Fugacities of gases and some mineralogical reactions at very high pressures and temperatures (an extrapolation)

1978 ◽  
Vol 2 (4) ◽  
pp. 297-303 ◽  
Author(s):  
I. A. Ostrovsky ◽  
B. N. Rizhenko
2014 ◽  
Vol 85 (2) ◽  
pp. 025102 ◽  
Author(s):  
R. Freedman ◽  
V. Anand ◽  
B. Grant ◽  
K. Ganesan ◽  
P. Tabrizi ◽  
...  

2018 ◽  
Vol 20 (18) ◽  
pp. 12589-12598 ◽  
Author(s):  
Josef N. Stern ◽  
Thomas Loerting

VHDA prepared at high pressures and temperatures appears to be mainly free of (nano)crystallinity. It is the thermally most stable amorphous solid phase of water at elevated pressures reported so far. Water's no man's land's low temperature boundary is thus shifted to higher temperatures by up to 4 K.


2007 ◽  
Vol 5 ◽  
pp. 113-120 ◽  
Author(s):  
R.Kh. Bolotnova

The method of construction the wide-range equations of state for organic liquids, describing the gas and liquid phases including dissociation and ionization which occurs during an intense collapse of steam bubbles and accompanied by ultra-high pressures and temperatures, is proposed.


2020 ◽  
Author(s):  
Kenji Ohta ◽  
Kei Hirose

Abstract Precise determinations of the thermal conductivity of iron alloys at high pressures and temperatures are essential for understanding the thermal history and dynamics of the metallic cores of the Earth. We review relevant high-pressure experiments using a diamond-anvil cell and discuss implications of high core conductivity for its thermal and compositional evolution.


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