Page 125 - Introduction to Transfer Phenomena in PEM Fuel Cells
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114     Introduction to Transfer Phenomena in PEM Fuel Cells
                                                                 
                             The average  rate of the fluid phase  u  is given as a function of the
                           pressure and potential gradients, in the macroscopic multidimensional case
                           by the Schlögl equation.  In addition to the Darcy term for the pressure
                           gradient, there is a term that translates the effects of an electrical potential
                           gradient on the charged solution (water + protons). This is known as electro-
                           osmosis:
                                      K      K            
                                 u =−    p  ∇ P −  E  ⋅ C ⋅ ⋅∇ϕ                          [3.62]
                                                        F
                                        μ    b   μ    f
                           where:
                                
                                                               –1
                             –  u  is the average flow rate, in (m.s );
                                                                          –1
                                                                       –1
                             – μ is the dynamic viscosity of water, in (kg .m .s );
                             – φ is the macroscopic electric potential, in (V);
                                                                         –3
                             – C  is the fixed charge concentration, in (mol.m );
                                 f
                             – P b is the pressure of the liquid water in the pore, in (Pa);
                             – K p and K E are respectively the hydraulic and electrokinetic
                                                                         2
                           permeabilities, in Darcy (D) with (1D = 0.97 .10 –12  m ).
                             For the transport of ions in the membrane, the protons migrate by
                           convection (overall  movement of the  solution) and by diffusion under the
                                                                       ~
                           effect of an  electrochemical potential  gradient ( μ  ). At the  microscopic
                                                                        H  +
                           scale, the Nernst–Planck relationship is used to determine the proton flow
                           ( N  ):
                              H  +
                                                        
                                             −
                                 N  + =  c  + ⋅  u D  +  ⋅∇μ −  +                        [3.63]
                                  H     H       H ,H O    H
                                                    2
                           where:

                             –  D  +    is the effective diffusion coefficient (protons in water) of the
                                 H,H O
                                     2
                                                       –1
                           pores of the membrane, in (m².s );
                                                                     –3
                             – c  +  is the proton concentration, in (mol.m );
                                H
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