Commit Graph

7 Commits

Author SHA1 Message Date
Bård Skaflestad
6c5ed7b8ff Add a layer of glue to extract data from deck
This is a work in progress.
2018-01-02 14:28:06 +01:00
Bård Skaflestad
17e93c5cce Install crude handling of data point outside vertical span
The initial implementation of RK4IVP<>::operator() failed to take
into account the possibility that we might need to evaluate the
function outside the vertical span for which it was initially
defined.  This situation occurs, for instance, in the not uncommon
cases of the GOC being above or the WOC being below the model.

This commit installs a crude Hermitian extrapolation procedure to
handle these cases.  Refinements are likely.
2018-01-02 14:28:06 +01:00
Bård Skaflestad
b21d3734db Document requirements of CellRange. 2018-01-02 14:28:06 +01:00
Bård Skaflestad
db2a21442c Document public interface of phasePressures(). 2018-01-02 14:28:06 +01:00
Bård Skaflestad
0ce1e96a00 Add reverse look-up mapping for region vectors
Class RegionMapping<> provides an easy way of extracting the cells
that belong to any identified region (e.g., as defined by EQLNUM) of
the deck.
2018-01-02 14:28:06 +01:00
Bård Skaflestad
4c63659b61 Compute phase pressures in subset of cells
This commit adds support for assigning the initial phase pressure
distribution to a subset of the total grid cells.  This is needed in
order to fully support equilibration regions.  The existing region
support (template parameter 'Region' in function 'phasePressures()')
was only used/needed to define PVT property (specifically, the fluid
phase density) calculator pertaining to a particular equilibration
region.
2018-01-02 14:28:06 +01:00
Bård Skaflestad
5ec0aec02e Add basic equilibration facility
This commit adds a simple facility for calculating initial phase
pressures assuming stationary conditions, a known reference pressure
in the oil zone as well as the depth and capillary pressures at the
water-oil and gas-oil contacts.

Function 'Opm::equil::phasePressures()' uses a simple ODE/IVP-based
approach, solved using the traditional RK4 method with constant step
sizes, to derive the required pressure values.  Specifically, we
solve the ODE

      dp/dz = rho(z,p) * g

with 'z' represening depth, 'p' being a phase pressure and 'rho' the
associate phase density.  Finally, 'g' is the acceleration of
gravity.  We assume that we can calculate phase densities, e.g.,
from table look-up.  This assumption holds in the case of an ECLIPSE
input deck.

Using RK4 with constant step sizes is a limitation of this
implementation.  This, basically, assumes that the phase densities
varies only smoothly with depth and pressure (at reservoir
conditions).
2018-01-02 14:28:06 +01:00