scholarly journals Well-posedness of an extended model for water-ice phase transitions

2013 ◽  
Vol 6 (2) ◽  
pp. 439-460 ◽  
Author(s):  
Pavel Krejčí ◽  
◽  
Elisabetta Rocca ◽  
1998 ◽  
Vol 05 (01) ◽  
pp. 437-441
Author(s):  
N. M. Persiantseva ◽  
O. B. Popovicheva ◽  
T. V. Rakhimova

The HCl-ice interaction has been investigated over a wide HCl pressure range of 10-7–10-4 Torr and ice temperatures 150–240 K. The Three characteristic values for HCl uptake efficiency were obtained which indicate the change of phase state and structure of the ice surface at increasing HCl pressure. The low value γ ≈ 0.1 ± 0.02 corresponds to HCl vapor interaction with pure ice and is realized at the atmosphere conditions. The value γ ≈ 0.5 ± 0.1 indicates the formation of hexahydrate HCl • 6H 2 O with increase of HCl pressure. And the largest value of γ ≈ 0.8 ± 0.1 is observed at appearance of liquid or amorphous solid 4:1 H 2O:HCl. The HCl uptake kinetics is analyzed. The flow of HCl molecules from the ice surface into the bulk is shown to play an important role in the redistribution of HCl molecules. It defines a low surface concentration of the adsorbed HCl molecules under stratospher condition at early times of interaction.


2009 ◽  
Vol 54 (4) ◽  
pp. 161-166 ◽  
Author(s):  
M. I. Samoĭlovich ◽  
A. L. Talis ◽  
G. F. Tereshchenko

2019 ◽  
Vol 28 (1) ◽  
pp. 103-113 ◽  
Author(s):  
I. V. Mezentsev ◽  
Yu. I. Aristov ◽  
N. N. Mezentseva ◽  
V. A. Mukhin

Algorithms ◽  
2020 ◽  
Vol 13 (7) ◽  
pp. 170 ◽  
Author(s):  
Giuseppe Maria Coclite ◽  
Lorenzo di Ruvo

High order convective Cahn-Hilliard type equations describe the faceting of a growing surface, or the dynamics of phase transitions in ternary oil-water-surfactant systems. In this paper, we prove the well-posedness of the classical solutions for the Cauchy problem, associated with this equation.


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