2012
DOI: 10.1103/physrevb.86.014101
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In situlattice measurement of the bcc phase boundary in Mg on the principal shock Hugoniot

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Cited by 15 publications
(14 citation statements)
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“…Therefore, the plasticity prior to the phase transition takes place as expected in the experiments. [3][4][5][8][9][10]15) According to the microstructures, we find that the phase transition does not happen uniformly either among different grains or within an individual grain under a weak loading strength, which is well consistent with the coexistence region in experiments of Mg under high pressure. [14][15][16] The dynamics for the shock compression is reflected in the longitudinal pressure profiles, particularly in the relaxation of the shear stress.…”
Section: Yy Zzsupporting
confidence: 83%
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“…Therefore, the plasticity prior to the phase transition takes place as expected in the experiments. [3][4][5][8][9][10]15) According to the microstructures, we find that the phase transition does not happen uniformly either among different grains or within an individual grain under a weak loading strength, which is well consistent with the coexistence region in experiments of Mg under high pressure. [14][15][16] The dynamics for the shock compression is reflected in the longitudinal pressure profiles, particularly in the relaxation of the shear stress.…”
Section: Yy Zzsupporting
confidence: 83%
“…In the 1980s, Olijnyk and Holzapfel firstly found the BCC structure in Mg by energydispersive X-ray diffraction at room temperature when the pressure was around 50 GPa through the linear compression. 14) Since then, a series of work was carried on phase transition of single crystal Mg in experiments 15,16) and theories. [17][18][19][20][21] For example, Milathianaki et al 15) investigated the phase transition of pure Mg under high pressure using single laser pulses, and found the coexistence region of HCP and BCC.…”
mentioning
confidence: 99%
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“…just above the HEL) as an intensitythreshold plot around the origin for a region in reciprocal space bounded by points with Miller indices (±3, ±3, ±3. 45), where the indices are referenced to the ambient unshocked material. At this shock pressure the crystal has been compressed to 87% of its original volume.…”
Section: Resultsmentioning
confidence: 99%
“…In turn, the presence of a Hugoniot discontinuity may provide an indication of a phase transition within the material. However, these methods may fail for solid-liquid transitions (or melting) (Hayes et al, 1999) and solid-solid transitions with expected volume collapses of less than 1%, such as the hexagonal close-packed to body-centred cubic transition in magnesium (Milathianaki et al, 2012).…”
Section: Introductionmentioning
confidence: 99%