http://www.cnr.it/ontology/cnr/individuo/prodotto/ID185707
Thermal diffusivity measurement in slabs using harmonic and one-dimensional propagation of thermal waves (Articolo in rivista)
- Type
- Label
- Thermal diffusivity measurement in slabs using harmonic and one-dimensional propagation of thermal waves (Articolo in rivista) (literal)
- Anno
- 2004-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1016/j.ijthermalsci.2003.10.005 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Alberto Muscio; Paolo G. Bison; Sergio Marinetti; Ermanno Grinzato (literal)
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- http://www.sciencedirect.com/science/article/pii/S1290072903001650 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
- Note
- ISI Web of Science (WOS) (literal)
- Scopu (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 1 : DIMeC--Dipartimento di Ingegneria Meccanica e Civile, Università di Modena e Reggio Emilia, Via Vignolese, 905/B, 41100 Modena, Italy
2-4 : CNR-ITC Padova section, Corso Stati Uniti, 4, 35127 Padova, Italy (literal)
- Titolo
- Thermal diffusivity measurement in slabs using harmonic and one-dimensional propagation of thermal waves (literal)
- Abstract
- The development of a novel approach to the well-known Ångström's method for the measurement of the thermal diffusivity is reported. In this method, the diffusivity is determined from the damping and the phase shift of a periodic thermal signal during its propagation along the specimen. The propagation can be easily monitored by infrared thermography. In general, a non-contact source is used to apply the signal.
In the present work, however, a direct-contact source is employed, with a temperature-oscillation signal supplied on a portion of one of the two main surfaces of the specimen, where a homogeneous contact can be yielded by using a proper contact pressure. Such practice implies that the measures of surface temperature can be used to estimate the diffusivity only beyond a certain distance from the source, where the wave-front of the temperature oscillation within the specimen becomes plane and perpendicular to the main surfaces. This distance is investigated here, to establish a general rule for the performance of the experiments.
A thermoelectric device based on the Peltier effect is employed as the thermal source. The main difficulty about its use is to obtain a perfectly harmonic and well-balanced thermal signal. This is necessary to avoid a complex processing of the experimental data, and it can be achieved by supplying a current with a properly-chosen time-evolution pattern. Such an approach, which is built upon previous work, is here enhanced by improving the underlying analytical model. (literal)
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