changes.mady.by.user Arthur Aslanyan (Nafta College)
Saved on Nov 10, 2021
\frac{\partial (\rho_A \, \phi) }{\partial t} + \nabla (\rho_A \, {\bf u}_A) = 0
\int_V \, \frac{\partial (\rho_A \, \phi) }{\partial t} \, dV = - \int_V \, \nabla (\rho_A \, {\bf u}_A) \, dV = - \int_{\partial V} \, \rho \, {\bf u}_A \, d {\bf A}
V \cdot (\rho_A \, \phi) = \delta \, m_A
V \cdot \left( \phi \, \sum_\alpha \rho_{A,\alpha} \, s_\alpha \right) = \mathring{\rho}_A \cdot \delta \, m q_A \rightarrow \left( \phi \, \sum_\alpha \frac{\rho_{A,\alpha}}{\mathring{\rho}_A} \, s_\alpha \right) = V^{-1} \cdot \delta \, q_A
effective porosity as function of formation pressure LaTeX Math Inlinebodyp(t)
cumulative gas influx from Gas Cap Expansion
cumulative water influx from Aquifer Expansion
normalized cross-phase exchange derivatives as functions of reservoir pressure
...