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Thermal effects on the physical properties of limestone from the Yucatan Peninsula

Published online by Cambridge University Press:  30 July 2014

W.S. Gónzalez-Gómez
Affiliation:
Applied Physics Department, Cinvestav-Unidad Mérida, Carr. Ant. a Progreso km 6, C.P. 97310 Mérida, Yucatán, México.
J. May-Crespo
Affiliation:
Applied Physics Department, Cinvestav-Unidad Mérida, Carr. Ant. a Progreso km 6, C.P. 97310 Mérida, Yucatán, México.
P. Quintana
Affiliation:
Applied Physics Department, Cinvestav-Unidad Mérida, Carr. Ant. a Progreso km 6, C.P. 97310 Mérida, Yucatán, México.
A. May-Pat
Affiliation:
Centro de Investigación Científica de Yucatán, Unidad de Materiales, Calle 43, No.130, Col. Chuburná de Hidalgo, CP 97200, Mérida, Yucatán, México.
F. Avilés
Affiliation:
Centro de Investigación Científica de Yucatán, Unidad de Materiales, Calle 43, No.130, Col. Chuburná de Hidalgo, CP 97200, Mérida, Yucatán, México.
J. J. Alvarado-Gil
Affiliation:
Applied Physics Department, Cinvestav-Unidad Mérida, Carr. Ant. a Progreso km 6, C.P. 97310 Mérida, Yucatán, México.
B.O. Ortega
Affiliation:
Departamento de Microbiología Ambiental y Biotecnología, Universidad Autónoma de Campeche, Av. Agustín Melgar s/n, Campeche, Campeche 24039, México.
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Abstract

Rocks are composed of minerals, bounding matrix, cracks and pores. The study of changes in the physical properties of rocks as a function of heat treatment is relevant to various engineering and industrial applications. The effect of thermal damage on the compression, strength, ultimate compression strain, color and loss of mass of two different limestones extracted from the Yucatan Peninsula is studied. Different thermal treatments are applied by heating the sample from room temperature up to 600°C, with steps of 100°C. The results show a high correlation between the heat transport characteristics, mechanical properties, content of organic matter and the presence of carbonates and iron oxides in each type of limestone rock.

Type
Articles
Copyright
Copyright © Materials Research Society 2014 

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References

REFERENCES

Cabadas, H. V., Solleiro, E., Sedov, S., Pi, T., Alcalá, J. R., Eurasian Soil Sci., 43, 14391457 (2010)CrossRefGoogle Scholar
Alonzo-Salomón, L. A., Espinoza-Graham, L., Ingeniería, 7-1, 2736 (2003).Google Scholar
Ozsoy, E.A., Yilmaz, G., Arman, H., Sci. Res. Essays, 5, 25792587 (2010).Google Scholar
ASTM D2216-98. Standard test method for laboratory determination of water (Moisture) content of soil and rock by mass. West Conshohocken (PA, USA): ASTM International (2007).Google Scholar
Yokoyama, T., Nakashima, S., Chem. Geol. 219, 309320 (2005).CrossRefGoogle Scholar
Yamanio, Y., Takeuchi, S., Okumura, S., Nakashima, S., Yokoyama, T., J. Volcanol. Geotherm. Res., 178, 8183 (2008).CrossRefGoogle Scholar
Pospíšil, J., Hrd&ubrcy, J., Optik, 118, 278288 (2007).CrossRefGoogle Scholar
Rizov, B., J Univ Chem Technol Metall. 47, 2, 207210 (2012).Google Scholar