Page tree

Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.

...

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


and use Then use the following equality:

LaTeX Math Block

...

anchorrhophi

...

alignmentleft
d(\rho \, \phi) = \rho \, d \phi + \phi \, d\rho = \rho \, \phi \, \left( \frac{d \phi }{\phi} +  \frac{d \rho }{\rho}  \right) 
= \rho \, \phi \, \left( \frac{1}{\phi} \frac{d \phi}{dp} \, dp +  \frac{1}{\rho} \frac{d \rho}{dp} \, dp  \right) 
= \rho \, \phi \, (c_{\phi} \, dp + c \, dp) = \rho \, \phi \, c_t \, dp

to pageDerivation of Linear pressure diffusion @model to arrive at:

LaTeX Math Block
anchorS8TNB
alignmentleft
\rho \, \phi \, c_t  \cdot \frac{\partial (p)}{\partial t} + \nabla \, ( \rho \, {\bf u}) = 0
LaTeX Math Block
anchorqk
alignmentleft
\int_{\Sigma_k} \, {\bf u} \,  d {\bf A} = q_k(t)

where

LaTeX Math Inline
bodyc_t = с_\phi+ c


Let's assume Darcy flow with constant permeability 

LaTeX Math Inline
body--uriencoded--\displaystyle \frac%7Bdk%7D%7Bdp%7D = 0
and ignore gravity forces:

...

LaTeX Math Block
anchorS8TNB
alignmentleft
\rho \, \phi \, c_t  \cdot \frac{\partial p}{\partial t} + \nabla \, ( k \cdot \frac{\rho}{\mu} \, \nabla  \, p) = 0
LaTeX Math Block
anchorqk
alignmentleft
\frac{k}{\mu} \cdot \int_{\Sigma_k} \,  {\bf \nabla p} \, p \cdot  d {\bf A} = q_k(t)

Let's express the density via Z-factor:

...

LaTeX Math Block
anchorS8TNB
alignmentleft
 \phi \, c_t \, \mu  \cdot \frac{p}{\mu \, Z} \cdot \frac{\partial p}{\partial t} + \nabla \, ( k \cdot \frac{p}{\mu \, Z} \, \nabla  \, p) = 0
LaTeX Math Block
anchorqk
alignmentleft
\frac{k}{\mu} \cdot \int_{\Sigma_k} \, {\bf p\nabla } \, p \cdot   d {\bf A} = q_k(t)

or

LaTeX Math Block
anchorprePZ
alignmentleft
\phi \, c_t \, \mu   \cdot \frac{\partial \Psi}{\partial t} + \nabla \, ( k \cdot \nabla  \, \Psi) = 0
LaTeX Math Block
anchorqk
alignmentleft
\frac{k}{\mu} \cdot \int_{\Sigma_k} \, {\bf p\nabla } \, p \cdot   d {\bf A} = q_k(t)

where

LaTeX Math Inline
body--uriencoded--\displaystyle \Psi(p) =2 \, \int_0%5ep \frac%7Bp \, dp%7D%7B\mu(p) \, Z(p)%7D

Pseudo-Pressure

...

LaTeX Math Block
anchortau
alignmentleft
\tau(t) = \int_0^t \frac{dt}{\mu (p_{BHP}(t )) \, c_t (p_{BHP}) } \, , \ \  p_{BHP} = p_{BHP}(t))}
 

to correct early-time transient  behaviour .which turn equation

LaTeX Math Block Reference
anchorprePZ
 into:

LaTeX Math Block
anchorDD3EH
alignmentleft
\phi  \cdot \frac{\partial \Psi}{\partial \tau} + \nabla \, ( k \cdot \nabla  \, \Psi) = 0



See also

...

Physics / Mechanics / Continuum mechanics / Fluid Mechanics / Fluid Dynamics / Pressure Diffusion / Pressure Diffusion @model / Pseudo-linear pressure diffusion @model

...