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

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 Roman terra 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-sigillata and high-quality sigillata periods. In the second example, we investigated the modifications occurring in Neolithic and geological flints aftermore » 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. In conclusion, 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.« less

Authors:
 [1];  [2];  [2];  [3];  [4]
  1. ETH Zurich, Zurich (Switzerland)
  2. Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
  3. CNRS - Univ. de Poitiers - ENSMA, Futuroscope (France)
  4. CEMES - CNRS - Univ. de Toulouse, Toulouse (France)
Publication Date:
Research Org.:
Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Basic Energy Sciences (BES)
OSTI Identifier:
1392969
Grant/Contract Number:  
AC02-05CH11231
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Applied Crystallography (Online)
Additional Journal Information:
Journal Name: Journal of Applied Crystallography (Online); Journal Volume: 48; Journal Issue: 5; Journal ID: ISSN 1600-5767
Publisher:
International Union of Crystallography
Country of Publication:
United States
Language:
English
Subject:
36 MATERIALS SCIENCE; cultural heritage materials; Laue microdiffraction; powder microdiffraction; grain size; residual strain

Citation Formats

Dejoie, Catherine, Tamura, Nobumichi, Kunz, Martin, Goudeau, Philippe, and Sciau, Philippe. Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials. United States: N. p., 2015. Web. doi:10.1107/S1600576715014983.
Dejoie, Catherine, Tamura, Nobumichi, Kunz, Martin, Goudeau, Philippe, & Sciau, Philippe. Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials. United States. doi:10.1107/S1600576715014983.
Dejoie, Catherine, Tamura, Nobumichi, Kunz, Martin, Goudeau, Philippe, and Sciau, Philippe. Sun . "Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials". United States. doi:10.1107/S1600576715014983. https://www.osti.gov/servlets/purl/1392969.
@article{osti_1392969,
title = {Complementary use of monochromatic and white-beam X-ray micro-diffraction for the investigation of ancient materials},
author = {Dejoie, Catherine and Tamura, Nobumichi and Kunz, Martin and Goudeau, Philippe and Sciau, Philippe},
abstractNote = {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 Roman terra 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-sigillata and high-quality sigillata periods. 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. In conclusion, 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.},
doi = {10.1107/S1600576715014983},
journal = {Journal of Applied Crystallography (Online)},
number = 5,
volume = 48,
place = {United States},
year = {2015},
month = {9}
}

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Cited by: 6 works
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    Works referencing / citing this record:

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