Geologic Model Simulation Grid Zone Mapping

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Solution Overview

Problem

Current gridding methods for geologic modeling in hydrocarbon exploration and production are inefficient, requiring high computational resources and often resulting in suboptimal cell alignments, which can lead to inaccurate reservoir simulations and costly miscalculations in well placement and fluid flow predictions.

Innovation Solution

An improved simulation gridding technique that generates a physical space simulation mesh by mapping a geologic model to a design space, partitioning cells with faults, and reverse mapping to the physical space, allowing for better cell alignments and reduced computational burden, while maintaining accurate representation of subsurface features.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Manufacturing precision

If conventional gridding methods are used to generate simulation meshes, then the mesh can be created with standard procedures, but the computational burden is high and cell alignments are suboptimal

Engineering Contradiction:
Improvecell alignment accuracyVSAvoidcomputational burden
Core Design Contradiction:
Manufacturing precisionVSDevice complexity

Solution Approach 1:

The patent introduces a design space as an intermediary between the physical space geologic model and the final simulation mesh. By mapping the geologic model to a simplified design space, performing gridding operations there, and then mapping back to physical space, the method achieves better cell alignments while reducing computational complexity compared to direct gridding in physical space.

Inventive Principle:
Principle #24Intermediary (Mediator)

2Measurement precision

If more numerous smaller volumetric elements are used in the mesh, then higher accuracy is achieved, but computational demands increase significantly

Engineering Contradiction:
Improvesimulation accuracyVSAvoidcomputational resources
Core Design Contradiction:
Measurement precisionVSUse of energy by moving object

Solution Approach 1:

The patent transforms the gridding problem by changing the coordinate system and working in design space rather than physical space. This parameter transformation allows for more efficient mesh generation that achieves the required simulation accuracy without needing excessively fine discretization, thereby reducing computational resource requirements.

Inventive Principle:
Principle #35Parameter changes

3Productivity

If conventional gridding methods are used, then the process is straightforward, but the gridding time is excessive

Engineering Contradiction:
Improvegridding speedVSAvoidgridding completion time
Core Design Contradiction:
ProductivityVSLoss of time

Solution Approach 1:

The patent segments the gridding process into distinct phases: mapping to design space, gridding in design space, and mapping back to physical space. This segmentation allows each phase to be optimized independently, with the design space gridding phase being computationally more efficient, thereby reducing overall gridding time while maintaining productivity.

Inventive Principle:
Principle #1Segmentation

Data Source

PatentUS11409024B2Methods and systems for generating simulation grids via zone by zone mapping from design space
Publication Date: 2022.08.09 EXXONMOBIL UPSTREAM RESEARCH COMPANY(US)
  • US11409024B2 patent drawing
  • US11409024B2 patent drawing
  • US11409024B2 patent drawing

AI summary

An illustrative geologic modeling method may comprise: obtaining a geologic model representing a subsurface region in physical space, the subsurface region being divided into multiple zones; sequentially generating a physical space simulation mesh for each of said multiple zones by: (a) mapping a current zone of the physical space geologic model to a current zone of a design space model representing a current zone of an unfaulted subsurface region; (b) gridding the design space model to obtain a design space mesh; (c) partitioning cells in the current zone of the design space mesh with faults mapped from the current zone of the physical space geologic model, thereby obtaining a partitioned design space mesh for the current zone; and (d) reverse mapping the partitioned design space mesh for the current zone to the physical space for the current zone.