Estudio de propiedades físicas de las rocas

El objetivo de este taller es mostrar a los alumnos mediante experiencias de laboratorio sencillas y de bajo coste algunas metodologías de estudio de las propiedades físicas de las rocas como material de construcción. Las propiedades físicas de las rocas determinan su uso y comportamiento tanto como materiales de construcción como soportes de obra civil. La determinación de las propiedades físicas complementan el estudio mineralógico y textural (petrográfico) de los materiales pétreos y naturales. Las propiedades petrofísicas más importantes que se abordan en este taller son el sistema poroso (porosidad); transporte de fluidos (permeabilidad, capilaridad); propiedades mecánicas (estáticas y dinámicas); la durabilidad de las rocas frente a las sales, hielo, ataque ácido, etc.

The influence of rock fabric in the durability of two sandstones used in the Andalusian Architectural Heritage (Montoro and Ronda, Spain)

Natural stone has been a popular and reliable building material throughout history appearing in many historic monuments and in more recent buildings. Research into the intrinsic properties of specific stones is important because it gives us a greater understanding of the factors that limit and act on them. This can help prevent serious problems from occurring in our buildings bringing both esthetic benefits and financial savings. To this end, the main objective of this research has been to study the influence of the fabric and the mineral composition of two types of sandstone on their durability. The first is a red continental sandstone from the Buntsandstein Age called “Molinaza Roja”, which is quarried in Montoro (Cordoba). The second is quarried in Ronda (Malaga) and is sold under the trade name of “Arenisca Ronda”. It is a light pink-whitish calcarenite deposited during the Late Tortonian to Late Messinian. We characterized their petrological and petrophysical properties by studying their rock fabrics, porous systems and mechanical properties. In order to obtain a complete vision of the behavior of their rock fabrics, we also carried out two decay tests, the salt crystallization and the freeze–thaw tests. We then measured the effects on the textures of the altered samples during and after the decay tests and we evaluated the changes in the porous system. By comparing the results between intact and altered samples, we found that Arenisca Ronda is less durable because it has a high quantity of expandable clays (smectites) and a high percentage of pores in the 0.1–1 μm range, in which the pressure produced by salt crystallization is strongest. In Molinaza Roja the decay agents caused significant sanding due to loss of cohesion between the clasts, especially during the salt crystallization test. In both stones, the anisotropies (oriented textures) have an important role in their hydric and dynamic behavior and also affect their mechanical properties (especially in the compression resistance). No changes in color were detected.