In situ structure determination of the high-pressure phase of Fe3O4

1999 ◽  
Vol 84 (1-2) ◽  
pp. 203-206 ◽  
Author(s):  
Yingwei Fei ◽  
Daniel J. Frost ◽  
Ho-Kwang Mao ◽  
Charles T. Prewitt ◽  
Daniel Haeusermann
2014 ◽  
Vol 115 (22) ◽  
pp. 223507 ◽  
Author(s):  
Yanchun Li ◽  
Chuanlong Lin ◽  
Gong Li ◽  
Jian Xu ◽  
Xiaodong Li ◽  
...  

2002 ◽  
Vol 106 (1) ◽  
pp. 30-33 ◽  
Author(s):  
Hiroyasu Shimizu ◽  
Tatsuya Kumazaki ◽  
Tetsuji Kume ◽  
Shigeo Sasaki

2019 ◽  
Vol 36 (4) ◽  
pp. 046103 ◽  
Author(s):  
Sheng Jiang ◽  
Jing Liu ◽  
Xiao-Dong Li ◽  
Yan-Chun Li ◽  
Shang-Ming He ◽  
...  

2017 ◽  
Vol 102 (3) ◽  
pp. 666-673 ◽  
Author(s):  
Anna Pakhomova ◽  
Leyla Ismailova ◽  
Elena Bykova ◽  
Maxim Bykov ◽  
Tiziana Boffa Ballaran ◽  
...  

2008 ◽  
Vol 1146 ◽  
Author(s):  
Simon Ruffell ◽  
Jodie Bradby ◽  
Jim Williams ◽  
Ryan Major ◽  
Oden Warren

AbstractPhase transformed zones of silicon have been formed by nanoindentation both at the micro- and nanoscale and electrically probed using an in-situ measurement system. Zones composed of the high pressure crystalline phases (Si-III/Si-XII) have higher conductivity than those of amorphous silicon (a-Si). At the microscale probing laterally across the surface shows that the conductivity varies within the zones composed of the high pressure phases. The sensitivity to the different conductivities of the two phases allows mapping within the zones. Finally, at the nanoscale the conductivity of the high pressure phase zones can be correlated with the position of the pop-out associated with the formation of the phases. The zones have higher conductivity when the pop-out occurs earlier on unloading and we suggest that this is due to the reduction in trace volumes of a-Si formed during the early portion of the unloading cycle.


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