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On the temperature dependence of the Gruneisen function
No full textThe experimental data seem to indicate a quasi independence of the Gruneisen function on temperature at room conditions. However, this is seen to be due to a misinterpretation of the experimental data, which, already at room conditions, show a considerable weight of the anharmonic terms in the free energy. In any case, even if the experimental thermal Gruneisen parameter were rigorously independent of temperature in a range of experimental conditions, this would not grant the temperature independence of the companion parameter entering the Mie-Gruneisen equation of state, or of the thermodynamic gamma itself in another range
Vertical movements along the northwestern side of Messina straits, in the 1967-1970 period
Get PDFThe results of a comparison of the spirit levelling data made by I.G.M. in 1967<br />and in 1970, are presented. An analysis of these data shows that the altitude<br />variations of bench marks in the considered triennial period seem to originate from<br />the collective rotation of an inclined plane, which intersects the geoid surface with<br />an azimuth of 43° to the North.<br />This is in accordance with the orientation of the fault pattern given by local<br />geology.<br />The fact that the existing bench marks were sited along the coastline, and the<br />lack of a comparison with data relative to motion on more compact geological<br />structures, lead necessarily to provisional conclusions
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