NIP (model theory)

The Fowler–Yang equations for pressure solution and viscous compaction in sedimentary basins can be written as:

$\frac{\partial \varphi }{\partial t}=\frac{\partial }{\partial z}[(1-\varphi )u],$

$u=\lambda {\varphi }^m[\frac{{\partial }^{2}u}{\partial z^2}-(1-\varphi )],$

where u is the Darcy velocity and $\varphi$ is the porosity of the porous media. In addition, 0 < λ < 10⁵ is a constant, and while m = 8. This system is highly nonlinear, which can explain the transition from one behaviour to another in pressure solution.

References

43 year old Petroleum Engineer Harry from Deep River, usually spends time with hobbies and interests like renting movies, property developers in singapore new condominium and vehicle racing. Constantly enjoys going to destinations like Camino Real de Tierra Adentro.