Application of XAFS in Archaeology I. Nakai, M. Matsunaga, M. Adachi, K.-I. Hidaka To cite this version: I. Nakai, M. Matsunaga, M. Adachi, K.-I. Hidaka. Application of XAFS in Archaeology. Journal de Physique IV Colloque, 1997, 7 (C2), pp.C3-1033-C3-1034. <10.1051/jp4:19972131>. <jpa-00255192> HAL Id: jpa-00255192 https://hal.archives-ouvertes.fr/jpa-00255192 Submitted on 1 Jan 1997 HAL is a multi-disciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés. L PPHrS IV FRANCE 7 (1997) Colloque C2, Suppltment au Journal de Physique I11 d'avril 1997 Application of XAFS in Archaeology I. Nakai, M. Matsunaga, M. Adachi and K.-I. Hidaka* Department of Applied Chemistry, Faculty of Science, Science University of Tokyo,Kagurazaka, Shinjuku, Tokyo 162, Japan * University of Tsukuba, Tsukuba, Ibaraki 305, Japan Abstract. X-ray fluorescence XAFS technique was successfully applied to the archaeological study to find colorant elements in old glass samples and to characterize the chemical states of iron in the ceramic sherds excavated from an archaeological site in Turkey. The origin of red color of the mosaic glass is found to be due to the colloidal copper particles in the glass. Blue color is attributed to divalent cobalt. Fe K-XANES spectra revealed that the color of the sherds changes from black, gray, brown, to orange with increasing the absorption edge energy. The gray ceramics typical for Phrygia age were produced in a reducing condition. The creatn color of the central Anatolian Iron Age could not be related with the oxidation state of iron. 1. Introduction Various colors in glasses are caused by metal ions in them [l]. They are usually elements belonging to the transition rows of the periodic system, which absorb characteristic frequencies of visible region as a result of the d-d electronic transitions. Similarly, iron is a key element to understanding the color of various types of pottery. Since this kind of information is important in understanding the manufacturing technique of glass wares and potteries, we have investigated ancient colored glasses from middle east and pottery sherds excavated from archaeological site of Kamall Kalehoyiik, Turkey by using XAFS technique. This is the first report of the archaeological application of this technique to ancient pottery analysis. 2. Experimental Samples used are mosaic glasses from Dome of Hagia Sophia build in 537 in Istanbul, Turkey and ceramic sherds from Kaman Kalelioyiik, Turkey [2]. These sherds were produced by Hittite and Phrygian civilizations. The colors of the sherds are red, gray, yellow, cream and black. X-ray absorption spectra were measured at Photon Factory (PF) in the National Institute of High Energy Physics, Tsukuba, Japan with a S i ( l l 1 ) double crystal monochromator. Two dimensional chemical state analysis of iron in the ceramic sherds was carried out at BL4A using Si(Li) S.S.D. as a detector and small X-ray beam (width 800km and height 400 +m ). EXAFS data were obtained at BL-6B using a fluorescent X-ray detector [3]. The K-edge spectra of the glass samples were measured in this mode. Reference spectra of standard compounds and minerals were also measured at BL-4A and BL-6B. The edge energy is defined by a half maximum value of the white line peak of each XANES spectrum. 3. Results a n d Discuseion Figure 1 shows Cu K-edge XANES spectra of the colored glasses and reference materials after having been normalized to the height of the edge jump. Radial structure functions of their EXAFS~oscillationobtained from the Fourier transforms of k3X(k)are given in Fig 2. A comparison of the spectrum of the red mosaic glass (Fig. l (b)) with that of the Cu metal (Fig.l(a)) indicates that Cu in the mosaic glass exists as copper metal. This finding is supported by the corresponding radial structure functions given in Figs. 2(a) and (b). It is well known hypothesis that colloidal particles of metallic copper is the origin of the red color in the copper red glass [l]. Figures 1 (d) and (f) are XANES spectra of a green mosaic glass and a green Egyptian glass and their FTs are given in Figs. 2 (d) and (f), respectively. The results indicate that oxidation state of copper in the mosaic glass is monovalent while it is divalent in the Egyptian glass. The Cu+ is d" ion and is not responsible for the green color which is the color of divalent copper (cf. (e) and (f)). Therefore, the origin of the green color in the mosaic glass could be ascribed to another ion. Similarly, it was found that c o 2 +was responsible for the blue color of the mosaic glass and Egyptian glass. Figure 3 is a summary of the results for the shreds analysis which shows a correlation of the color of the sherds and Fe K-edge energy. The difference in the analyzed spot in a sherd, i.e. surface or inside accounts for the diversity of the data. The color of the ceramic sherds changes from black, gray. brown to orange with increasing the edge energy. When we compare the edge energy of the reference samples with that of the sherds, it is found that the black sample gives the lowest energy close to that of the magnetite region, and similarly, gray to silicates containing both ferrous and ferric ions, reddish brown to hematite and orange to ferric silicate minerals. Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jp4:19972131 JOURNAL DE PHYSIQUE IV C2-1034 (a) Cu metal ... -( a ) Cu metal ( b ) red mosaic glass - - (C) Cu20 . .. ... (d)green - (b) red mosaic glass -( c ) c u 2 0 mosaic glass ... -(e)CuO . (d)ereett mosaic gloss (e)CuO (t) Egyptian green .... ( 0 Egyptian green glass glass P\ keV Figure 1: Cu K-edge XANES spectra of glass samples Figure 2: Fourier transforms of the k' x (k) of glass samples Two dimensional chemical state analysis of a section (Fig. 4(a) ) of so called "golden mica slip ware." (dated Phrygian age) was carried out and XANES spectra measured at points A: B, C and D in Fig. 4(a) were given in Fig. 4(b). The colors of the points A and D are pale orange while it is gray at point C. It can be seen from Fig 4(b) that the spectra shift to higher energy from C to A indicating that iron at the surface is more oxidized than that in the inside. From these observation it is possible to deduce that this pottery was fired once in reducing condition then under oxidizing condition in a kiln. Our analysis showed that the gray ceramics typical for Phrygia age were produced in reducing conditions. The cream color of the central Anatorian Iron Age creamware could not be related with the oxidation state of iron. The information derived from the Fe K-XANES spectra of pottery sherds is the electronic structure of iron in them, which is determined by mineral sources, their relative composition and the thermal history of each clay received during firing conditions, which may differ from kiln to kiln. In concIusion, present study indicated that XAFS spectroscopy offers many advantages over conventional chemical speciation techniques such as Mossbauer spectroscopy and XPS. XAFS allows us to carry out two dimensional chemical state analysis, whose spatial resolution is determined by the beam size; e.g., with a focusing optics we can currently obtain microbearn of a few pm order at BL-4A. Since the excitation source is hard X-rays, the method is truly nondestructive analysis that can be done in air. These characteristics are particularly important in archaeological application in which samples are precious cultural heritage. XAFS requires no special vacuum chamber like XPS and no restriction in sample sizes and their materials, i.e. they may be metals, ceramics, cloths, glasses, etc. Moreover, XAFS technique is applicable to most of the elements with atomic number, practically. greater than 13(=A1), whereas Mossbauer spectroscopy is limited to a small number of elements. References [ l ] Doremus R.H., Glass Science (John Wiley & Sons, New York, 1973)pp.327-330. [2] Mori M.,Omura S. Bull. Middle E a s t e r Culture Cerrter Jnpnw, 8 (1995) 1-55. [3] Lytle F.W., Greegor R.B., andstrom D.R.,Marques E.C., Wong J.. Spiro C.L., Huffman G.P.Hugins F.E..A'ucuc[. Instr. (1984)542-548. orange buff light bmwn brown &dish brown darkbrown yellowish cgray light hlack light gray d& hlack r hlack silicatd~C.~?) magnetite ... Meth. 226 .. ---S -. -. ..... .. - .. -..- . .. .- pyrite .Fe mnal energy (eV) Figure 3. Fe K-edge energy of ceramic sherds and their colors energy(keV) Figure 1:Two dimensional XANES analyses of a ceramic sherd. (a) sample section, (b) Fe K-edge XANES spectra
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