The Relationships Between Absorption, Alterability and Granulation of Coarse Aggregates from Different Lithologies from Southern Brazil

This paper studies the mathematical and statistical correlations between absorption, alterability, and granulation of aggregates from different lithological origins in southern Brazil. In order to achieve this goal, a petrographic analysis of the aggregates was carried out, in addition to a qualitat...

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Detalhes bibliográficos
Autores: Ceccato, Haline Dugolin, Back, Ana Helena, Sagrilo, Amanda Vielmo, Nummer, Andrea Valli, Pinheiro, Rinaldo José Barbosa, Baroni, Magnos
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2024
País:Brasil
Recursos:Universidade Federal do Rio de Janeiro (UFRJ)
Repositorio:Anuário do Instituto de Geociências (Online)
Idioma:inglés
OAI Identifier:oai:ojs.pkp.sfu.ca:article/55983
Acesso em linha:https://revistas.ufrj.br/index.php/aigeo/article/view/55983
Access Level:acceso abierto
Palavra-chave:Granulation
RStudio
Degree of alterability
Descrição
Resumo:This paper studies the mathematical and statistical correlations between absorption, alterability, and granulation of aggregates from different lithological origins in southern Brazil. In order to achieve this goal, a petrographic analysis of the aggregates was carried out, in addition to a qualitative evaluation of granulation/alterability and absorption tests for the 1/2” (12.5 mm), 3/8” (9.5 mm), and #4 (4.75 mm) sieve. Statistical analysis relied on the Shapiro-Wilk and Breusch-Pagan tests, using R-Studio software. The results show that the variables “granulation” and “alteration” exhibit satisfactory correlations with the variable “absorption”, indicating that the larger the grain size the lower the absorption, while the higher the alteration the higher the absorption. The more the particle size decreases, the greater the variable “absorption” can explain “granulation”. Regarding the alteration and absorption degree, the analysis was not feasible, since  the analyzed group that included high absorption and low alteration volcanic rocks could modify the trend, contradicting the consensus that the more altered the rock, the more it absorbs. Overall, the employed methodology proved to be satisfactory for the database analyzed, with the suggestion of increasing the number of samples in future studies.