Physical characterization of an extensive volcanic rock in México: “red tezontle” from Cerro de la Cruz, in Tlahuelilpan, Hidalgo, Mexico

Tezontle is an extrusive volcanic rock, coming in black or red in color. Despite its many uses and applications, there are few studies concerning the attributes of this rock. Therefore, this work to the physical characterization of red tezontle samples, taken from Tlahuelilpan, Hidalgo, Mexico. Afte...

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Detalles Bibliográficos
Autores: Ponce Lira, Brenda, Ortiz Polo, Araceli, Otazo Sánchez, Elena María, Reguera Ruiz, Edilso, Acevedo Sandoval, Otilio Arturo, Prieto Garcia, Francisco, Gonzalez Ramírez, César Abelardo
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2013
País:México
Institución:UNIVERSIDAD DE GUANAJUATO
Repositorio:Acta Universitaria
Idioma:español
OAI Identifier:oai:www.actauniversitaria.ugto.mx:article/462
Acceso en línea:https://www.actauniversitaria.ugto.mx/index.php/acta/article/view/462
Access Level:acceso abierto
Palabra clave:Tezontle
volcanic rock
physical characterization.
roca volcánica
caracterización física.
Descripción
Sumario:Tezontle is an extrusive volcanic rock, coming in black or red in color. Despite its many uses and applications, there are few studies concerning the attributes of this rock. Therefore, this work to the physical characterization of red tezontle samples, taken from Tlahuelilpan, Hidalgo, Mexico. After grinding and sieving, the following properties were obtained: humidity (0.37% to 0.48%), weighed moisture-retention capacity (7.50% – 43.56%) and volumetric mois­ture-retention capacity (5% – 25%), which justifies its hydroponic and gardening uses; particle density (2.37 g cm-3 - 2.83 g cm-3), dry bulk density (0.87 g cm-3 - 1.33 g cm-3), total pore space (52.83% - 63.90 %), specific surface area (5.558 m2 g-1 and 9.66 m2 g-1) and cation exchange capacity (4.04 Cmol(+) kg-1), whose low values contradict the high efficiency reported for cation removal. The preliminary analysis of the X-ray diffraction pattern shows intense peaks of quartz and suggests the presence of plagioclases (anorthite and albite).