  The structural dynamics of ice in the freezing - thawing process has been
studied in the context of the concept of two-phase water. It was previously
shown that water is a two-phase system consisting of free and bound (liquid
crystal) fractions. Bound water is represented by hydrated shells of sodium
chloride microcrystals, which are constantly present in water and are visible
in the optical microscope as a dispersed phase. With rapid freezing, free water
crystallizes, turning into ice with the inclusion of the dispersed phase. At
this stage, xenogenic air bubbles are released. When ice melts, multiple small
bubbles form from diffusely dissolved air. At the same time, the ice acquires a
characteristic cellular structure. Bubbles grow, merge and form variegated air
channels that contribute to the release of air into the melt water. The
dispersed phase during the freezing of water under the conditions of our
experiment did not show external signs of glaciation. However, when ice melted,
a part of this fraction was kneaded from the main volume of water in the form
of loose flakes. The loss of water of part of the microdispersed phase and most
of the gases causes a change in a number of physical properties of the melt
water. Possible involvement of the observed processes in the appearance of
"snowballs" on the banks of rivers is discussed.
