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Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials

Authors :
Philippe Sciau
Philippe Goudeau
Catherine Dejoie
Martin Kunz
Nobumichi Tamura
Laboratory of Crystallography [ETH Zürich]
Department of Materials [ETH Zürich] (D-MATL)
Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology [Zürich] (ETH Zürich)
Stanford Synchrotron Radiation Lightsource (SSRL SLAC)
SLAC National Accelerator Laboratory (SLAC)
Stanford University-Stanford University
Institut Pprime (PPRIME)
Université de Poitiers-ENSMA-Centre National de la Recherche Scientifique (CNRS)
Centre d'élaboration de matériaux et d'études structurales (CEMES)
Institut National des Sciences Appliquées - Toulouse (INSA Toulouse)
Institut National des Sciences Appliquées (INSA)-Université de Toulouse (UT)-Institut National des Sciences Appliquées (INSA)-Université de Toulouse (UT)-Institut de Chimie de Toulouse (ICT)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP)
Université de Toulouse (UT)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Institut de Chimie du CNRS (INC)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP)
Université de Toulouse (UT)-Centre National de la Recherche Scientifique (CNRS)
ENSMA-Centre National de la Recherche Scientifique (CNRS)-Université de Poitiers
Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Chimie de Toulouse (ICT-FR 2599)
Institut National Polytechnique (Toulouse) (Toulouse INP)
Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université Fédérale Toulouse Midi-Pyrénées-Institut de Chimie du CNRS (INC)-Institut National Polytechnique (Toulouse) (Toulouse INP)
Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut de Chimie du CNRS (INC)-Institut National des Sciences Appliquées - Toulouse (INSA Toulouse)
Institut National des Sciences Appliquées (INSA)-Institut National des Sciences Appliquées (INSA)
Source :
JOURNAL OF APPLIED CRYSTALLOGRAPHY, Journal of Applied Crystallography, Journal of Applied Crystallography, 2015, 48, pp.1522-1533. ⟨10.1107/S1600576715014983⟩, Journal of Applied Crystallography, International Union of Crystallography, 2015, 48, pp.1522-1533. ⟨10.1107/S1600576715014983⟩, Dejoie, C; Tamura, N; Kunz, M; Goudeau, P; & Sciau, P. (2015). Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials. Journal of Applied Crystallography, 48, 1522-1533. doi: 10.1107/S1600576715014983. Lawrence Berkeley National Laboratory: Retrieved from: http://www.escholarship.org/uc/item/4ft7j7c2, Journal of Applied Crystallography, vol 48, iss 5
Publication Year :
2015

Abstract

Archaeological artefacts are often heterogeneous materials where several phases coexist in a wide grain size distribution. Most of the time, retrieving structure information at the micrometre scale is of great importance for these materials. Particularly, the organization of different phases at the micrometre scale is closely related to optical or mechanical properties, manufacturing processes, functionalities in ancient times and long-term conservation. Between classic X-ray powder diffraction with a millimetre beam and transmission electron microscopy, a gap exists and structure and phase information at the micrometre scale are missing. Using a micrometre-size synchrotron X-ray beam, a hybrid approach combining both monochromatic powder micro-diffraction and Laue single-crystal micro-diffraction was deployed to obtain information from nanometre- and micrometre-size phases, respectively. Therefore providing a way to bridge the aforementioned gap, this unique methodology was applied to three different types of ancient materials that all show a strong heterogeneity. In Romanterra sigillata, the specific distribution of nanocrystalline hematite is mainly responsible for the deep-red tone of the slip, while the distribution of micrometre-size quartz in ceramic bodies reflects the change of manufacturing process between pre-sigillataand high-qualitysigillataperiods. In the second example, we investigated the modifications occurring in Neolithic and geological flints after a heating process. By separating the diffracted signal coming from the nano- and the micrometre scale, we observed a domain size increase for nanocrystalline quartz in geological flints and a relaxation of the residual strain in larger detritic quartz. Finally, through the study of a Roman iron nail, we showed that the carburation process to strengthen the steel was mainly a surface process that formed 10–20 µm size domains of single-crystal ferrite and nanocrystalline cementite.

Details

ISSN :
00218898 and 16005767
Volume :
48
Database :
OpenAIRE
Journal :
JOURNAL OF APPLIED CRYSTALLOGRAPHY
Accession number :
edsair.doi.dedup.....4a630972987ae83c61f372b6794e7a33
Full Text :
https://doi.org/10.1107/S1600576715014983