Abstract

Maya blue, an ancient pigment used by Mayas in Mesoamerica, can be considered an ancestor of modern nano-composites as it forms by grinding and heating the guest indigo molecule with a hosting clay framework (palygorskite or sepiolite). specific bonds form between the guest dye and the hosting matrix, conferring the pigment an exceptional stability to both acid and alkali attacks. While most works have been focused on the study of the palygorskite/indigo complex, this project is aimed to unveil the structural features of Maya blue when sepiolite is the hosting framework. a freshly-synthesized sepiolite-based Maya blue was prepared accordingly to ancient Mayas recipes and investigated with various spectroscopic techniques (uv-visible, FtiR, Raman). all evidences show that by strongly crushing and heating (190°C in air or 150°C in vacuum) the sepiolite + indigo (2 wt%) composite, the dye aggregates dissociate to monomers favouring diffusion inside the clay tunnels emptied from loosely bound zeolitic H2o. once encapsulated indigo partly decomposes to dehydroindigo, its oxidized form, whose flexible molecule can easily diffuse inside the tunnels slightly changing the pigment colour (from deep blue to blue/green). applied heating, however, does not cause loss of Mg-coordinated oH2 which forms H-bonds with the indigo reactive groups (C=o and n–H) after encapsulation, thus stabilizing the composite. spectroscopic evidences supporting presence of H-bonds are less evident in sepiolite-based rather than in palygorskite-based composites with indigo. in fact while indigo is perfectly juxtaposed in the narrower tunnels of palygorskite (6.4 x 3.7 A), receiving H-bonds on both sides of the molecule, in the wider tunnels of sepiolite (10.6 x 3.7 A) its molecule has to get near to one border in order to form a single bond. in a sepiolite-based Maya blue pigment the global number of possible host/guest interactions is therefore dramatically halved with respect to a palygorskite-based one, inevitably reducing resistance to chemical attacks. Consequently, the extent of Maya blue renowned stability is directly related to the composition of its main clay constituents. Riassunto il blu Maya, un antico pigmento utilizzato dai Maya nell’america centrale, puo essere considerato un antesignano dei moderni composti d’inclusione, prodotto della macinazione e riscaldamento dell’indaco con un minerale argilloso (palygorskite o sepiolite). specifici legami si formano tra la molecola ospite e la matrice ospitante, conferendo al pigmento un’eccezionale stabilita chimica nei confronti di attacchi acidi e basici. dal momento che la maggior parte dei lavori sin qui pubblicati e stata incentrata sullo studio del complesso palygorskite/indaco, il presente progetto e stato finalizzato alla PerIodIco di MIneralogIa established in 1930 Period. Mineral. (2010), Special Issue, 21-37 doi: 10.2451/2010PM0019 http://go.to/permin An International Journal of MINERALOGY, CRYSTALLOGRAPHY, GEOCHEMISTRY, ORE DEPOSITS, PETROLOGY, VOLCANOLOGY and applied topics on Environment, Archeometry and Cultural Heritage Spectroscopic characterization of a sepiolite-based Maya Blue pigment RobERto GiustEtto*1, Kalaivani sEEnivasan2 and silvia boRdiGa2 1department of Mineralogical and Petrologic sciences and nis Centre of Excellence, universita degli studi di torino via valperga Caluso 35, 10125 torino (italy), 2department of inorganic, Physical and Materials Chemistry, instM Centro di Riferimento and nis Centre of Excellence, universita di torino, via Quarello 11, 10135 torino, italy Submitted, September 2010 Accepted, November 2010 *Corresponding author, E-mail: roberto.giustetto@unito.it giustetto:periodico 30/11/2010 15:23 Pagina 21

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call