Page tree

Versions Compared

Key

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

...

Small deviations of ambient pressure 

LaTeX Math Inline
bodyp(t, {\bf r})
 from initial pressure fromarion formation 
LaTeX Math Inline
bodyp_0(t, {\bf r})
 lead to the exponential changes in permeabilityporosity:

LaTeX Math Block
anchorCPHWYYZKOW
alignmentleft
k=k_0 \, e^{\beta_pn_k \cdot c_r (p-p_0)}

where 

LaTeX Math Inline
bodyc_r
 is formation compressibility
LaTeX Math Inline
bodyk_0
 is permeability at reference pressure 
LaTeX Math Inline
bodyp_0
 (usually picked up at initial reservoir pressure 
LaTeX Math Inline
bodyp_0 = p_i
 ),
LaTeX Math Inline
bodyn_k
 is power degree of permeability-porosity correlation:

LaTeX Math Block
anchorkphi
alignmentleft
k = k_0 \left( \frac{\phi}{\phi_0}   \right)^{n_k}


The above correlation assumes constant reservoir compressibility which in most practical applications holds true in a wide range of pressure variations all the way down to porosity cut-off and all the way up to the fracture point.


The substantial reduction of formation pressure leads to shrinking a lot of pore throats and massive reduction in permeability deviating from exponential.

...