Analytic Solutions and Entropy Production Of the Double Diffusive Equation System

We investigate the partial differential equation system which describes the double-diffusion convection phenomena with the reduction formalism. Double-diffusion means when two scalar quantities with different diffusivity, such as heat and solute concentration, contribute to density gradients within a fluid under the influence of gravity. The time-dependent self-similar trial function is applied and analytic results are presented for the dynamical variables and analyzed in details. Additionally, the entropy production was derived as well. In the second part of the study we investigate the role of an additional heat source.