers or other contact information may be out of date; please see current
contact information at media
contacts.
Sediment Study 'Good News' for Quake-Prone Southern
California
The Los Angeles basin's sediments seem to lessen the
ground motion that threatens single-story and low-rise
buildings in a severe earthquake, a new study of data
from the 1994 Northridge quake has revealed. The study
was conducted through the National Science Foundation
(NSF)'s Southern California Earthquake Center.
University of Southern California seismologist Edward
H. Field says that his team's research, which is published
in this week's issue of the journal Nature,
is "good news" for Southern California.
"This work is an important step in our efforts to
mitigate the damage caused by earthquakes," says James
Whitcomb, program director in NSF's division of earth
sciences, which funds SCEC. "Now, we must categorize
the geological conditions and building types for which
this phenomenon holds true. That's the cutting edge
of future earthquake research."
Geologically, the Los Angeles basin is a valley filled
with debris (sediments) that eroded from neighboring
mountains over hundreds of thousands of years, Field
notes. For more than a century, scientists have known
that such sediments usually amplify ground motion
in earthquakes. But seismologists and engineers disagree
as to whether the degree of amplification will change
as the level of shaking increases.
Do all sediment-filled valleys shake like a bowl of
jelly in larger earthquakes, as they do during smaller
quakes? Or do some behave like a bowl of sand in which
seismic energy is "absorbed" as the grains rub together,
effectively reducing ground motion?
Based on laboratory studies of sediments, engineers
have argued for the bowl-of-sand theory and have designed
structures on the assumption that amplification factors
go down as the level of shaking increases -- that
is, that the shaking effects of a stronger earthquake
aren't boosted as much as those of a smaller quake.
Seismologists, though, have traditionally argued for
the bowl-of-jelly model. They have seen little evidence
that sediment amplification is reduced, especially
when the soil is of the stiff, dry variety found in
the Los Angeles basin. They have therefore been concerned
that some engineering designs may fail to account
for the degree of seismic hazard that sediments actually
pose.
The new study provides the first evidence based on
large-scale measurements that the answer is closer
to the engineering view than seismologists had thought.
Sediment amplification in the Los Angeles basin would
be significantly reduced during large earthquakes,
the researchers found. Although the Nature
paper takes a step toward settling the debate, the
researchers believe more work is needed to assess
whether current engineering practices adequately reflect
the degree of seismic hazard posed by the local sediments.
Editors: Field will attend the meeting of the
American Geophysical Union in San Francisco during
the week of publication. He may be reached at the
Westin St. Francis Hotel at (415) 397-7000.
|