2017
DOI: 10.1080/15583058.2017.1354096
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Strength anisotropy in building granites

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Cited by 9 publications
(7 citation statements)
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“…The application of NDT is, therefore, especially interesting in the case of architectural heritage. One of the most common NDT techniques to estimate the mechanical properties of building materials is the ultrasonic pulse velocity (UPV) method, which has been proved to be useful to identify the mechanical properties, anisotropy, compactness and presence of discontinuities in rocks (7)(8)(9)(10)(11). Several works have applied this technique to assess the state of conservation of historical buildings (8,(12)(13)(14).…”
Section: Introductionmentioning
confidence: 99%
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“…The application of NDT is, therefore, especially interesting in the case of architectural heritage. One of the most common NDT techniques to estimate the mechanical properties of building materials is the ultrasonic pulse velocity (UPV) method, which has been proved to be useful to identify the mechanical properties, anisotropy, compactness and presence of discontinuities in rocks (7)(8)(9)(10)(11). Several works have applied this technique to assess the state of conservation of historical buildings (8,(12)(13)(14).…”
Section: Introductionmentioning
confidence: 99%
“…One of the most common NDT techniques to estimate the mechanical properties of building materials is the ultrasonic pulse velocity (UPV) method, which has been proved to be useful to identify the mechanical properties, anisotropy, compactness and presence of discontinuities in rocks (7)(8)(9)(10)(11). Several works have applied this technique to assess the state of conservation of historical buildings (8,(12)(13)(14). UPV also has been used in combination with other NDT techniques, such as ground-penetrating radar, which has a wide range and allows high resolution of up to ten centimeters from a centimeter (14), and the Leeb rebound hardness test (7).…”
Section: Introductionmentioning
confidence: 99%
“…In previous works, it has been demonstrated that micro-cracks are already formed at lower temperatures [20] due to thermal expansion [21], cooling [22], or being linked to thermal cycles of 20 • C to 105 • C [23,24]. Temperature increase generates stresses in granitic rocks [25] which is also associated with the anisotropy of granite micro-texture [26,27]. Understanding such behavior and cracking-linked damage of the granitic rocks need further studies.…”
Section: Introductionmentioning
confidence: 99%
“…Due to Grisolia stone's historical and architectural importance, several authors have studied it extensively from a geological point of view (3)(4)(5)(6). Nevertheless, complete petrophysical and mechanical characterization has not yet been performed.…”
Section: Introductionmentioning
confidence: 99%