The transport of NaCl and ethanol through the microbial cellulose membrane was used as a generator of layers with density gradients, parallel to gravity vector. Changes in NaCl concentrations connected with density gradients in these layers were monitored by means of Ag|AgCl electrodes dipped directly into aqueous NaCl solutions with or without ethanol. The parameters used in this article and characterizing diffusive or diffusiveconvective processes in layers are the ratio of NaCl concentrations at electrode surfaces (C i =C e ) calculated for voltage which was measured 6 h after rebuilding of layers with density gradients, and time of appearance of hydrodynamic instabilities in the membrane system. The C i =C e is the nonlinear function of initial ratio of NaCl on the membrane (C h =C l ), with maximum concentration at initial moment dependent on ethanol and configuration of the membrane system. The time of appearance of hydrodynamic instabilities in layers with density gradients parallel and directed opposite to the gravity vector depends on C h =C l , ethanol concentration, and configuration of the membrane system. Besides, for aqueous NaCl solutions, critical values of density gradients and thicknesses of layers needed This work was supported by KNW-1-086/10. 78 S. Grzegorczyn et al. for the appearance of hydrodynamic instabilities were calculated and presented as functions of C h =C l .