Expanding the calculation of activation volumes: Self-diffusion in liquid water

2018 ◽  
Vol 148 (13) ◽  
pp. 134105 ◽  
Author(s):  
Zeke A. Piskulich ◽  
Oluwaseun O. Mesele ◽  
Ward H. Thompson
Keyword(s):  
1998 ◽  
Vol 44 (148) ◽  
pp. 467-468 ◽  
Author(s):  
J. F. Nye

Abstract The annual layering in the Greenland and Antarctic ice sheets revealed by the b 0 record becomes less distinct with depth because of self-diffusion. However, the calculated diffusion rates are loo slow to explain die observations. It is suggested that the presence of veins of liquid water increases the effective diffusion constant by a factor of about 20.


1974 ◽  
Vol 48 (4) ◽  
pp. 289-290 ◽  
Author(s):  
F.D. Ricci ◽  
M.A. Ricci ◽  
D. Rocca

2000 ◽  
Vol 62 (3) ◽  
pp. 3572-3580 ◽  
Author(s):  
T. V. Lokotosh ◽  
S. Magazù ◽  
G. Maisano ◽  
N. P. Malomuzh

Molecules ◽  
2021 ◽  
Vol 26 (19) ◽  
pp. 5899
Author(s):  
Carmelo Corsaro ◽  
Enza Fazio

Liquid’s behaviour, when close to critical points, is of extreme importance both for fundamental research and industrial applications. A detailed knowledge of the structural–dynamical correlations in their proximity is still today a target to reach. Liquid water anomalies are ascribed to the presence of a second liquid–liquid critical point, which seems to be located in the very deep supercooled regime, even below 200 K and at pressure around 2 kbar. In this work, the thermal behaviour of the self-diffusion coefficient for liquid water is analyzed, in terms of a two-states model, for the first time in a very wide thermal region (126 K < T < 623 K), including those of the two critical points. Further, the corresponding configurational entropy and isobaric-specific heat have been evaluated within the same interval. The two liquid states correspond to high and low-density water local structures that play a primary role on water dynamical behavior over 500 K.


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