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sessione 2.3 - Ogs

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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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