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LaTeX Math Block
anchorPZ_singlephase
alignmentleft
\phi \cdot c_t \cdot \partial_t p -   \nabla  \left( M \cdot ( \nabla p - \rho \cdot \mathbf{g} )   \right)  - c \cdot M \cdot (\nabla p)^2  = \sum_k q({\bf r}) \cdot \delta({\bf r}-{\bf r}_k)


The alternative form is:

LaTeX Math Block
anchorXSQUE
alignmentleft
\phi \cdot c_t \cdot \mu \cdot \partial_t \Psi -   
 \nabla \cdot \left( k \cdot  ( \vec \nabla \Psi  - \frac{\rho^2}{\mu}  \, {\bf g} )  \right) 
  = \sum_k q({\bf r}) \cdot \delta({\bf r}-{\bf r}_k)


Physical models of pressure diffusion can be split into two categories: Newtonian and Rheological (non-Newtonian) based on the fluid stress model.

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