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LaTeX Math Block
anchorPZ1
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\phi \cdot c_t \cdot \partial_t p + \nabla  {\bf u}  
+ c \cdot ( {\bf u} \, \nabla p)
= 0



LaTeX Math Block
anchoruu1
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{\bf u} = - M \cdot ( \nabla p - \rho \, {\bf g})



LaTeX Math Block
anchorqk
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\int_{\Sigma_k} \, {\bf u} \,  d {\bf A\Sigma} = q_k(t)


where

LaTeX Math Inline
body\Sigma_k

well-reservoir contact of the 

LaTeX Math Inline
bodyk
-th well

LaTeX Math Inline
body--uriencoded--d %7B\bf \Sigma%7D

normal vector of differential area on the well-reservoir contact, pointing inside wellbore


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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