scholarly journals Relation between occupation in the first coordination shells and Widom line in core-softened potentials

2013 ◽  
Vol 138 (16) ◽  
pp. 164502 ◽  
Author(s):  
Evy Salcedo ◽  
Ney M. Barraz ◽  
Marcia C. Barbosa
Keyword(s):  
2002 ◽  
Vol 117 (8) ◽  
pp. 3941-3950 ◽  
Author(s):  
P. Tarazona ◽  
E. Chacón ◽  
M. Reinaldo-Falagán ◽  
E. Velasco

2014 ◽  
Vol 89 (4) ◽  
Author(s):  
V. V. Brazhkin ◽  
Yu. D. Fomin ◽  
V. N. Ryzhov ◽  
E. E. Tareyeva ◽  
E. N. Tsiok
Keyword(s):  

2019 ◽  
Vol 89 (3) ◽  
pp. 452
Author(s):  
Г.С. Бордонский

AbstractThe microwave absorption of fresh ice subjected to plastic deformation when changing temperature from 0 to –60°C has been measured. A decrease in the losses of radiation transmission through ice at frequencies of 32 and 125 GHz with extremum at a temperature of –45°C was found. This temperature corresponds to the point at atmospheric pressure at the Widom line, which starts from a hypothetic second critical point in pressure–temperature phase space. The used measuring technique makes it possible to obtain layers of deeply supercooled water into ice and study the position of the Widom line and second critical point in phase space.


2021 ◽  
Vol 16 (3) ◽  
pp. 134-139
Author(s):  
Bordonskiy Georgy S. ◽  

The influence of the nuclei of the liquid phase arising during mechanical deformations of polycrystalline ice at temperatures below -40 ... -45 C on its explosive instability is considered. The nucleus of the liquid phase appear in ice when part of the hydrogen bonds are broken when high pressure is applied to ice crystals. The resulting clusters can have characteristics close to those of bulk metastable water. It is known that such water in the region of negative temperatures has anomalous thermodynamic characteristics. In particular, at a temperature of -60 C and a pressure of 100 MPa, there is a second critical point of water for the liquid-liquid transition. It was found that the transition occurs between the two types of water LDL (low density water) and HDL (high density water), with the Widom line coming out into the one-component region of the water phase diagram. This line is the locus of increased fluctuations in entropy and density. Near atmospheric pressure, the temperature on the Widom line is -45 C. If the pressure inside the ice and its temperature turn out to be close to the line of coexistence of LDL and HDL, then liquid inhomogeneities can become a source of mechanical instability of the medium due to the growth of fluctuations in the energy of molecules and destruction of the ice structure. Such conditions can occur at temperatures below -45 C and pressures above 100 MPa.


2021 ◽  
Vol 155 (5) ◽  
pp. 054502
Author(s):  
Laura Lupi ◽  
Benjamín Vázquez Ramírez ◽  
Paola Gallo

2014 ◽  
Vol 90 (6) ◽  
Author(s):  
Rashid V. Williams-García ◽  
Mark Moore ◽  
John M. Beggs ◽  
Gerardo Ortiz
Keyword(s):  

2013 ◽  
Vol 139 (20) ◽  
pp. 204503 ◽  
Author(s):  
P. Gallo ◽  
D. Corradini ◽  
M. Rovere
Keyword(s):  

2018 ◽  
Vol 115 (38) ◽  
pp. 9444-9449 ◽  
Author(s):  
Rui Shi ◽  
John Russo ◽  
Hajime Tanaka

Liquids can be broadly classified into two categories, fragile and strong ones, depending on how their dynamical properties change with temperature. The dynamics of a strong liquid obey the Arrhenius law, whereas the fragile one displays a super-Arrhenius law, with a much steeper slowing down upon cooling. Recently, however, it was discovered that many materials such as water, oxides, and metals do not obey this simple classification, apparently exhibiting a fragile-to-strong transition far above Tg. Such a transition is particularly well known for water, and it is now regarded as one of water’s most important anomalies. This phenomenon has been attributed to either an unusual glass transition behavior or the crossing of a Widom line emanating from a liquid–liquid critical point. Here by computer simulations of two popular water models and through analyses of experimental data, we show that the emergent fragile-to-strong transition is actually a crossover between two Arrhenius regimes with different activation energies, which can be naturally explained by a two-state description of the dynamics. Our finding provides insight into the fragile-to-strong transition observed in a wide class of materials.


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