Structural and compositional anisotropy in Macael marble (Spain) by ultrasonic, XRD and optical microscopy methods
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Fecha
2009Materia/s Unesco
3305.32 Ingeniería de Estructuras
3305.90 Transmisión de Calor en la Edificación
3328.16 Transferencia de Calor
3312.08 Propiedades de Los Materiales
3312.09 Resistencia de Materiales
Resumen
By using the non-destructive technique of ultrasonic transmission, this paper undertakes a study of the compositional and structural discontinuities in marble from Macael (Almería, Spain), which is the material of the columns in the Court of the Lions in the Alhambra (Granada, Spain), in order to contribute to understanding of the processes of deterioration and conservation affecting them. Thermal stress is responsible for alterations in the columns, and is affected by scaling, loss of substance, stains, etc. The results allow us to establish that, apart from the discontinuities in the mineralogical composition of the marble, the preferential orientation of the calcite crystals has an important effect on its anisotropic reaction. This preferential orientation is confirmed by textural studies using X-ray diffraction and determinations using a petrographic microscope equipped with universal stage. © 2008 Elsevier Ltd. All rights reserved.
By using the non-destructive technique of ultrasonic transmission, this paper undertakes a study of the compositional and structural discontinuities in marble from Macael (Almería, Spain), which is the material of the columns in the Court of the Lions in the Alhambra (Granada, Spain), in order to contribute to understanding of the processes of deterioration and conservation affecting them. Thermal stress is responsible for alterations in the columns, and is affected by scaling, loss of substance, stains, etc. The results allow us to establish that, apart from the discontinuities in the mineralogical composition of the marble, the preferential orientation of the calcite crystals has an important effect on its anisotropic reaction. This preferential orientation is confirmed by textural studies using X-ray diffraction and determinations using a petrographic microscope equipped with universal stage. © 2008 Elsevier Ltd. All rights reserved.





