A combined synchrotron powder diffraction and vibrational study of the thermal treatment of palygorskite–indigo to produce Maya blue

The heating process (30–200 ºC) of a palygorskite- indigo mixture has been monitored in situ and simultaneously by synchrotron powder diffraction and Raman spectroscopy. During this process, the dye and the clay interact to form Maya blue (MB), a pigment highly resistant to degradation. It is shown...

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Detalles Bibliográficos
Autores: Sánchez del Río, Manuel, Boccaleri, Enrico, Milanesio, Marco, Croce, Gianluca, Beek, Wouter van, Tsiantos, Constantinos, Chyssikos, Georgios D., Gionis, Vassilis, Kacandes, Georges H., Súarez Barrios, Mercedes, García Romero, Emilia
Tipo de recurso: artículo
Fecha de publicación:2009
País:España
Institución:Universidad Complutense de Madrid (UCM)
Repositorio:Docta Complutense
Idioma:inglés
OAI Identifier:oai:docta.ucm.es:20.500.14352/49753
Acceso en línea:https://hdl.handle.net/20.500.14352/49753
Access Level:acceso abierto
Palabra clave:549.6
Palygorskite–indigo
Maya blue
Diffraction and Raman spectroscopy
Mineralogía (Geología)
2506.11 Mineralogía
Descripción
Sumario:The heating process (30–200 ºC) of a palygorskite- indigo mixture has been monitored in situ and simultaneously by synchrotron powder diffraction and Raman spectroscopy. During this process, the dye and the clay interact to form Maya blue (MB), a pigment highly resistant to degradation. It is shown that the formation of a very stable pigment occurs in the 70–130 ºC interval; i.e., when palygorskite starts to loose zeolitic water, and is accompanied by a reduction of the crystallographic a parameter, as well as by alterations in the C=C and C=O bonds of indigo. Mid- and near-infrared spectroscopic work and microporosity measurements, employed to study the rehydration process after the complex formation, provide evidence for the inhibition of the rehydration of MB as compared with palygorskite. These results are consistent with the blocking of the palygorskite tunnel entrance by indigo molecules with a possible partial penetration inside the tunnels. The surface silanols of palygorskite are not perturbed by indigo, suggesting that MB is not a surface complex.