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The results of numerical studies of condensation on the surface of the air component of atmospheric condensation nuclei of various shapes. Mathematical modeling performed at ambient temperatures typical of summer and winter seasons. It is found that the trajectory of motion of particles of various shapes differ significantly. Numerical studies were carried out at atmospheric parameters corresponding airspace adjacent to the areas of the TPP. Testing results obtained audited conservative difference scheme

The influence of the form of condensation nucleus on the formation and propagation of acid precipitation near operating TPS