The use of Mt. Epomeo Green Tuff (MEGT) as a building stone is widespread on Ischia Island (Italy). We assess here the fire resistance of MEGT by thermally stressing samples to temperatures up to 1000 °C. Porosity and uniaxial compressive strength increase and decrease from 44% and 4.5 MPa at ambient temperature to 48% and 1.5 MPa following exposure to 1000 °C, respectively. Complementary thermogravimetric and X-ray powder diffraction analyses, experiments that monitor acoustic emissions during heating/cooling, and microstructural observations highlight that these changes are the result of thermal microcracks, formed due to the breakdown of zeolites and clays (MEGT contains 35 wt.% analcime, 15 wt.% smectite, and 3 wt.% illite) at high temperature. Although the stability of structures built from MEGT will be jeopardised at high temperature, a very low thermal diffusivity requires that fires must burn for many hours to compromise the strength of a typical dimension stone: tuffs are tough in the event of fire.
Fire resistance of the Mt. Epomeo Green Tuff, a widely-used building stone on Ischia Island (Italy) / Heap, Michael; Kushnir, Alexandra; Griffiths, Luke; Wadsworth, Fabian; Marmoni, Gianmarco; Fiorucci, Matteo; Martino, Salvatore; Baud, Patrick; Gilg, H. Albert; Reuschlé, Thierry. - In: VOLCANICA. - ISSN 2610-3540. - ELETTRONICO. - 1:1(2018), pp. 33-48. [10.30909/vol.01.01.3348]
Fire resistance of the Mt. Epomeo Green Tuff, a widely-used building stone on Ischia Island (Italy)
Marmoni, Gianmarco;Fiorucci, Matteo;Martino, Salvatore;
2018
Abstract
The use of Mt. Epomeo Green Tuff (MEGT) as a building stone is widespread on Ischia Island (Italy). We assess here the fire resistance of MEGT by thermally stressing samples to temperatures up to 1000 °C. Porosity and uniaxial compressive strength increase and decrease from 44% and 4.5 MPa at ambient temperature to 48% and 1.5 MPa following exposure to 1000 °C, respectively. Complementary thermogravimetric and X-ray powder diffraction analyses, experiments that monitor acoustic emissions during heating/cooling, and microstructural observations highlight that these changes are the result of thermal microcracks, formed due to the breakdown of zeolites and clays (MEGT contains 35 wt.% analcime, 15 wt.% smectite, and 3 wt.% illite) at high temperature. Although the stability of structures built from MEGT will be jeopardised at high temperature, a very low thermal diffusivity requires that fires must burn for many hours to compromise the strength of a typical dimension stone: tuffs are tough in the event of fire.File | Dimensione | Formato | |
---|---|---|---|
Heap_Fire_2018.pdf
accesso aperto
Note: https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/6/11
Tipologia:
Versione editoriale (versione pubblicata con il layout dell'editore)
Licenza:
Creative commons
Dimensione
9.26 MB
Formato
Adobe PDF
|
9.26 MB | Adobe PDF |
I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.