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Article |
1 John A. Blume Earthquake Engineering
Center
Department of Civil and Environmental Engineering
Stanford
University
Stanford, California
94305-4020
ptothong{at}stanford.edu
cornell{at}stanford.edu
This article presents an empirical ground-motion prediction model
(attenuation
relation) for inelastic (as opposed to elastic) spectral displacement
(Sdi) for
ground motions without forward directivity effects. It is a function of two
earthquake
parameters, moment magnitude (Mw) and the closest distance
to rupture (Rrup), and
two bilinear oscillator parameters, an undamped elastic period (T) and
a yield displacement
(dy). The dy is introduced via the
predicted median strength-reduction
factor (
), a proxy for the ratio of elastic spectral
displacement (Sde) to dy, which is
identical with the familiar strength-reduction factor (R). The proxy
recognizes that
R can only be estimated indirectly because it implicitly contains the
random variable,
Sde, which cannot be known a priori; therefore, the
median estimate or predicted
median (
de) from a conventional (elastic) ground-motion
prediction model is used
instead to calculate
=
de/dy. For enhanced generality, the
inelastic spectral displacement
prediction model here is based on a ratio concept, that is, the total model
is a (any) conventional elastic prediction model coupled with a new inelastic
displacement
ratio prediction model, with proper statistical correlation between the two.
We empirically consider the dependence of this ratio on source and path effects
(i.e.,
Mw and Rrup), and find that
Mw is significant, but Rrup is not. The
resulting prediction
model can easily be added to existing probabilistic seismic-hazard analysis
(PSHA)
software packages with only one extra structure-specific parameter,
dy of the oscillator.
In practical engineering applications, this will likely have been estimated from
the conventional static pushover analysis of the multi-degree-of-freedom
(MDOF)
structure under consideration.
The resulting PSHA product is a hazard curve for Sdi, the inelastic spectral displacement of a nonlinear oscillator. Such a curve can provide a more direct hazard- based target displacement for nonlinear static procedures (Federal Emergency Management Agency [FEMA] 356, 2000) and/or a basic input function for new probabilistic seismic-demand analyses that is based on Sdi (as opposed to Sde) as an efficient and sufficient intensity measure. This new attenuation relationship will be particularly useful in evaluating the performance of existing structures and specified designs with known lateral strength. In particular, unlike most past studies, it does not pre-fix the ductility level.
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