Hostname: page-component-586b7cd67f-t7czq Total loading time: 0 Render date: 2024-11-22T18:17:22.186Z Has data issue: false hasContentIssue false

Structural Study of Maya Blue: Textural, Thermal and Solid-State Multinuclear Magnetic Resonance Characterization of the Palygorskite-Indigo and Sepiolite-Indigo Adducts

Published online by Cambridge University Press:  01 January 2024

Basil Hubbard
Affiliation:
Center for Catalysis Research and Innovation, Department of Chemistry, University of Ottawa, Ottawa, Ontario, Canada K1N 6N5
Wenxing Kuang
Affiliation:
Center for Catalysis Research and Innovation, Department of Chemistry, University of Ottawa, Ottawa, Ontario, Canada K1N 6N5
Arvin Moser
Affiliation:
Center for Catalysis Research and Innovation, Department of Chemistry, University of Ottawa, Ottawa, Ontario, Canada K1N 6N5
Glenn A. Facey
Affiliation:
Center for Catalysis Research and Innovation, Department of Chemistry, University of Ottawa, Ottawa, Ontario, Canada K1N 6N5
Christian Detellier*
Affiliation:
Center for Catalysis Research and Innovation, Department of Chemistry, University of Ottawa, Ottawa, Ontario, Canada K1N 6N5
*
*E-mail address of corresponding author: [email protected]
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Palygorskite-indigo and sepiolite-indigo adducts (2 wt.% indigo) were prepared by crushing the two compounds together in a mortar and heating the resulting mixtures at 150 and 120°C, respectively, for 20 h. The samples were tested chemically to ensure that they displayed the characteristic properties of Maya Blue. Textural analysis revealed that no apparent changes in microporosity occurred in sepiolite or palygorskite after thermal treatment at 120°C (sepiolite) and 150°C (palygorskite) for 20 h. Micropore measurements showed a loss of microporosity in both sepiolite and palygorskite after reaction with indigo. The TGA-DTG curves of the sepiolite-indigo and palygorskite-indigo adducts were similar to their pure clay mineral counterparts except for an additional weight loss at ∼360°C due to indigo.

The 29Si CP/MAS-NMR spectrum of the heated sepiolite-indigo adduct is very reminiscent of the spectrum of dehydrated sepiolite. Crushing indigo and sepiolite together initiates a complexation, clearly seen in the 13C CP/MAS-NMR spectrum, which can be driven to completion by heat application. In contrast to the broad peaks of the pure indigo 13C CP/MAS-NMR spectrum, the sepiolite-indigo adduct spectrum consists of a well-defined series of six narrow peaks in the 120.0–125.0 ppm range. In addition, the sepiolite-indigo spectrum has two narrow, shifted peaks corresponding to the carbonyl group and the C-7 (C-16) of indigo. A model is proposed in which indigo molecules are rigidly fixed to the clay mineral surface through hydrogen bonds with edge silanol groups, and these molecules act to block the nano-tunnel entrances.

Type
Research Article
Copyright
Copyright © 2003, The Clay Minerals Society

References

Ahlrichs, J.L. Serna, C. and Serratosa, J.M., (1975) Structural hydroxyls in sepiolite Clays and Clay Minerals 23 119124 10.1346/CCMN.1975.0230207.Google Scholar
Brindley, G.W., (1959) X-ray and electron diffraction data for sepiolite American Mineralogist 44 495 500.Google Scholar
Cooksey, C.J. and Dronsfield, A.T., (2002) Adolf von Baeyer and the indigo molecule Dyes in History and Archaeology 18 13 19.Google Scholar
Gettens, R.J., (1962) Maya blue: an unsolved problem in ancient pigments American Antiquity 27 557564 10.2307/277679.Google Scholar
Gettens, R.J. and Stout, G.L., (1946) Painting Materials: A Short Encyclopedia New York D. Van Nostrand 130 131.Google Scholar
Gordon, P.F. and Gregory, P., (1983) Indigoid Dyes Organic Chemistry in Colour Berlin Springer-Verlag 208 211.Google Scholar
Gribova, E.A., (1955) X-ray study of indigo and thioindigo L. Ya Karpov Physical Chemistry Institute: Doklady Akademii Nauk SSSR 102 279 81.Google Scholar
Horvath, G. and Kawazoe, K., (1983) Method for the calculation of effective pore size distribution in molecular sieve carbon Journal of Chemical Engineering of Japan 16 470475 10.1252/jcej.16.470.Google Scholar
Jones, B.F. Galán, E. and Bailey, S.W., (1998) Sepiolite and palygorskite Hydrous Phyllosilicates Washington, D.C Mineralogical Society of America 631 674.Google Scholar
Jose-Yacaman, M. Rendon, L. Arenas, J. and Puche, M.C.S., (1996) Maya blue paint: an ancient nanostructured material Science 273 223225 10.1126/science.273.5272.223.CrossRefGoogle ScholarPubMed
Kleber, R. Masschelein-Kleiner, L. and Thissen, J., (1967) Study and identification of Maya blue Studies in Conservation 12 4156 10.1179/sic.1967.s005.Google Scholar
Kuang, W., Hubbard, B., Moser, A., Facey, G.A. and Detellier, C. (2002) Organo-sepiolite and palygorskite nanocomposites. Proceedings of the 5 th International Conference on Solid State Chemistry, Bratislava, Slovak Republic.Google Scholar
Le Van Mao, R. Rutinduka, E. Detellier, C. Gougay, P. Hascoet, V. Tavakoliyan, S. Hoa, S.V. and Matsuura, T., (1999) Mechanical and pore characteristics of zeolite composite membranes Journal of Materials Chemistry 9 783788 10.1039/a806624h.Google Scholar
Merwin, H.E. (1931) In: The Temple of the Warriors at Chichen Itza (Morris, E.H., Charlot, J. and Morris, A.A., editors). Carnegie Institution of Washington, Washington, D.C., publ. 406.Google Scholar
Myriam, M. Suarez, M. and Martin-Pozas, J.M., (1998) Structural and textural modifications of palygorskite and sepiolite under acid treatment Clays and Clay Minerals 46 225231 10.1346/CCMN.1998.0460301.Google Scholar
Pedro, G., (1972) Report of the AIPEA Nomenclature Committee AIPEA Newsletter 4 3 4.Google Scholar
Polette, L.A. Meitzner, G. Jose-Yacaman, M. and Chianelli, R.R., (2002) Maya blue: application of XAS and HRTEM to materials science in art and archaeology Microchemical Journal 71 167174 10.1016/S0026-265X(02)00008-5.CrossRefGoogle Scholar
Ruiz-Hitzky, E., (2001) Molecular access to intracrystalline tunnels of sepiolite Journal of Materials Chemistry 11 8691 10.1039/b003197f.Google Scholar
Serna, C. and van Scoyoc, G.E. (1979) Infrared study of sepiolite and palygorskite surfaces. Pp. 197206 in: Proceedings of the International Clay Conference, Oxford, 1978 (Mortland, M.M. and Farmer, V.C., editors). Elsevier, Amsterdam.Google Scholar
Shepard, A., (1962) Maya blue: alternative hypotheses American Antiquity 27 565566 10.2307/277680.Google Scholar
Tagle, A. Paschinger, H. Richard, H. and Infante, G., (1990) Maya blue: its presence in Cuban colonial wall paintings Studies in Conservation 35 156 159.Google Scholar
Van Olphen, H., (1966) Maya Blue: a clay mineral-organic pigment? Science 154 645646 10.1126/science.154.3749.645.CrossRefGoogle Scholar
Wang, Q.K. Matsuura, T. Feng, C.Y. Weir, M.R. Detellier, C. Rutinduka, E. and Le Van Mao, R., (2001) The sepiolite membrane for ultrafiltration Journal of Membrane Science 184 153163 10.1016/S0376-7388(00)00605-0.Google Scholar
Weir, M.R. Facey, G.A. and Detellier, C., (2000) 1H, 2H and 29Si solid state NMR study of guest acetone molecules occupying the zeolitic channels of partially dehydrated sepiolite clay Studies in Surface Science and Catalysis 129 551558 10.1016/S0167-2991(00)80257-8.Google Scholar
Weir, M.R. Rutinduka, E. Detellier, C. Feng, C.Y. Wang, Q. Matsuura, T. and Le Van Mao, R., (2001) Fabrication, characterization and preliminary testing of all-inorganic ultrafiltration membranes composed entirely of a naturally occurring sepiolite clay mineral Journal of Membrane Science 182 4150 10.1016/S0376-7388(00)00547-0.Google Scholar
Weir, M.R. Kuang, W. Facey, G.A. and Detellier, C., (2002) Solid state nuclear magnetic resonance study of sepiolite and partially dehydrated sepiolite Clays and Clay Minerals 50 240247 10.1346/000986002760832838.Google Scholar