Formation behavior of basal texture under the high temperature plane strain compression deformation in AZ80 magnesium alloy
Creators
- 1. Department of Metallurgical Engineering, Pukyong National University, Busan 608-739 (Korea, Republic of)
- 2. Department of Solid State Materials and Engineering, Yokohama National University, Yokohama 240-8501 (Japan)
Description
The formation behavior of basal texture during high temperature deformation of AZ80 magnesium alloys in single phase was investigated by plane strain compression deformation. Three kinds of specimens with different initial textures were machined out from an extruded bar having a <101-bar0> texture. Plane strain compression tests were conducted at temperatures of 623K and 723K and a strain rate of 5.0×10-2s-1, with a strain range of between - 0.4 and -1.0. After deformation, the specimens were immediately quenched in oil. Texture measurement was carried out on the compression planes by the Schulz reflection method using nickel filtered Cu Kα radiation. Electron backscatter diffraction (EBSD) measurements were also conducted in order to examine the spatial distribution of orientations. Three kinds of specimens named A, B and C were prepared from the same extruded bar. In the specimens A, B and C, {0001} was distributed preferentially parallel to ND, TD, and RD, respectively. After deformation, texture evaluation was conducted on the mid-plane section. At the plane strain compression deformation, peaks appeared in the true stress-true strain curves irrespective of the kinds of specimen used. It was found that the main components and the pole densities of the textures vary depending on deformation condition and initial texture. Six kinds of texture components were observed after deformation. The (0001)<101-bar0> has formed regardless of the initial texture. There are two types of texture components; one exists before the deformation, and the other does not. Either types are considered to have stable orientations for plane strain compression. Also, the basal texture is composed of two crystal orientation components - (0001)<101-bar0> and (0001)<112-bar0>. When (0001) existed before deformation, an extremely sharp (0001) (compression plane) texture is formed. (paper)
Availability note (English)
Available from http://dx.doi.org/10.1088/1757-899X/82/1/012049Additional details
Identifiers
Publishing Information
- Journal Title
- IOP Conference Series. Materials Science and Engineering (Online)
- Journal Volume
- 82
- Journal Issue
- 1
- Journal Page Range
- [4 p.]
- ISSN
- 1757-899X
Conference
- Title
- 17. international conference on textures of materials
- Acronym
- ICOTOM 17
- Dates
- 24-29 Aug 2014
- Place
- Dresden (Germany)
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 47099326
- Subject category
- S36: MATERIALS SCIENCE;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- BACKSCATTERING; COMPRESSION; CRYSTALS; DEFORMATION; DENSITY; ELECTRON DIFFRACTION; ELECTRONS; EVALUATION; FILTERS; MAGNESIUM ALLOYS; NICKEL; OILS; REFLECTION; SPATIAL DISTRIBUTION; STRAIN RATE; STRAINS; STRESSES; TEXTURE
- Descriptors DEC
- ALLOYS; COHERENT SCATTERING; DIFFRACTION; DISTRIBUTION; ELEMENTARY PARTICLES; ELEMENTS; FERMIONS; LEPTONS; METALS; ORGANIC COMPOUNDS; OTHER ORGANIC COMPOUNDS; PHYSICAL PROPERTIES; SCATTERING; TRANSITION ELEMENTS