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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Detalhes 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 documento: artigo
Estado:Versão publicada
Data de publicação:2013
País:México
Recursos:UNIVERSIDAD DE GUANAJUATO
Repositório:Acta Universitaria
Idioma:espanhol
OAI Identifier:oai:www.actauniversitaria.ugto.mx:article/462
Acesso em linha:https://www.actauniversitaria.ugto.mx/index.php/acta/article/view/462
Access Level:Acceso aberto
Palavra-chave:Tezontle
volcanic rock
physical characterization.
roca volcánica
caracterización física.
Descrição
Resumo: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).