Ice Adhesion. Группа авторов

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end of the First Industrial Revolution also saw the introduction of another artificial refrigeration concept: thermoelectrics. French watch dealer-turned physicist Jean Charles Athanase Peltier described in his 1834 paper “Nouvelles Expérences sur la Caloricité des Courans Électriques” [New Experiments on the Heat Effects of Electric Currents] that passing a current through bimetallic circuits caused the absorption of heat at one of the metal junctions and rejection of heat at the other. When Peltier welded bismuth with antimony, the semiconductor yielded a temperature of -45°C [50]. In 1838 physicist Emil Lenz used the same bismuth-antimony junction in his experimental apparatus to freeze water when current was applied in one direction, and melt the ice when current was reversed [51]. Almost simultaneously to the work of Peltier and Lenz, German medical doctor and physicist Thomas Johann Seebeck described how bimetallic circuits would deflect the needle of a compass when the circuit’s junctions were held at different temperatures [52]. Danish physicist Hans Christian Ørsted connected Seebeck’s work with his own on the relationship between current and magnetism and realized that the temperature difference between the junctions produces a voltage, driving an electric current [53]. We now call these two thermoelectric effects the “Peltier-Seebeck effect”, connoting that they are converse manifestations of the same physical process. The Seebeck portion of the effect forms the basis of the working principle for thermocouples, the temperature measurement devices which have become indispensable in rigorous surface icing research, and indeed in scientific research as a whole [54]. The Peltier effect gained considerable attention in the 1950’s after Abram Ioffe demonstrated the increased thermoelectric effect possessed by doped semiconductors [55]. It was theorized that thermoelectric cooling could surpass vapour-compression technology for domestic refrigeration. This time of frenzied semiconductor research culminated in H. Julian Goldsmid’s discovery of Bi2Te3-Sb2Te3 as the material with the highest thermoelectric effect [56]. Even so, bismuth-telluride alloys only produce moderate amounts of cooling compared to vapour-compression refrigerators. Nonetheless, the Peltier plate has become widely used in surface icing experimentation as it offers researchers high reliability and control over temperatures [57].

      As can be seen from the previous discussion of man’s attempts at researching and combatting surface ice formation, the implemented solutions have been rather active solutions, necessitating reapplication for continued effect. Contrarily, research since the turn of the 21st century has aspired toward anti-icing/icephobic materials which offer a passive method of keeping a surface free of ice. In the next section we outline an important 20th century concept which was omitted from the previous historical discussion, the Classical Nucleation Theory (CNT). CNT has re-emerged with the introduction of new nano-scale manufacturing techniques as a way to rationally design surfaces which thermodynamically inhibit the formation of ice.

      The Classical Nucleation Theory (CNT) arose from the work of German chemists Volmer and Weber in 1926 in which they estimated the rate of the condensation of over-saturated vapours to liquid, as a function of the degree of over-saturation [68]. Becker and Döring furthered this research in 1935 when they noted that the condensation process has a certain activation energy that must be overcome for the new phase to form [69]. Finally, the homogeneous CNT was completed in 1939 when Frenkel made the important conclusion that the Volmer-Weber/Becker-Döring condensation model also applies to systems which are not over-saturated. Frenkel correctly hypothesized that even under-saturated solutions have a steady-state distribution of small-sized clusters due to continuous nucleation and decay of unstable clusters [70].

      1.2.1 Homogeneous Classical Nucleation Theory

      where ∆GIW(T) and γIW(T) denote the free energy difference between ice and water (per unit volume) and the interfacial energy

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