Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-26T20:53:25.747Z Has data issue: false hasContentIssue false

The Role of Sepiolite-Palygorskite in the Decay of Ancient Egyptian Limestone Sculptures

Published online by Cambridge University Press:  28 February 2024

Carlos Rodriguez-Navarro
Affiliation:
The Getty Conservation Institute, 1200 Getty Center Drive, Suite 700, Los Angeles, California 90049
Eduardo Sebastian
Affiliation:
Dept. Mineralogia y Petrologia, Universidad de Granada, Fuente Nueva s/n, 18003 Granada, Spain
Eric Doehne
Affiliation:
The Getty Conservation Institute, 1200 Getty Center Drive, Suite 700, Los Angeles, California 90049
William S. Ginell
Affiliation:
The Getty Conservation Institute, 1200 Getty Center Drive, Suite 700, Los Angeles, California 90049
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.

An ancient Egyptian limestone sculpture was found to be undergoing major structural decay when stored in a museum environment. Mineralogical and petrographic analysis of the limestone showed a high proportion of clay (≥ 10% by weight) that was concentrated along bedding planes. The clay fraction consisted mostly of sepiolite (>90%) and palygorskite (<10%). Minor quantities (≤l%) of soluble salts (NaCl and NaNO3) were also found. Wetting/drying with distilled water and relative humidity cycling resulted in the same delamination cracking damage as that observed in the museum environment. Thermomechanical analyses (TMA) confirmed that the damage was due to expansion (>4.5%) parallel to bedding planes when the limestone was immersed in water. The expansion due to swelling of the clays was directly observed at high magnification in an environmental scanning electron microscope (ESEM) when wetting/drying cycles were performed. X-ray diffraction (XRD) analysis showed that crystalline swelling of sepiolite occurred. This was determined by a shift of (110) reflection (from 12.07 to 12.20 Å) and a decrease of (060) reflection (4.47 Å, to 4.44 and 4.41 Å), when in contact with ethylene glycol (EG) and dimethyl sulfoxide (DMSO), respectively. Swelling also occurred due to hydration of the clay surfaces and to electrostatic forces between clay particles, which, it was assumed, was promoted by the presence of Na counterions in water solution. Possible treatments for the conservation of these artistic objects are proposed and discussed.

Type
Research Article
Copyright
Copyright © 1998, The Clay Minerals Society

References

Amer, A.F. Krintsov, M.I. and Hanna, F.L., 1970 The Egyptian carbonate rocks and the possibilities of their utilisation Studies of some mineral deposits of Egypt Riad, United Arab Republic Ministry of Industry Geol Survey 195208.Google Scholar
Arnold, A., 1981 Nature of reactions of saline minerals in walls. In: Rossi-Manaresi R Preprints of the contributions to the International Symposium on the Conservation of Stone II Bologna Centra Conservazione Sculture All’aperto 1323.Google Scholar
Bradley, S.M. and Middleton, A.P., 1988 A study of the deterioration of Egyptian limestone sculpture J Am Institute for Conservation 27 2768 10.2307/3179403.CrossRefGoogle Scholar
Brattli, B. and Broch, E., 1995 Stability problems in water tunnels caused by expandable minerals. Swelling pressure measurements and mineralogical analysis Engin Geol 39 39169 10.1016/0013-7952(95)00009-5.CrossRefGoogle Scholar
Brauner, K. and Preisinger, A., 1956 Struktur und Enstehung des Sepioliths Tschermaks Miner Petrog Mitt 6 6140 10.1007/BF01128033.CrossRefGoogle Scholar
Caner, E.N. and Seeley, N.J., 1978 The clay minerals and the decay of limestone UNESCO/RILEM Symp Deterioration and Protection of Stone Monuments 2 5 3.Google Scholar
Charola, A.E. Wheeler, G.E. Koestler, R.J., Gauri, K.L. and Gwinn, J.A., 1982 Treatment of the Abydos Reliefs: Preliminary investigations Proc 4th Int Cong Deterioration and Preservation of Stone Objects Louisville Univ of Louisville 7788.Google Scholar
Chatterji, S. Christensen, P. and Overgaard, G., 1979 Mechanisms of breakdown of natural stones caused by sodium salts Proc 3rd Int Cong on the Deterioration and Preservation of Stones Padova Instituto di Chimica Industriale, Universita’degli Studi di Padova 131134.Google Scholar
Dunn, J.R. and Hudec, P.P., 1966 Water, clay and rock soundness The Ohio J Sci 66 153168.Google Scholar
Fleischer, P., 1972 Sepiolite associated with Miocene diatomite, Santa Cruz basin, California Am Mineral 57 903913.Google Scholar
Guven, N. and Carney, L.L., 1979 The hydrothermal transformation of sepiolite to stevensite and the effect of added chlorides and hydroxides Clays Clay Miner 27 27260 10.1346/CCMN.1979.0270403.CrossRefGoogle Scholar
Hanna, S.B., Brommelle, N.S. Pye, E.M. Smith, P. and Thomson, G., 1984 The use of organo-silanes for the treatment of limestone in an advanced state of deterioration Preprints Contrib Paris Cong on Adhesives and Consolidants Paris Int Inst for Conservation 171176.Google Scholar
Helms, G.M., 1977 Conservation of Egyptian limestone: The Abydos Reliefs 3rd Annual Art Conservation Training Programmes Conf Kingston Queen’s Univ 4050.Google Scholar
Jeffers, J.D. and Reynolds, R.C. Jr., 1987 Expandable palygorskite from Cretaceous-Tertiary boundary, Mangyshlak Peninsula, USSR Clays Clay Miner 35 473476 10.1346/CCMN.1987.0350609.CrossRefGoogle Scholar
Jones, B.F. Galan, E. and Bailey, S.W., 1988 Sepiolite and palygorskite Hydrous phyllosilicates. Rev Mineral 18 Washington, DC Mineral Soc Am. 631674 10.1515/9781501508998-021.CrossRefGoogle Scholar
Kowalski, W.C., 1975 The influence of changes of water content on mechanical strength and deformability of rocks in the weathering zone Bull Int Assoc Eng Geology 12 12 43.Google Scholar
Kuhnel, R.A. van der Gaast, S.J. Brych, J. Laan, G.J. and Kulnig, H., 1994 The role of clay minerals in durability of rocks: Observation on basaltic rocks Applied Clay Sci 9 9237 10.1016/0169-1317(94)90001-9.CrossRefGoogle Scholar
Laird, D.A., 1996 Model for crystalline swelling of 2:1 phyllosilicates Clays Clay Miner 44 44559 10.1346/CCMN.1996.0440415.CrossRefGoogle Scholar
Low, P.F., Schulz, L.G. van Olphen, H. and Mumpton, F.A., 1987 The clay-water interface Proc Int Clay Conf Denver, CO. Bloomington, IN Clay Miner Soc. 247256.Google Scholar
MacEwan, D.M.C. Wilson, M.J., Brindley, G.W. and Brown, G., 1980 Interlayer and intercalation complexes of clay minerals Crystal structure of clay minerals and their X-ray identification London Mineral Soc. 197248.CrossRefGoogle Scholar
Martin-Patino, M.T. Madruga, F. and Saavedra, J., 1993 The internal structure of the Villamayor sandstone as it affects its use as a construction material Applied Clay Sci 8 877 10.1016/0169-1317(93)90026-W.CrossRefGoogle Scholar
McGreevy, J.P. and Smith, B.J., 1984 The possible role of clay minerals in salt weathering Catena 11 11175 10.1016/S0341-8162(84)80016-8.CrossRefGoogle Scholar
Messier, P. and Vitale, T., 1993 Cracking in albumen photographs: An ESEM investigation Microscopy Res Tech 25 25383 10.1002/jemt.1070250505.CrossRefGoogle ScholarPubMed
Middleton, A.P. and Bradley, S.M., 1989 Provenancing of Egyptian limestone sculpture J Archeological Sci 16 16488 10.1016/0305-4403(89)90069-1.CrossRefGoogle Scholar
Miller, E., 1992 Current practice at the British Museum for the consolidation of decayed porous stones The Conservator 16 1683 10.1080/01400096.1992.9635629.CrossRefGoogle Scholar
Newman, A.C.D. and Newman, A.C.D., 1987 The interaction of water with clay mineral surfaces Chemistry of clays and clay minerals New York J. Wiley 237274.Google Scholar
Norrish, K., 1954 The swelling of montmorillonite Discussions Far Soc 18 18135.Google Scholar
Oddy, W.A. Hughes, M.W. and Baker, S., 1976 The washing of limestone sculptures from Egypt and the Middle East Lithoclastia 2 210.Google Scholar
Permien, T. and Lagaly, G., 1995 The Theological and colloidal properties of bentonite dispersions in the presence of organic compounds. V. Bentonite and sodium montmorillonite and surfactants Clays Clay Miner 43 43236 10.1346/CCMN.1995.0430210.CrossRefGoogle Scholar
Price, C. Brimblecombe, P., Roy, A. and Smith, P., 1994 Preventing salt damage in porous materials Preprints Contrib Ottawa Congress on Preventive Conservation Practice Theory and Research Ottawa Int Inst of Conservation 9093.Google Scholar
Prost, R. and Bailey, S.W., 1976 Interactions between adsorbed water molecules and the structure of clay minerals: Hydration mechanism of smectites Proc Int Clay Conf Wilmette, II Applied Publ 351359.Google Scholar
Rodriguez-Navarro, C. Sebastian, E. Ginell, W.S., Ortega-Huertas, M. López-Galindo, A. and Palomo-Delgado, I., 1996 ESEM analysis of swelling process in sepiolite-bearing Egyptian limestone sculptures Advances in clay minerals Granada Univ de Granada 301303.Google Scholar
Ruiz, V.G. Calleja, L S d and Rio, L.M., 1995 Acoustic emission during swelling and contraction tests Eng Geol 39 39150.Google Scholar
Rutherford, J.B., 1988 Geotechnical causes of ancient tomb damage: Valley of the Kings, Egypt Proc Symp on Geotechnical Aspect of Restoration and Maintenance of Infra-structures and Historical Monuments Bangkok Asian Inst of Technology 305324.Google Scholar
Said, R., 1962 The geology of Egypt New York Elsevier.Google Scholar
Said, R. 1990. The geology of Egypt. Said, R., editor. Rotterdam: Balkema Publ. 734 p.Google Scholar
Shidharan, A. and Satyamurty, P.V., 1996 Potential-distance relationships of clay-water systems considering the Stern theory Clays Clay Miner 44 44484.Google Scholar
van Olphen, H., 1977 An introduction to clay colloid chemistry 2nd edition New York J. Wiley.Google Scholar
van Olphen, H. and Newman, A.C.D., 1987 Dispersion and flocculation Chemistry of clays and clay minerals London J. Wiley 203224.Google Scholar
Watts, N.L., 1976 Paleopedogenic palygorskite from the basal Permo-Triassic of northwest Scotland Am Mineral 61 61302.Google Scholar
Weaver, C.E., 1989 Clays, muds, and shales Amsterdam Elsevier.Google Scholar
Wendler, E. Klemm, D.D. and Snethlage, R., 1991 Contour scale on building facades: Dependence on stone type and environmental conditions Mat Res Soc Symp Proc 185 185271.Google Scholar
Wendler, E. Charola, A.E. Fitzner, B. and Riederer, J., 1996 Easter Island tuff: Laboratory studies for its consolidation Proc 8th Int Cong Deterioration and Conservation of Stone Berlin Moller Druck und Verlag Gmbh. 11591170.Google Scholar
Wiersma, J., 1970 Provenance, genesis and paleo-geographical implication of macrominerals occurring in sedimentary rocks of Jordan Valley Area Amsterdam Publ Fys Geogr Bodenk Lab Univ..Google Scholar
Yatsu, E., 1988 The nature of weathering: An introduction Tokyo Sozosha.Google Scholar