S. Demouchy, M. Thieme, F. Barou, B. Beausir, V. Taupin, P. Cordier
{"title":"实验变形多晶橄榄石中的位错和向错密度","authors":"S. Demouchy, M. Thieme, F. Barou, B. Beausir, V. Taupin, P. Cordier","doi":"10.5194/ejm-35-219-2023","DOIUrl":null,"url":null,"abstract":"Abstract. We report a comprehensive data set characterizing and\nquantifying the geometrically necessary dislocation (GND) density in the\ncrystallographic frame (ραc) and disclination density\n(ρθ) in fine-grained polycrystalline olivine deformed in\nuniaxial compression or torsion, at 1000 and 1200 ∘C, under a confining pressure of 300 MPa. Finite strains range from 0.11 up\nto 8.6 %, and stresses reach up to 1073 MPa. The data set is a selection\nof 19 electron backscatter diffraction maps acquired with conventional\nangular resolution (0.5∘) but at high spatial resolution (step\nsize ranging between 0.05 and 0.1 µm). Thanks to analytical\nimprovement for data acquisition and treatment, notably with the use of ATEX (Analysis Tools for Electron and X-ray diffraction)\nsoftware, we report the spatial distribution of both GND and disclination\ndensities. Areas with the highest GND densities define sub-grain boundaries.\nThe type of GND densities involved also indicates that most olivine sub-grain\nboundaries have a mixed character. Moreover, the strategy for visualization also\npermits identifying minor GND that is not well organized as sub-grain boundaries\nyet. A low-temperature and high-stress sample displays a higher but less organized GND density than in a sample deformed at high temperature for a similar\nfinite strain, grain size, and identical strain rate, confirming the action\nof dislocation creep in these samples, even for micrometric grains (2 µm). Furthermore, disclination dipoles along grain boundaries are identified\nin every undeformed and deformed electron backscatter diffraction (EBSD) map, mostly at the junction of a\ngrain boundary with a sub-grain but also along sub-grain boundaries and at\nsub-grain boundary tips. Nevertheless, for the range of experimental\nparameters investigated, there is no notable correlation of the disclination\ndensity with stress, strain, or temperature. However, a broad positive\ncorrelation between average disclination density and average GND density per\ngrain is found, confirming their similar role as defects producing\nintragranular misorientation. Furthermore, a broad negative correlation\nbetween the disclination density and the grain size or perimeter is found,\nproviding a first rule of thumb on the distribution of disclinations. Field\ndislocation and disclination mechanics (FDDM) of the elastic fields due to\nexperimentally measured dislocations and disclinations (e.g., strains/rotations and stresses) provides further evidence of the interplay\nbetween both types of defects. At last, our results also support that\ndisclinations act as a plastic deformation mechanism, by allowing rotation\nof a very small crystal volume.\n","PeriodicalId":11971,"journal":{"name":"European Journal of Mineralogy","volume":null,"pages":null},"PeriodicalIF":1.8000,"publicationDate":"2023-03-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":"{\"title\":\"Dislocation and disclination densities in experimentally deformed polycrystalline olivine\",\"authors\":\"S. Demouchy, M. Thieme, F. Barou, B. Beausir, V. Taupin, P. Cordier\",\"doi\":\"10.5194/ejm-35-219-2023\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Abstract. We report a comprehensive data set characterizing and\\nquantifying the geometrically necessary dislocation (GND) density in the\\ncrystallographic frame (ραc) and disclination density\\n(ρθ) in fine-grained polycrystalline olivine deformed in\\nuniaxial compression or torsion, at 1000 and 1200 ∘C, under a confining pressure of 300 MPa. Finite strains range from 0.11 up\\nto 8.6 %, and stresses reach up to 1073 MPa. The data set is a selection\\nof 19 electron backscatter diffraction maps acquired with conventional\\nangular resolution (0.5∘) but at high spatial resolution (step\\nsize ranging between 0.05 and 0.1 µm). Thanks to analytical\\nimprovement for data acquisition and treatment, notably with the use of ATEX (Analysis Tools for Electron and X-ray diffraction)\\nsoftware, we report the spatial distribution of both GND and disclination\\ndensities. Areas with the highest GND densities define sub-grain boundaries.\\nThe type of GND densities involved also indicates that most olivine sub-grain\\nboundaries have a mixed character. Moreover, the strategy for visualization also\\npermits identifying minor GND that is not well organized as sub-grain boundaries\\nyet. A low-temperature and high-stress sample displays a higher but less organized GND density than in a sample deformed at high temperature for a similar\\nfinite strain, grain size, and identical strain rate, confirming the action\\nof dislocation creep in these samples, even for micrometric grains (2 µm). Furthermore, disclination dipoles along grain boundaries are identified\\nin every undeformed and deformed electron backscatter diffraction (EBSD) map, mostly at the junction of a\\ngrain boundary with a sub-grain but also along sub-grain boundaries and at\\nsub-grain boundary tips. Nevertheless, for the range of experimental\\nparameters investigated, there is no notable correlation of the disclination\\ndensity with stress, strain, or temperature. However, a broad positive\\ncorrelation between average disclination density and average GND density per\\ngrain is found, confirming their similar role as defects producing\\nintragranular misorientation. Furthermore, a broad negative correlation\\nbetween the disclination density and the grain size or perimeter is found,\\nproviding a first rule of thumb on the distribution of disclinations. Field\\ndislocation and disclination mechanics (FDDM) of the elastic fields due to\\nexperimentally measured dislocations and disclinations (e.g., strains/rotations and stresses) provides further evidence of the interplay\\nbetween both types of defects. At last, our results also support that\\ndisclinations act as a plastic deformation mechanism, by allowing rotation\\nof a very small crystal volume.\\n\",\"PeriodicalId\":11971,\"journal\":{\"name\":\"European Journal of Mineralogy\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.8000,\"publicationDate\":\"2023-03-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"2\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"European Journal of Mineralogy\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.5194/ejm-35-219-2023\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"MINERALOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"European Journal of Mineralogy","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5194/ejm-35-219-2023","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MINERALOGY","Score":null,"Total":0}
Dislocation and disclination densities in experimentally deformed polycrystalline olivine
Abstract. We report a comprehensive data set characterizing and
quantifying the geometrically necessary dislocation (GND) density in the
crystallographic frame (ραc) and disclination density
(ρθ) in fine-grained polycrystalline olivine deformed in
uniaxial compression or torsion, at 1000 and 1200 ∘C, under a confining pressure of 300 MPa. Finite strains range from 0.11 up
to 8.6 %, and stresses reach up to 1073 MPa. The data set is a selection
of 19 electron backscatter diffraction maps acquired with conventional
angular resolution (0.5∘) but at high spatial resolution (step
size ranging between 0.05 and 0.1 µm). Thanks to analytical
improvement for data acquisition and treatment, notably with the use of ATEX (Analysis Tools for Electron and X-ray diffraction)
software, we report the spatial distribution of both GND and disclination
densities. Areas with the highest GND densities define sub-grain boundaries.
The type of GND densities involved also indicates that most olivine sub-grain
boundaries have a mixed character. Moreover, the strategy for visualization also
permits identifying minor GND that is not well organized as sub-grain boundaries
yet. A low-temperature and high-stress sample displays a higher but less organized GND density than in a sample deformed at high temperature for a similar
finite strain, grain size, and identical strain rate, confirming the action
of dislocation creep in these samples, even for micrometric grains (2 µm). Furthermore, disclination dipoles along grain boundaries are identified
in every undeformed and deformed electron backscatter diffraction (EBSD) map, mostly at the junction of a
grain boundary with a sub-grain but also along sub-grain boundaries and at
sub-grain boundary tips. Nevertheless, for the range of experimental
parameters investigated, there is no notable correlation of the disclination
density with stress, strain, or temperature. However, a broad positive
correlation between average disclination density and average GND density per
grain is found, confirming their similar role as defects producing
intragranular misorientation. Furthermore, a broad negative correlation
between the disclination density and the grain size or perimeter is found,
providing a first rule of thumb on the distribution of disclinations. Field
dislocation and disclination mechanics (FDDM) of the elastic fields due to
experimentally measured dislocations and disclinations (e.g., strains/rotations and stresses) provides further evidence of the interplay
between both types of defects. At last, our results also support that
disclinations act as a plastic deformation mechanism, by allowing rotation
of a very small crystal volume.
期刊介绍:
EJM was founded to reach a large audience on an international scale and also for achieving closer cooperation of European countries in the publication of scientific results. The founding societies have set themselves the task of publishing a journal of the highest standard open to all scientists performing mineralogical research in the widest sense of the term, all over the world. Contributions will therefore be published primarily in English.
EJM publishes original papers, review articles and letters dealing with the mineralogical sciences s.l., primarily mineralogy, petrology, geochemistry, crystallography and ore deposits, but also biomineralogy, environmental, applied and technical mineralogy. Nevertheless, papers in any related field, including cultural heritage, will be considered.