Geologic fault representation for flow simulation

1. A method comprising:

mapping a stairstepped grid to a surface wherein the stairstepped grid and the surface represent a discontinuity in a geologic environment, wherein the stairstepped grid comprises cuboid shaped grid cells and wherein the mapping accounts for spatial discrepancies between the stairstepped grid and the surface;

based at least in part on the mapping, for adjacent cuboid shaped grid cells that represent material on one side of the discontinuity and material on another side of the discontinuity, without reshaping the adjacent cuboid shaped grid cells, adjusting physical properties and adjusting connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface, wherein adjusting physical properties comprises adjusting permeability and wherein adjusting connectivity comprises adjusting transmissibility; and

simulating flow in the geologic environment using a flow simulator, the stairstepped grid to represent the discontinuity, the adjusted physical properties and the adjusted connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface to generate simulation results.

2. The method of claim 1 wherein adjusting connectivity comprises adjusting connectivity of a portion of the stairstepped grid on the one side of the discontinuity with respect to a portion of the stairstepped grid on the other side of the discontinuity.

3. The method of claim 1 wherein the discontinuity comprises a fault.

4. The method of claim 1 wherein the mapping comprises projecting nodes of the stairstepped grid to the surface.

5. The method of claim 1 comprising discretizing the surface.

6. The method of claim 5 wherein the discretizing comprises triangulating the surface to define a triangulated surface.

7. The method of claim 5 wherein the discretizing is based at least in part on the mapping.

8. The method of claim 4 comprising discretizing the surface based at least in part on locations of the nodes of the stairstepped grid as projected onto the surface.

9. The method of claim 1 comprising mapping the stairstepped grid to one side of the surface.

10. The method of claim 1 comprising mapping the stairstepped grid to two sides of the surface.

11. The method of claim 1 comprising adjusting transmissibility based at least in part on one or more of the adjusted physical properties.

12. A system comprising:

a processor;

memory operatively coupled to the processor; and

processor-executable instructions stored in the memory to instruct the system, the instructions comprising instructions to:

map a stairstepped grid to a surface wherein the stairstepped grid and the surface represent a discontinuity in a geologic environment, wherein the stairstepped grid comprises cuboid shaped grid cells and wherein the mapping accounts for spatial discrepancies between the stairstepped grid and the surface;

based at least in part on the mapping, for adjacent cuboid shaped grid cells that represent material on one side of the discontinuity and material on another side of the discontinuity, without reshaping the adjacent cuboid shaped grid cells, adjust physical properties and adjust connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface, wherein the physical properties comprise permeability and wherein the connectivity comprises transmissibility; and

simulate flow in the geologic environment using the stairstepped grid to represent the discontinuity, the adjusted physical properties and the adjusted connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface to generate simulation results.

13. The method of claim 3 wherein the fault extends across layers of a model wherein the layers differ as to rock composition.

14. The method of claim 13 wherein the layers comprise a sand layer and a shale layer.

15. One or more non-transitory computer-readable storage media comprising computer-executable instructions to instruct a flow simulator, the instructions comprising instructions to:

map a stairstepped grid to a surface wherein the stairstepped grid and the surface represent a discontinuity in a geologic environment, wherein the stairstepped grid comprises cuboid shaped grid cells and wherein the mapping accounts for spatial discrepancies between the stairstepped grid and the surface;

based at least in part on the mapping, for adjacent cuboid shaped grid cells that represent material on one side of the discontinuity and material on another side of the discontinuity, without reshaping the adjacent cuboid shaped grid cells, adjust physical properties and adjust connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface, wherein the physical properties comprise permeability and wherein the connectivity comprises transmissibility; and

simulate flow in the geologic environment using the stairstepped grid to represent the discontinuity, the adjusted physical properties and the adjusted connectivity to compensate for the spatial discrepancies between the stairstepped grid and the surface to generate simulation results.

16. The one or more non-transitory computer-readable storage media of claim 15 wherein the spatial discrepancies comprise length mismatches between risers and/or treads of the stairstepped grid and lengths along the surface.

17. The one or more non-transitory computer-readable storage media of claim 15 wherein the instructions to map comprise instructions to map the stairstepped grid to each of two sides of the surface.

18. The one or more non-transitory computer-readable storage media of claim 15 wherein the discontinuity comprises a fault.

19. The method of claim 1 comprising based at least in part on the simulation results, performing an operation with respect to the geologic environment, wherein the operation comprises a member selected from a group consisting of sensing, drilling, injection and extracting.