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The freezing of water into ice

Inside the deep freeze of a refrigerator, water easily transforms itself into ice without any difficulty. So it does in the upper atmosphere where the beautiful snowflakes form. The upper layers of water in the lakes in the arctic region freeze into ice sheets in winter. When the temperature is raised, the same ice transforms back into water without any difficulty. The freezing of water into ice and the reverse process of the melting of ice into water are common processes that we see are happening around us all the time. Ice formation is also known to occur in interstellar space. [Pg.305]

However, in experiments one finds that water droplets remain unfrozen till -40 °C. Water has proven to be notoriously difficult to freeze in computer simulations, where long runs and either slightly lower density or modified potential models [Pg.305]

It is well known that the volume of ice is greater than that of water by about 8%. F or most liquids the density increases on transforming the liquid to ice, as the solid is usually denser than the liquid. This clearly shows that ice is more stmctured and has more open space in its molecular arrangement. The volume expansion of water upon freezing is an anomalous behavior because volume decreases upon freezing for other simple liquids. It is this very anomaly by which fish can survive in low-temperature regions because ice floats on the upper layer of the lake and the lower layer of the lake still contains liquid water which is of higher density. [Pg.306]


Note In equilibrium statistical mechanics, one says that a first-order phase transition occurs at r = r. . For this value of r, there is equal probability of finding the system in the state corresponding to any of the three minima. The freezing of water into ice is the most familiar example of a first-order phase transition.)... [Pg.84]

However, it was not possible, till very recently, to learn about the mechanism of the freezing of water into ice from computer simulations because water just would not freeze into ice in the computer That is, the freezing of liquid water is not as simple as one would imagine This completely agrees with the early experiments of Speedy and Angell. But the reason is not clearly understood even today That is, even the apparently simple process of forming ice eludes us ... [Pg.308]

Perhaps the first demonstration of the freezing of water into ice in computer simulation was observed by Matsumoto et al. [6,7]. These authors simulated many... [Pg.310]

It should be clear from the above that because of sustained efforts over many decades, significant progress has now been achieved in the understanding of the freezing of water into ice. However, there stiU remain many unsolved problems in this area. For example, we do not yet have a quantitative theory of the nucleation of ice in supercooled water. The molecular models we use in simulations are perhaps too primitive, as most of them do not include the polarizabihty of water molecules. The polarizability of water is large due to the two lone pairs of electrons on the lone oxygen atom. Perhaps one would need to consider quantum simulations to fully understand the freezing of ice. [Pg.315]

Case (iii). The lower left quadrant, where AH < 0, A5 < 0, is favorable only when the temperature is low enough, so that T < AH/AS. Examples are condensation of steam into water, freezing of water into ice, monomers polymerizing into polymers, CO2 absorbs into CaO. [Pg.123]

Freezing involves different factors in the conversion of water into ice thermodynamic factors that define the position of the system under equilibrium conditions, and kinetic factors that describe the rates at which equilibrium might be approached. The freezing process includes two main stages the formation of ice crystals (nucleation), and the subsequent increase in crystal size (growth). [Pg.310]

The freezing of water into crystalline ice presents another highly interesting problem. Pure water, when broken into small droplets, remains in... [Pg.305]

Even though this process is endothermic, it is spontaneous at temperatures above the freezing point of water (0 C). The reverse process, the freezing of water to ice, is spontaneous at temperatures below 0°C. Thus, we know that ice at room temperature wUl melt and that water put into a freezer at —20 C will turn into ice both of these processes are spontaneous even though they are the reverse of one another. In Chapter 19 we will address the spontaneity of processes more fully. We will see why a process can be spontaneous at one temperature, but not at another, as is the case for the conversion of water to ice. [Pg.168]

The freeze concentration process is based on the partial solidification of water into ice in a fluid food product followed by the removal of the solid ice phase from the concentrated liquid phase. This process has some inherent advantages over evaporation and reverse osmosis for concentrating fluid foods as well as other process streams (1). One advantage is that essentially none... [Pg.316]

After insertion of one emulsion-filled cell into the calorimeter, and thermal equilibrium has been reached, the calorimeter is programmed to be cooled down and heated between two limits of temperature. As the test is especially suitable for W/0 emulsions, focus is placed on the freezing of water and the melting of ice. Therefore, the scanning is performed from +20°C down to -80°C at least, as late solidification, due to undercooling and dissolved solute in water, may occur. The other cells left at room temperature are studied in the same way. [Pg.331]

V, 36 Experiments on the Production of Air by the Freezing of Water air is formed from melting ice, hence it is not dissolved air water converted into vapour forms phlogisticated air. ... [Pg.159]

When concrete structures are subjected to variations of temperature below zero and to the freezing of water solutions in the pore system, then exposure to destructive processes of the cement-based matrices is serious. An increase in the volume of water in the pores when it is transformed into ice is approximately 9% and it may produce important internal stresses, inducing cracks and spallings. This is particularly dangerous in the following situations ... [Pg.402]


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