For description of erosion processes the method of thermodynamic potentials was used. The thermodynamic potential of Gibbs is more suitable for this purpose, because it is possible to develop mechanisms for experimental measurement of independent variables being parts of a corresponding differential equation. It was shown that the potential of erosion resistance is an additive and constant for specific soil, expressing its properties, i.e. may be taken as a common integral criterion of the estimation of erosion resistance of soils.
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