GeoScale - Direct Reservoir Simulation on Geocellular Models

Fast Flow Simulations by Optimal Reordering and Discontinuous Galerkin Discretisations

Fast, accurate, and robust solution of advection dominated transport equations

  • time-of-flight and single-phase tracer flow
  • multiphase and multicomponent flow

A grid-based alternative to streamline simulation that is mass-conservative and avoids problems with mapping and choice of representative streamline distribution.

Basic Ideas

  • reordering of equations for efficient element-wise or blockwise solution of the resulting (non)linear discrete systems
  • local control of nonlinear iterations reduces runtime dramatically and increases the range of feasible time-steps
  • discontinuous Galerkin spatial discretisation for compact higher-order discretisations of purely advective transport equations

Features

The reordering procedure is applicable to any grid that can be mapped to a directed graph (with directions given by inter-cell fluxes). Based on the reordering, one can formulate a highly efficient Gauss-Seidel type (non)linear solver.  Applications studied so far: 

  • fast computation of time-of-flight in grid cells; isocontours of time-of-flight are the natural time-lines in the reservoir and thus ideal for fast visualisation of flow patterns
  • fast computation of tracer flow; isocontours of tracer concentrations can be used for delineation of reservoir volumes and computation of drainage/flooded volumes
  • fast simulation of multiphase flow in the absence of gravity and capillary forces. Example: For the SPE10 model with 1,1 million cells,  runtime for 100 time steps with the implicit single-point upwind method was about 2 minutes on a standard PC.

The discontinuous Galerkin discretisation:

  • gives increased spatial accuracy through higher-order stencils localised to a single grid cell
  • allows for local hp-refinement
  • reduces grid-orientation problems for miscible flows

Advantages

A fast grid-based alternative to streamline simulation that

  • avoids mapping and choice of representative streamline distribution
  • avoids problems associated with calculation of production curves
  • is guaranteed to be mass conservative

References:

  1. J. R. Natvig and K.-A. Lie. On efficient implicit upwind schemes.  Proceedings of ECMOR XI, Bergen, Norway, 8-11 September 2008. 
  2. J. R. Natvig and K.-A. Lie. Fast computation of multiphase flow in porous media by implicit discontinuous Galerkin schemes with optimal ordering of elements. J. Comput. Phys, Volume 227, Issue 24, pp. 10108-10124, 2008. DOI: doi:10.1016/j.jcp.2008.08.024.
  3. J. R. Natvig, K.-A. Lie, B. Eikemo, and I. Berre. A discontinous Galerkin method for single-phase flow in porous media. Advances in Water Resources, Vol. 30, Issue 12, December 2007, pp. 2424-2438. DOI: 10.1016/j.advwatres.2007.05.015.

Isocontours of time-of-flight define natural timelines in the reservoir, here visualized in a half slice of a 3D quarter five-spot with heterogeneous permeability.

 


Drainage volumes for the SPE 10 model defined by computing the steady-state solution of a continuous tracer injection.

 


Localization of nonlinear iteration by use of reordering. The color shows the number of iterations per cell during a typical transport step. Compared with a standard Newton-Raphson method this gives 100 times reduction of runtime for this model.


Published September 17, 2009

A portfolio of strategic research projects funded by the Research Council of Norway