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160  7  Simulating Thermal and Chemical Effects of Intruded Magma Solidification Problems
                                  1          4
                    m                                      m
                   X = 0.5 +             ln              (X > 0.5)       (7.10)
                    w               2667     mf            w
                              6.25 −        k w
                                     T
                                                                          mf
                   m
            where X is the mole fraction of H 2 O in the NaAlSi 3 O 8 melt; T is in Kelvin; k w is
                   w
            the equilibrium constant for H 2 O in melts of feldspar composition.
                 mf                     −8  2         −4
              ln k  = 5 + (ln P)(4.481 × 10 T − 1.51 × 10 T − 1.137)
                 w
                                       −8
                                          2
                                                      −5
                                                                     −2
                            2
                     + (ln P) (1.831 × 10 T − 4.882 × 10 T + 4.656 × 10 )
                                                                         (7.11)
                              −3
                                                 −4
                                     3
                                                        4
                                                                    −3
                     + 7.8 × 10 (ln P) − 5.012 × 10 (ln P) + 4.754 × 10 T
                                    2
                                −6
                     − 1.621 × 10 T ,
            where P is the pressure of the intruded magma; P and T are in bars and Kelvin,
            respectively.
              Using the concept of molar mass, the mass source of the volatile fluids released
            during solidification from the intruded magma can be expressed as
                                                 m
                                               X W  w m
                                                 w
                                     X W      (1 − X )W
                        Q(x, y, t) =    m  m        m  m         ,       (7.12)
                                       w  w        w   albite
                                            +                Δt Mk
                                       ρ m        ρ m
                                        w          albite
            where Δt Mk is the time period required to complete the magma solidification within
            a given solidification thickness ΔL Mk ; W  m  and ρ  m  are the molar mass and den-
                                              w      w
            sity of the volatile fluids in the magma; W m  and ρ m  are the molecular mass
                                              albite   albite
            and density of the albite (NaAlSi 3 O 8 ) melt. It is noted that using the definition in
            Eq. (7.12), the mass source of the released volatile fluids has units of the density of
            the albite (NaAlSi 3 O 8 ) melt divided by time.
              In the case of the intruded magma temperature being equal to the solidification
            magma temperature, Eq. (7.8) can be rewritten as

                                                ∂x I    ∂y
                                                          I
                                         ρ M L n x  + n y
                                                 ∂t      ∂t
                             f (x, y, t) =                   .           (7.13)
                                                ΔL Mk
            7.2 Implementation of the Equivalent Source Algorithm
                in the Finite Element Analysis with Fixed Meshes
            If the physically equivalent heat source term, f (x, y, t), is determined either ana-
            lytically or experimentally, Eqs. (7.6) and (7.7) can be directly solved using the
            conventional finite element method (Zienkiewicz 1977). For dike-like and sill-like
            intruded magmas, the physically equivalent heat source due to the solidification can
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