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Analysis and modelling of the seismic behaviour of high ... - Ingegneria

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2. DUCTILITY AND SEISMIC RESPONSE OF STRUCTURES<br />

The basis, <strong>modelling</strong> approaches, <strong>and</strong> acceptance criteria <strong>of</strong> <strong>the</strong> NDP are similar to<br />

those <strong>of</strong> <strong>the</strong> NSP. The main exception is that <strong>the</strong> response calculations are carried<br />

out using a time-history analysis. With <strong>the</strong> NDP, design displacements are not<br />

established using a target displacement, but are determined directly through<br />

dynamic analysis using ground motion histories instead. Calculated responses can<br />

be <strong>high</strong>ly sensitive characteristics <strong>of</strong> individual ground motions; in fact, when<br />

subjected to different ground motions, a model will <strong>of</strong>ten produce quite dissimilar<br />

responses that are difficult to predict a priori. Therefore, it is recommended to carry<br />

out analyses with more than one ground motion record. This variability also leads<br />

to <strong>the</strong> need for statistical treatment <strong>of</strong> multi-record IDA output in order to<br />

summarize <strong>the</strong> results <strong>and</strong> in order to use <strong>the</strong>m effectively in a predictive mode, as<br />

for example in a PBE context. In accordance with Eurocode 8 (2002), depending<br />

on <strong>the</strong> nature <strong>of</strong> <strong>the</strong> application <strong>and</strong> on <strong>the</strong> information actually available, <strong>the</strong><br />

description <strong>of</strong> <strong>the</strong> <strong>seismic</strong> motion may be made by using artificial accelerograms<br />

<strong>and</strong> recorded or simulated accelerograms. Artificial accelerograms shall be<br />

generated so as to match <strong>the</strong> elastic response spectra for 5% viscous damping ( =<br />

5%). The duration <strong>of</strong> <strong>the</strong> accelerograms shall be consistent with <strong>the</strong> magnitude <strong>and</strong><br />

<strong>the</strong> o<strong>the</strong>r relevant features <strong>of</strong> <strong>the</strong> <strong>seismic</strong> event underlying <strong>the</strong> establishment <strong>of</strong> ag.<br />

When site-specific data are not available, <strong>the</strong> minimum duration Ts <strong>of</strong> <strong>the</strong> stationary<br />

part <strong>of</strong> <strong>the</strong> accelerograms should be equal to 10 s. Recorded accelerograms or<br />

accelerograms generated through a physical simulation <strong>of</strong> source <strong>and</strong> travel path<br />

mechanisms may be used, provided that <strong>the</strong> samples used are adequately<br />

qualified with regard to <strong>the</strong> seismogenetic features <strong>of</strong> <strong>the</strong> sources <strong>and</strong> to <strong>the</strong> soil<br />

conditions appropriate to <strong>the</strong> site, <strong>and</strong> <strong>the</strong>ir values are scaled to <strong>the</strong> value <strong>of</strong> agS for<br />

<strong>the</strong> zone under consideration. The suite <strong>of</strong> artificial <strong>and</strong> recorded or simulated<br />

accelerograms should observe <strong>the</strong> following rules:<br />

a. a minimum <strong>of</strong> 3 accelerograms should be used;<br />

b. <strong>the</strong> mean <strong>of</strong> <strong>the</strong> zero period spectral response acceleration values<br />

(calculated from <strong>the</strong> individual time histories) should not be smaller than<br />

<strong>the</strong> value <strong>of</strong> agS for <strong>the</strong> site in question;<br />

c. in <strong>the</strong> range <strong>of</strong> periods between 0,2T1 <strong>and</strong> 2T1 where T1 is <strong>the</strong> fundamental<br />

period <strong>of</strong> <strong>the</strong> structure in <strong>the</strong> direction where <strong>the</strong> accelerogram will be<br />

applied no value <strong>of</strong> <strong>the</strong> mean 5% damping elastic spectrum, calculated<br />

from all time histories, should be less than 90% <strong>of</strong> <strong>the</strong> corresponding value<br />

<strong>of</strong> <strong>the</strong> 5% damping elastic response spectrum.<br />

The <strong>seismic</strong> motion, represented in terms <strong>of</strong> ground acceleration time-histories <strong>and</strong><br />

related quantities (velocity <strong>and</strong> displacement) shall consist <strong>of</strong> three simultaneously<br />

acting accelerograms. The same accelerogram may not be used simultaneously<br />

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