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Tensile behaviour in natural building stone: Serena sandstone

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Abstract

The tensile behavior of Serena sandstone is investigated by means of uni-axial tensile and bending tests. In order to obtain an overall characterisation of a quasi-brittle material, such as Serena sandstone, it is necessary to investigate the post-peak softening branch by adopting a stable control system. Test results on different size specimens are presented. Also analysed in this paper is the effect of the boundary conditions in a uni-axial tensile test by comparing free and fixed platens tests. A laser interferometry technique (ESPI) was adopted to investigate the strain field and crack propagation in the material.

A notable outcome of the research is the location of crack penetration before the peak load, that in the case of the bending test is almost constant in specimens of different size.

Résumé

Le comportement en traction du Grès de Serena est étudié ici au moyen d'essais de traction et de flexion mono-dimensionnels. Da façon à caractériser de manière générale un matériau quasifragile, tel que le grès de Serena, il est nécessaire d'étudier le domaine “plastique”, après le point de charge maximale en adoptant un système de pilotage stable. Les résultats des essais effectués sur des échantillons de taille différente sont présentés. Le présent article documente également l'effet des conditions aux limites dans un essai de traction pure, en comparant des essais avec platines libre et fixe. Une technique d'interférométrie LASER (ESPI) a été adoptée pour étudier le champ de contraintes et la propagation des fissures dans le matériau. Un résultat remarquable de cette recherche est la mise en évidence d'une amorce de fissure avant l'application de la charge maximale, que l'on peut constamment observer sur des échantillons de taille différente, lors des essais de flexion.

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Abbreviations

σN t :

nominal stress in uni-axial tensile test

σN b :

nominal stress in four-point bending test

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Meda, A. Tensile behaviour in natural building stone: Serena sandstone. Mat. Struct. 36, 553–559 (2003). https://doi.org/10.1007/BF02480833

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