scholarly journals Thermal equation of state of Molybdenum determined from in situ synchrotron X-ray diffraction with laser-heated diamond anvil cells

2016 ◽  
Vol 6 (1) ◽  
Author(s):  
Xiaoli Huang ◽  
Fangfei Li ◽  
Qiang Zhou ◽  
Yue Meng ◽  
Konstantin D. Litasov ◽  
...  
Keyword(s):  
Equation Of State ◽  
X Ray Diffraction ◽  
Diamond Anvil Cells ◽  
Thermal Equation ◽  
X Ray ◽  
Thermal Equation Of State ◽  
Diamond Anvil ◽  
Laser Heated

In situ synchrotron X-ray diffraction with laser-heated diamond anvil cells study of Pt up to 95 GPa and 3150 K

RSC Advances ◽  
2015 ◽  
Vol 5 (19) ◽  
pp. 14603-14609 ◽  
Author(s):  
Xiaoli Huang ◽  
Fangfei Li ◽  
Qiang Zhou ◽  
Gang Wu ◽  
Yanping Huang ◽  
...  
Keyword(s):  
X Ray Diffraction ◽  
Diamond Anvil Cells ◽  
X Ray ◽  
Diamond Anvil ◽  
Laser Heated

In situ synchrotron X-ray diffraction with laser-heated diamond anvil cells study the EOS of Pt.

Thermal equation of state of MgSiO4H2 phase H determined by in situ X-ray diffraction and a multianvil apparatus

2018 ◽  
Vol 45 (10) ◽  
pp. 995-1001 ◽  
Author(s):  
Masayuki Nishi ◽  
Jun Tsuchiya ◽  
Takeshi Arimoto ◽  
Sho Kakizawa ◽  
Takehiro Kunimoto ◽  
...  
Keyword(s):  
Equation Of State ◽  
X Ray Diffraction ◽  
Thermal Equation ◽  
X Ray ◽  
Thermal Equation Of State

Thermal equation of state of solid naphthalene to 13 GPa and 773 K: In situ X-ray diffraction study and first principles calculations

2014 ◽  
Vol 140 (16) ◽  
pp. 164508 ◽  
Author(s):  
Anna Y. Likhacheva ◽  
Sergey V. Rashchenko ◽  
Artem D. Chanyshev ◽  
Talgat M. Inerbaev ◽  
Konstantin D. Litasov ◽  
...  
Keyword(s):  
Equation Of State ◽  
Diffraction Study ◽  
First Principles ◽  
First Principles Calculations ◽  
X Ray Diffraction ◽  
Thermal Equation ◽  
X Ray ◽  
Thermal Equation Of State

scholarly journals The thermal equation of state of FeTiO3 ilmenite based on in situ X-ray diffraction at high pressures and temperatures

2010 ◽  
Vol 95 (11-12) ◽  
pp. 1708-1716 ◽  
Author(s):  
E. J. Tronche ◽  
M. van Kan Parker ◽  
J. de Vries ◽  
Y. Wang ◽  
T. Sanehira ◽  
...  
Keyword(s):  
Equation Of State ◽  
High Pressures ◽  
X Ray Diffraction ◽  
Thermal Equation ◽  
X Ray ◽  
Thermal Equation Of State ◽  
High Pressures And Temperatures

Construction of laser-heated diamond anvil cell system for in situ x-ray diffraction study at SPring-8

2001 ◽  
Vol 72 (2) ◽  
pp. 1289 ◽  
Author(s):  
Tetsu Watanuki ◽  
Osamu Shimomura ◽  
Takehiko Yagi ◽  
Tadashi Kondo ◽  
Maiko Isshiki
Keyword(s):  
Diffraction Study ◽  
Diamond Anvil Cell ◽  
Cell System ◽  
X Ray Diffraction ◽  
X Ray ◽  
Diamond Anvil ◽  
Laser Heated

Thermal equation-of-state of osmium: a synchrotron X-ray diffraction study

2005 ◽  
Vol 66 (5) ◽  
pp. 706-710 ◽  
Author(s):  
G.A. Voronin ◽  
C. Pantea ◽  
T.W. Zerda ◽  
L. Wang ◽  
Y. Zhao
Keyword(s):  
Equation Of State ◽  
Diffraction Study ◽  
X Ray Diffraction ◽  
Thermal Equation ◽  
X Ray ◽  
Thermal Equation Of State

In situ synchrotron X-ray diffraction study of the formation of TaB2 from the elements in a laser heated diamond anvil cell

2010 ◽  
Vol 12 (12) ◽  
pp. 2059-2064 ◽  
Author(s):  
Björn Winkler ◽  
Erick A. Juarez-Arellano ◽  
Alexandra Friedrich ◽  
Lkhamsuren Bayarjargal ◽  
Florian Schröder ◽  
...  
Keyword(s):  
Diffraction Study ◽  
Diamond Anvil Cell ◽  
X Ray Diffraction ◽  
X Ray ◽  
Diamond Anvil ◽  
Laser Heated

In situ synchrotron X-ray diffraction in the laser-heated diamond anvil cell: Melting phenomena and synthesis of new materials

2014 ◽  
Vol 277-278 ◽  
pp. 15-30 ◽  
Author(s):  
Ashkan Salamat ◽  
Rebecca A. Fischer ◽  
Richard Briggs ◽  
Malcolm I. McMahon ◽  
Sylvain Petitgirard
Keyword(s):  
Diamond Anvil Cell ◽  
New Materials ◽  
X Ray Diffraction ◽  
X Ray ◽  
Diamond Anvil ◽  
Laser Heated

Deep Earth mineralogy revealed by ultrahigh-pressure experiments

2014 ◽  
Vol 78 (2) ◽  
pp. 437-446 ◽  
Author(s):  
Kei Hirose
Keyword(s):  
Phase Transition ◽  
Ultrahigh Pressure ◽  
X Ray Diffraction ◽  
X Ray ◽  
Deep Earth ◽  
Diamond Anvil ◽  
Lowermost Part ◽  
Fe Alloys ◽  
Laser Heated

AbstractUltrahigh-pressure and -temperature (P-T) experimental techniques have progressed rapidly in recent years. By combining them with X-ray diffraction measurements at synchrotron radiation facilities, it is now possible to examine deep Earth mineralogy in situ at relevant high P-T conditions in a laser-heated diamond anvil cell (DAC). The lowermost part of the mantle, known as the D″ layer, has long been enigmatic because of a number of unexplained seismological features. Nevertheless, the discovery of a phase transition from MgSiO3 perovskite to ‘post-perovskite’ above 120 GPa and 2400 K indicates that post-perovskite is a principal constituent in the lowermost mantle, which is compatible with seismic observations. The ultrahigh P-T conditions of the Earth’s core have not been accessible by static experiments, but the structure and phase transition of Fe and Fe-alloys are now being examined up to 400 GPa and 6000 K by laser-heated DAC studies.

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