Abstract
The special contribution of matter lying in and around phase boundaries to the total energy of heterogeneous systems is normally ignored in thermodynamic treatises. This neglect implies that the density of energy of a given phase remains uniform up to a mathematical surface separating it from contiguous phases. However, because of the finite, although short, range of action of atomic forces, the assumed sharp phase boundaries should actually be replaced by an interphasal region of finite thickness across which the density of energy or of any other thermodynamic property changes much less abruptly. It is reasonable to expect the normal thickness of this transition region to be of the order of a few molecular diameters ; unless the system has a relatively high surface to volume ratio, as would be the case in colloidal systems, the additional contribution of the “surface” atoms to the total energy content may justifiably be ignored.
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de Bruyn, P.L. (1966). Some Aspects of Classical Surface Thermodynamics. In: Bonis, L.J., de Bruyn, P.L., Duga, J.J. (eds) Surface Phenomena. Fundamental Phenomena in the Materials Sciences. Springer, Boston, MA. https://doi.org/10.1007/978-1-4899-6347-5_1
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