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Title: High stereographic resolution texture and residual stress evaluation using time-of-flight neutron diffraction

Abstract

Neutron diffraction texture measurements provide bulk averaged textures with excellent grain orientation statistics, even for large-grained materials, owing to the probed volume being of the order of 1 cm3. Furthermore, crystallographic parameters and other valuable microstructure information such as phase fraction, coherent crystallite size, root-mean-square microstrain, macroscopic or intergranular strain and stress, etc. can be derived from neutron diffractograms. A procedure for combined high stereographic resolution texture and residual stress evaluation was established on the pulsed-neutron-source-based engineering materials diffractometer TAKUMI at the Materials and Life Science Experimental Facility of the Japan Proton Accelerator Research Center, through division of the neutron detector panel regions. Pole figure evaluation of a limestone standard sample with a well known texture suggested that the precision obtained for texture measurement is comparable to that of the established neutron beamlines utilized for texture measurement, such as the HIPPO diffractometer at the Los Alamos Neutron Science Center (New Mexico, USA) and the D20 angle-dispersive neutron diffractometer at the Institut Laue–Langevin (Grenoble, France). A high-strength martensite–austenite multilayered steel was employed for further verification of the reliability of simultaneous Rietveld analysis of multiphase textures and macro stress tensors. By using a texture-weighted geometric mean micromechanical (BulkPathGEO) model, a macro stressmore » tensor analysis with a plane stress assumption showed a rolling direction–transverse direction (RD–TD) in-plane compressive stress (about –330 MPa) in the martensite layers and an RD–TD in-plane tensile stress (about 320 MPa) in the austenite layers. The phase stress partitioning was ascribed mainly to the additive effect of the volume expansion during martensite transformation and the linear contraction misfit between austenite layers and newly transformed martensite layers during the water quenching process.« less

Authors:
ORCiD logo [1]; ORCiD logo [2];  [3];  [1]; ORCiD logo [4];  [2]; ORCiD logo [5];  [6]; ORCiD logo [7];  [2];  [1]
  1. Japan Atomic Energy Agency (JAEA), Ibaraki (Japan)
  2. Japan Atomic Energy Agency (JAEA), Ibaraki (Japan). J-PARC Center
  3. Univ. of Tokyo (Japan). Dept. of Materials Engineering
  4. Comprehensive Research Org. for Science and Society, Ibaraki (Japan). Neutron Science and Technology Center
  5. Los Alamos National Lab. (LANL), Los Alamos, NM (United States). LANSCE
  6. Univ. of Tokyo (Japan). Research Center for Advanced Science and Technology
  7. Japan Atomic Energy Agency (JAEA), Ibaraki (Japan). J-PARC Center; National Inst. for Materials Science (NIMS), Ibaraki (Japan)
Publication Date:
Research Org.:
Los Alamos National Laboratory (LANL), Los Alamos, NM (United States)
Sponsoring Org.:
USDOE Office of Science (SC)
OSTI Identifier:
1625774
Grant/Contract Number:  
AC52-06NA25396
Resource Type:
Accepted Manuscript
Journal Name:
Journal of Applied Crystallography (Online)
Additional Journal Information:
Journal Name: Journal of Applied Crystallography (Online); Journal Volume: 51; Journal Issue: 3; Journal ID: ISSN 1600-5767
Publisher:
International Union of Crystallography
Country of Publication:
United States
Language:
English
Subject:
37 INORGANIC, ORGANIC, PHYSICAL, AND ANALYTICAL CHEMISTRY; 72 PHYSICS OF ELEMENTARY PARTICLES AND FIELDS; chemistry; crystallography; neutron diffraction; texture measurement; stress tensor analysis; multilayered steels; limestone.

Citation Formats

Xu, Pingguang, Harjo, Stefanus, Ojima, Mayumi, Suzuki, Hiroshi, Ito, Takayoshi, Gong, Wu, Vogel, Sven C., Inoue, Junya, Tomota, Yo, Aizawa, Kazuya, and Akita, Koichi. High stereographic resolution texture and residual stress evaluation using time-of-flight neutron diffraction. United States: N. p., 2018. Web. doi:10.1107/s1600576718004004.
Xu, Pingguang, Harjo, Stefanus, Ojima, Mayumi, Suzuki, Hiroshi, Ito, Takayoshi, Gong, Wu, Vogel, Sven C., Inoue, Junya, Tomota, Yo, Aizawa, Kazuya, & Akita, Koichi. High stereographic resolution texture and residual stress evaluation using time-of-flight neutron diffraction. United States. https://doi.org/10.1107/s1600576718004004
Xu, Pingguang, Harjo, Stefanus, Ojima, Mayumi, Suzuki, Hiroshi, Ito, Takayoshi, Gong, Wu, Vogel, Sven C., Inoue, Junya, Tomota, Yo, Aizawa, Kazuya, and Akita, Koichi. Wed . "High stereographic resolution texture and residual stress evaluation using time-of-flight neutron diffraction". United States. https://doi.org/10.1107/s1600576718004004. https://www.osti.gov/servlets/purl/1625774.
@article{osti_1625774,
title = {High stereographic resolution texture and residual stress evaluation using time-of-flight neutron diffraction},
author = {Xu, Pingguang and Harjo, Stefanus and Ojima, Mayumi and Suzuki, Hiroshi and Ito, Takayoshi and Gong, Wu and Vogel, Sven C. and Inoue, Junya and Tomota, Yo and Aizawa, Kazuya and Akita, Koichi},
abstractNote = {Neutron diffraction texture measurements provide bulk averaged textures with excellent grain orientation statistics, even for large-grained materials, owing to the probed volume being of the order of 1 cm3. Furthermore, crystallographic parameters and other valuable microstructure information such as phase fraction, coherent crystallite size, root-mean-square microstrain, macroscopic or intergranular strain and stress, etc. can be derived from neutron diffractograms. A procedure for combined high stereographic resolution texture and residual stress evaluation was established on the pulsed-neutron-source-based engineering materials diffractometer TAKUMI at the Materials and Life Science Experimental Facility of the Japan Proton Accelerator Research Center, through division of the neutron detector panel regions. Pole figure evaluation of a limestone standard sample with a well known texture suggested that the precision obtained for texture measurement is comparable to that of the established neutron beamlines utilized for texture measurement, such as the HIPPO diffractometer at the Los Alamos Neutron Science Center (New Mexico, USA) and the D20 angle-dispersive neutron diffractometer at the Institut Laue–Langevin (Grenoble, France). A high-strength martensite–austenite multilayered steel was employed for further verification of the reliability of simultaneous Rietveld analysis of multiphase textures and macro stress tensors. By using a texture-weighted geometric mean micromechanical (BulkPathGEO) model, a macro stress tensor analysis with a plane stress assumption showed a rolling direction–transverse direction (RD–TD) in-plane compressive stress (about –330 MPa) in the martensite layers and an RD–TD in-plane tensile stress (about 320 MPa) in the austenite layers. The phase stress partitioning was ascribed mainly to the additive effect of the volume expansion during martensite transformation and the linear contraction misfit between austenite layers and newly transformed martensite layers during the water quenching process.},
doi = {10.1107/s1600576718004004},
journal = {Journal of Applied Crystallography (Online)},
number = 3,
volume = 51,
place = {United States},
year = {Wed May 09 00:00:00 EDT 2018},
month = {Wed May 09 00:00:00 EDT 2018}
}

Journal Article:
Free Publicly Available Full Text
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Figures / Tables:

Figure 1 Figure 1: ($a$) Scanning electron microscope image of SUS301/SUS420J2 austenite–martensite multilayered steel along the thickness direction. Black shading denotes martensite (M) and gray shading denotes austenite (A). ($b$) Grain orientation map of the martensite–austenite layers obtained from EBSD. The various colors in the inset standard inverse pole figure (IPF) scalemore » are used to denote the different grain orientations in the IPF mappings of martensite blocks and austenite grains by referring to the normal direction (ND) of multilayered steel; for example, the red grains have $\langle$001$\rangle$ || ND, the green grains have $\langle$110$\rangle$ || ND and the blue grains have $\langle$111$\rangle$|| ND. Grain boundaries are shown with a misorientation angle of 15° .« less

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