Subsoil Formation Determination via Global Flow Velocity Field
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Solution Overview
Problem
Existing methods for determining subsoil formations in the hydrocarbon industry require pre-meshing, which introduces biases and fails to accurately account for sedimentary bodies and geological relationships, making it difficult to satisfy well constraints and associate cells with facies or geophysical properties.
Innovation Solution
A method using parametric models that simulate sedimentary flows with deterministic and stochastic terms, allowing for realistic modeling of geological formations without initial meshing, and employing NURBS surfaces to define and distort formations to fit constraints, followed by meshing that adapts to the determined shapes.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Ease of manufacture
If pre-meshing is performed before modeling, then the modeling process can be initiated, but biases are introduced in mesh size, orientation, and number that affect modeling accuracy
Solution Approach 1:
The patent inverts the traditional workflow by performing modeling first and meshing afterward. Instead of meshing the model before analysis, the method generates an unmeshed model, performs the modeling operations to determine geological formations, and then creates the mesh based on the results. This inversion eliminates the biases introduced by pre-meshing while maintaining the ability to initiate and complete the modeling process.
2Device complexity
If pre-meshing is used, then the model structure is defined in advance, but sedimentary bodies and geological formations cannot be accurately represented
Solution Approach 1:
The patent applies preliminary action by defining the geological model structure, sedimentary bodies, and formations through modeling operations before creating the mesh. The unmeshed model allows geological formations to be identified and defined with accuracy, and only after this preliminary modeling is complete is the mesh generated to match the determined geological structures.
3Ease of operation
If pre-meshed models are used, then the model can be processed, but it is difficult to satisfy well constraints due to blocking methods that reduce log data precision
Solution Approach 1:
The patent inverts the traditional approach by satisfying well constraints during the unmeshed modeling phase before meshing occurs. Log data and well constraints are applied to the unmeshed model where full precision is maintained, allowing accurate satisfaction of constraints. The mesh is then generated afterward to match the already-constrained geological model, avoiding the need for blocking methods that would reduce data precision.
4Productivity
If cells are associated with facies or geophysical properties in pre-meshed models, then the model can be analyzed, but cell dimension limitations prevent proper identification of positional relationships
Solution Approach 1:
The patent performs the association of cells with facies and geophysical properties as a preliminary action after modeling but before final mesh generation. In the unmeshed model, geological formations and their spatial relationships are identified with high precision. The mesh and cell associations are then created based on these precisely identified formations, ensuring that positional relationships are properly maintained while enabling model analysis.
Data Source
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AI summary
The present disclosure relates to a method for determination of real subsoil geological formation characterized in that the method comprises: /a/ receiving a model representing the real subsoil, said model comprising a stratigraphic layer, said stratigraphic layer comprising a shore line (800) dividing the stratigraphic layer into a continental zone (801) and a marine zone (802); /b/ receiving a first flow speed field (811) representative of a continental domain for the stratigraphic layer; /c/ receiving a second flow speed field (812) representative of a marine domain for the stratigraphic layer; /d/ determining a weighted combination, named global flow speed field, of the first flow speed field and the second flow speed field for each position in the stratigraphic layer, weights of the combination are based on a distance of said position to the shore line (800) and the fact that the position is within the continental zone or the marine zone; /e/ determining a real subsoil geological formation for the stratigraphic layer based on the determined global flow speed field.