Page 132 - Introduction to Transfer Phenomena in PEM Fuel Cells
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generally evaluated experimentally. These coefficients, difficult to evaluate,
                           largely determine the transport of water in the membrane.
                           3.6.5. Parametric laws                     Mass Transfer Phenomena     121
                           3.6.5.1. Water content

                             The diffusion coefficient of water in the membrane ( D m  ) strongly
                                                                                   H 2 O
                           depends on the local water content, which is defined as the ratio between the
                           number of water molecules and the number of sulfonic sites (SO 3) available
                           in the polymer. The following descriptions involve the water content of the
                           membrane (λ). This variable represents the number of water molecules per
                           active site (SO 3):

                                    n
                                 λ=  HO                                                  [3.80]
                                       2
                                    n   −
                                     SO 3
                             In addition, electroneutrality imposes an equal number of  positive
                           charges (protons) and negative charges (active sites). The ratio of water
                           molecules to active sites then reflects the potential number  of water
                           molecules in the vicinity of each proton. The water content can also be
                                                                              1
                           defined according to the equivalent mass (EW) in (g mol SO 3), the density of
                                                                –3
                           the dry membrane ( dry) expressed in (g.m ), and the water concentration in
                           the membrane ( c  ):
                                          H 2 O
                                    EW
                                 λ=      c ⋅                                             [3.81]
                                    ρ dry  HO
                                           2

                             In practice, the value of (λ) varies between 2 and 22.

                             In this relation, we neglect the variation of volume related to the variation
                           of concentration in water. The variable (λ) is commonly used in the literature
                           because it  makes it possible to determine the  hydration state of the
                           membrane with respect to a controlled parameter, the number of active sites.
                           The water content can also be expressed using the coefficient of water
                           activity as follows:
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