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GNGTS 2009 SESSIONE <strong>2.3</strong><br />
Fig. 4 - Schematization of the simple FEM<br />
model of the school of Corno di Rosazzo<br />
(UD) and rappresentation of the first and<br />
second eigen-shapes associated to the frequencies<br />
5 Hz and 7.1 Hz respectively (computed<br />
by FEM model).<br />
Possibly, a FEM modeling can confirm or improve how obtained by tremor measurement and in<br />
some case the comparison between the measured natural frequencies and the FEM one may give<br />
information about the material. In this case the FEM model (Fig. 4) has confirmed both, the natural<br />
frequencies and the principal eigen-shapes (Tab. 1 and Fig. 5). The natural frequencies obtained<br />
via FEM model strongly depends from the loads and overall from the elastic characteristic of the<br />
material. Therefore it is possible to find for which type of material the FEM eigen-frequencies tend<br />
to the measured one. In the examined case the best result is obtained with simper stone posed with<br />
a good organization (see Tab. 3 for the elastic and mechanics characteristics).<br />
Tab. 1 - Natural frequencies and natural periods from FEM modeling.<br />
Tab. 2. Mechanical and elastic characteristic of masonry used in the FEM model.<br />
The measured natural frequency can be compared also with the values obtained by empirical<br />
relationship (i.e. Tab. 3). The empirical relationships are really fast to apply but obviously can give<br />
values that are significantly different from the real one, particularly for not regular buildings (see<br />
also Mucciarelli Tuberi, 2007, Mucciarelli et al., 2007).<br />
Tab. 3. Example of empirical relationship to compute the principal periods of some types of structures.<br />
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