Abstract: | Solutions are found for the stationary and nonstationary equations of convective diffusion on the basis of an experimentally detected hydrodynamic flow picture of an ideal fluid. The agreement between the results of boundary-layer soundings, obtained by different methods, is shown.Translated from Inzhenerno-Fizicheskii Zhurnal, Vol. 32, No. 4, pp. 674–682, April, 1977. |