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xxiii πανελληνιο συνεδριο φυσικης στερεας καταστασης & επιστημης ...

xxiii πανελληνιο συνεδριο φυσικης στερεας καταστασης & επιστημης ...

xxiii πανελληνιο συνεδριο φυσικης στερεας καταστασης & επιστημης ...

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Simulating the neutron diffraction profiles of the mineralogical variations during firing<br />

in ancient ceramics<br />

I.M.Siouris 1 , V.Moumtzi 2 ,F.Moumtzis 2 ,, W. Kockelmann 3<br />

1<br />

Department of Production and Management Engineering , Democritus University of Thrace<br />

Xanthi, 67 1 00 Xanthis, Greece<br />

2 Altec SA, Research Programmes Division, 56429 Thessalonica, Greece<br />

3 Rutherford Appleton Laboratory, ISIS Facility, OX11 0QX Chilton, United Kingdom<br />

*jsiou@pme.duth.gr<br />

The possibility to perform quantitative phase analysis on intact archaeological ceramic objects or pottery<br />

fragments by neutron diffraction (ND) was extensively demonstrated before [1,2]. However, the determination<br />

and interpretation of maximum firing temperatures is the subject of many debates in the archaeology community<br />

[3]. The knowledge of the mineral content and the firing temperatures are of interest since they permit an<br />

assessment of the raw materials used and of details of the firing procedures. This information may allow for an<br />

assessment of the technical skills of the ancient potters and hence on the cultural achievements of ancient<br />

civilizations. When only oxidizing firing is considered, the physical and chemical transformations taking place in<br />

pottery clays cannot be reversed by firing again below the original firing temperature [4]. Such in-situ<br />

measurements of mineral phase transformation are well performed on a neutron diffractometer that do not<br />

require detector scans. The current study was the first part of a proposed systematic investigation, using TOF-<br />

ND, on the characterization of ancient pottery from different periods ranging from prehistoric to 1 st<br />

century BC, found at various excavation sites in North Greece. The aim of this project is to supply a<br />

ceramic/pottery database on the constituent minerals, firing and weathering conditions, to both archaeologist and<br />

scientists in the field. The present experiment was performed in two steps. First, each of the eight ceramic pieces<br />

of approximate dimensions 3 - 15 cm 2 and 0.7 – 1.5 cm thick, were exposed to the beam for several hours at<br />

room temperature and ND patterns were collected (Fig. 1).<br />

Fig.1: Observed diffraction patterns collected at room temperature of seven ceramic samples.<br />

During the second step a single piece of very low fired pottery from Karabournaki was selected for<br />

firing measurements in a furnace. In-situ of ND patterns were collected (Fig.2). The aim was to estimate the<br />

firing temperature by re-firing pottery samples on the beam line and record the neutron diffraction pattern after<br />

each firing step. The starting temperature was 600 ºC and the first significant changes in the diffraction pattern<br />

were observed for temperatures above 650 ºC. Then the temperature was increased from 700 to 975 ºC in<br />

steps of 25 ºC. The neutron diffraction data was analyzed and structure refinement on the observed mineral<br />

phases was performed using the program AMPhOrAe (Archeometric Multi Phase Ornament & Artefacts<br />

analyses)[5]. This program was developed to serve the multiphase modeling requirements of TOF –ND data<br />

analysis. The neutron diffraction data was analyzed and structure refinement on the observed mineral phases<br />

was performed using the program AMPhOrAe (Archeometric Multi Phase Ornament & Artefacts analyses)[5].<br />

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