Rheology of ε-iron up to 19 GPa and 600 K in the D-DIA
dc.contributor.author | Nishiyama, N | en_AU |
dc.contributor.author | Wang, YD | en_AU |
dc.contributor.author | Rivers, ML | en_AU |
dc.contributor.author | Sutton, SR | en_AU |
dc.contributor.author | Cookson, DJ | en_AU |
dc.date.accessioned | 2008-04-28T04:47:23Z | en_AU |
dc.date.accessioned | 2010-04-30T05:03:02Z | en_AU |
dc.date.available | 2008-04-28T04:47:23Z | en_AU |
dc.date.available | 2010-04-30T05:03:02Z | en_AU |
dc.date.issued | 2007-12-07 | en_AU |
dc.date.statistics | 2007-12 | en_AU |
dc.description.abstract | Stress-strain curves, i.e., relations between the differential stress and macroscopic sample strain, of polycrystalline ε-iron have been obtained at pressures of 17(±1) GPa, three different temperatures (600, 400, and 300 K), and various strain rates between 3.8 × 10−6 and 2.3 × 10−5 s−1 using the deformation-DIA coupled with monochromatic X-rays. Five independent stress-strain curves were obtained on axial shortening and the sample exhibited ductile behavior in all. Above 4% axial strain, sample stresses reach saturation and the sample exhibited steady-state deformation. Stress exponents at temperatures of 400 and 600 K were determined to be ∼31 and ∼7, respectively. These results indicate that ε-iron deforms in plasticity regime below 400 K and that the dominant deformation mechanism at 600 K may be low temperature power-law creep. The overall deformation behavior for ε-iron is consistent with that of zinc, suggesting that the deformation mechanism map of ε-iron resembles those of other hexagonal metals. © 2007, American Geophysical Union | en_AU |
dc.identifier.citation | Nishiyama, N., Wang, Y., Rivers, M. L., Sutton, S. R., & Cookson, D. (2007). Rheology of epsilon-iron up to 19 GPa and 600 K in the D-DIA. Geophysical Research Letters, 35(23), L23304. doi:10.1029/2007GL031431 | en_AU |
dc.identifier.govdoc | 1194 | en_AU |
dc.identifier.issn | 0094-8276 | en_AU |
dc.identifier.issue | 23 | en_AU |
dc.identifier.journaltitle | Geophysical Research Letters | en_AU |
dc.identifier.pagination | L23304 | en_AU |
dc.identifier.uri | http://dx.doi.org/10.1029/2007GL031431 | en_AU |
dc.identifier.uri | http://apo.ansto.gov.au/dspace/handle/10238/1133 | en_AU |
dc.identifier.volume | 35 | en_AU |
dc.language.iso | en | en_AU |
dc.publisher | American Geophysical Union | en_AU |
dc.subject | Earth core | en_AU |
dc.subject | Crystal structure | en_AU |
dc.subject | Deformation | en_AU |
dc.subject | Zinc | en_AU |
dc.subject | Iron | en_AU |
dc.subject | Rheology | en_AU |
dc.title | Rheology of ε-iron up to 19 GPa and 600 K in the D-DIA | en_AU |
dc.type | Journal Article | en_AU |