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44 CHAPTER 2
















                               Fig.  2.10.  Schematic diagram to
                               show that  in  liquid  water there  are
                               networks of associated water mole-
                               cules and also a certain fraction of
                               free, unassociated water molecules.


            atoms, such as Cl, F, O, and S when they are in solution. There is nothing mysterious
            about the energy behind H bonding; it derives from the positive charge on the proton
            and the negative one on   for example.
                                                                             –1
               However, H bonding (the value of the bond strength is small, only 10–40 kJ mol )
            does affect the properties of water and is responsible for water’s anomalously high
            boiling point. If one extrapolates the boiling points of the hydrides of the elements in
            group VI of the Periodic Table to the expected value for the hydride of O, it turns out
            to be ~ 215 K. The fact that it is actually 158 K higher than that is undoubtedly because
            individual water molecules are not free to evaporate as the temperature is increased.
            Many of them bond to each other through the H bonds. The thermal stability of water
            has had an important effect on the structure of the earth, for if there were no H bonds,
            the seas would never have formed (they would have remained in the vapor phase) and
            it is doubtful if life would have begun.
                Structural research on water, which originated in a classic paper by Bernal and
            Fowler, has shown that under most conditions liquid water is best described as a rather
            broken-down, slightly expanded (Table 2.3) form of the ice lattice (Fig. 2.8). Thus,
            X-ray and other techniques indicate that in water there is a considerable degree of
            short-range order that is characteristic of the tetrahedral bonding in ice. Thus, liquid
            water partly retains the tetrahedral bonding and resulting network structure charac-
            teristic of crystalline ice. In addition to the water molecules that are part of the network,
            some structurally  free,  nonassociated water molecules can be present in  interstitial
            regions of the network (Fig. 2.10). When a network water molecule breaks its hydrogen
            bonds with the network, it can move as an interstitial water molecule that can rotate
            freely.  The classification of  the water  molecules into  network water  and  free (or
            interstitial) water is not a static one. It is dynamic. As argued in a classic paper by
            Frank and Wen, clusters of water molecules cooperate to form networks and at the
            same time the networks can break down. A water molecule may be free in an interstitial
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