Accumulation Terms

The general form of the mass accumulation term that includes equilibrium sorption on the solid grains is:

Mκ=φβSβρβXβκ+(1φ)ρRρlXlκKdM^\kappa\quad=\quad\varphi\sum_{\beta}{S_\beta\rho_\beta X_\beta^\kappa}+(1-\varphi)\rho_R\rho_lX_l^\kappa K_d (4-2)

where φ\varphi is porosity, SβS_\betais the saturation of phase β\beta (e.g., β\beta = gas, aqueous, non-aqueous phase liquid/oil), ρβ\rho_\betais the density of phase β\beta, and XβκX_\beta^\kappais the mass fraction of component k in phase β\beta, ρR\rho_Ris the rock grain density, and KdK_d is the aqueous (liquid) phase distribution coefficient. The total mass of component k is obtained by summing over the fluid phases β\beta. The heat accumulation term in a multiphase system is

Mh=(1φ)ρRCRT+φβSβρβuβM^h\quad=\quad(1-\varphi)\rho_RC_RT+\varphi \sum _\beta S_βρ_βu_β (4-3)

where CRC_Ris the specific heat of the rock grains, T is temperature, and uβu_\betais the specific internal energy of phase β\beta.

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