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Ancient ceramic analysis by neutron activation in association with multivariate methods

Abstract

We report a comparative study of two archaeological sites, Bela Vista and Serrano, located in the Araruama region of the state of Rio de Janeiro, in Brazil. The elemental geochemical compositions of the ceramics from both sites were determined by Instrumental Neutron Activation Analysis (INAA). A statistical treatment of the data, using cluster analysis and principal component analysis, indicates that there are no correlations between these sites.


APPLIED PHYSICS AND INSTRUMENTATION

Ancient ceramic analysis by neutron activation in association with multivariate methods

U. M. Vinagre FilhoI; R. M. LatiniII; A V. B. BellidoII; A. BuarqueIII; A. M. BorgesII

IInstituto de Engenharia Nuclear - IEN-CNEN. Cid. Univ., Ilha do Fundão Caixa Postal 68550, 21945-970, Rio de Janeiro, RJ, Brazil

IIUniversidade Federal Fluminense, IQ-UFF. Outeiro São João Batista, sn. Valonguinho, 24020-150, Niterói, RJ, Brazil

IIIMuseu Nacional - Depto. de Antropologia-UFRJ. Quinta da Boa Vista, São Cristovão, 20940-040, Rio de Janeiro, RJ, Brazil

ABSTRACT

We report a comparative study of two archaeological sites, Bela Vista and Serrano, located in the Araruama region of the state of Rio de Janeiro, in Brazil. The elemental geochemical compositions of the ceramics from both sites were determined by Instrumental Neutron Activation Analysis (INAA). A statistical treatment of the data, using cluster analysis and principal component analysis, indicates that there are no correlations between these sites.

I. INTRODUCTION

The presence of ceramic sherds is always observed at the latest levels of the Sambaqui occupation in Rio de Janeiro, which were identified as belonging to the Una and Tupinambá archaeological groups [1,2]. In Brazilian archaeology it is interesting to investigate the contacts and relationship among horticulture, ceramics and fishermen, and hunter-gathering groups (FHG; Sambaquieiros) [1].

The disappearance of these FHG groups in some regions may has been associated with the arrival of new ceramic groups. In this investigation, we use analytical tools in order to identify and characterize collected ceramics fragments from the archaeological sites in the Araruama region. Ceramic objects are made from clays and often mixed with tempers , which may be organic materials, sand, ceramic powder, shells, or other types of clays [3]. From a mineralogical point of view, a clay species and its respective chemical composition can show variations due to different geological conditions of formation and to the degree of isomorphic substitutions or exchanges by similarity and exchangeable cations. Therefore, the determination of the chemical composition of a particular sherd gives an indication of the specific clay source [4]. The characterization of the elemental chemical composition of the ceramic samples was done by using the nuclear technique of instrumental neutron activation analysis (INAA) [5,6,7,8]. For classification studies, the data were treated by two multivariate statistical methods, cluster analysis and principal component analysis.

II. ARCHAEOLOGICAL SITES

The ceramic materials used in this study were collected at the Condomínio Bela Vista and Serrano Archaeological Sites. Figure1 shows the intense Tupinambá occupation in this region. Polychromic ceramics with geometric decoration were mainly used for funerary and ornamental ware. Another archaeological study in the region, checking the elemental chemical composition, shows differentiation between domestic (cooking), ornamental, and funerary wares [9].


III. INSTRUMENTAL NEUTRON ACTIVATION ANALYSIS

We analyzed 18 collected ceramic fragments. The clay standard reference material was the Podmore Red Clay, which has an elemental concentration very close to our analyzed samples [6]. Approximately 200 mg of representative ceramic fragments and standards were weighted and encapsulated in an appropriate polyethylene container for irradiation. In order to keep the same counting geometry, and to achieve the best results, we used approximately the same weight for samples and standards. The samples were irradiated at the IEA-R1 research reactor of the Instituto de Pesquisas Energéticas e Nucleares (IPEN). The thermal neutron flux was of the order of 1012n.cm-2s-1. The irradiation time was in accordance with the half life of the measured radionuclides. The detection and measuring system consisted of a HPGe detector, a 4096 multichannel analyzer, an amplifier, as well as an associated electronic Ortec and Canberra, with 1,9 keV resolution to g-ray 1332,501 keV 60Co. We have used the technique of gamma-ray spectrometry and the computer code GRGAN [10] for data reduction. Special attention was given to choosing the photopeaks, i.e. ensuring that they were free from interference. The elements determined were Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, Lu, Mn, Na, Rb, Sb, Sc, Sm Ta, Th, Ti, U, and V

IV. STATISTICAL TREATMENT OF THE ANALYTICAL DATA

The elemental concentrations obtained from INAA were used as variables in the statistical treatment. We used the SPSS packet [11], cluster analysis, and principal components analysis [12]. Initially, the data were normalized using "z-scores," a transformation that generated new variables with zero average and standard deviation equal to one. In the cluster analysis, we used the square Euclidean distance as a measure in n-dimensional space, and the hierarchical means in the Ward subroutine (minimum variance). As a result of the cluster analysis, the samples were divided into two groups, the Bela Vista group and the Serrano group, determined from the chemical composition of these groups (Figure2: dendogram).


The characterization of these groups was made by the average and standard deviation of each one of the studied elements (Table I)

The groups were then analyzed in order to search for evidences of correlations between variables. The principal component analysis (PCA) was used to identify the significant elements that contributed to each cluster. The cluster analysis output is due to differentiated internal correlations. For the Bela Vista group, the chemical elements in factor 1 (PCA 1) are Dy, Ta, Yb, Co, and Fe; in factor 2 (PCA 2), they are La and Eu (Figure 3). For the Serrano group, the chemical elements in factor 1 (PCA 1) are Mn, Rb, Na, and Ce; in factor 2 (PCA 2), they are are Sm and Dy (Figure 4).



V. CONCLUSION

The results obtained to date indicate clear differences in chemical composition of fragments from these two archeological sites. On the basis of the ceramic composition, it is suggested that the ceramic objects were made from different kinds of clay or using different methods of fabrication.

VI. ACKNOWLEDGMENTS

Thanks are due to Dr. M. Vasconcellos, Dra. M. Saiki and the Radiochemistry Group at IPEN for the NAA support.

VII. REFERENCES

11. SPSS Inc. 444, North Michigan Ave. Chicago IL, 60611.

12. A. V. B. Bellido, M. R. Chandratillake, and V. I. Robinson, Cluster Analysis in Ceramic Provenance Studies: Methods for Dealing with Elemental Correlations (in preparation).

Received on 23 January, 2005

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  • 9. R. M. Latini, A. V. B. Bellido Jr., and A. Buarque, Estudos de classificaçăo e dataçăo de cerâmicas arqueológicas do Estado do Rio de Janeiro, V Congresso de Geoquímica dos Países de Língua Portuguesa and VII Congresso Brasileiro de Geoquímica, 333-335, 1999.
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Publication Dates

  • Publication in this collection
    07 Nov 2005
  • Date of issue
    Sept 2005

History

  • Received
    23 Jan 2005
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