Fluvial Zone Simulation via Deterministic-Stochastic Particle Model

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Solution Overview

Problem

Current models fail to accurately simulate the geological formation of fluvial zones, which are crucial for oil prospecting, as they do not effectively account for the specific features of these zones using observation data.

Innovation Solution

A method is developed to simulate the geological formation of fluvial zones by defining a spatial model with both deterministic and stochastic terms based on observation data, incorporating a meandriform term and random perturbations to model particle displacement, and allowing for events like particle separation, joining, and disappearance, while also considering external sources.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Reliability

If a deterministic model is used to simulate particle displacement, then the model is simple to implement, but it cannot accurately represent the complex geological formation processes of fluvial zones

Engineering Contradiction:
Improvesimulation accuracyVSAvoidmodel complexity
Core Design Contradiction:
ReliabilityVSDevice complexity

Solution Approach 1:

The patent combines deterministic advection (representing mean flow) with stochastic diffusion (representing turbulent fluctuations and depositional variability) into a unified particle displacement model. This merging allows the simulation to capture both the overall transport direction and the complex, random nature of geological deposition processes, thereby improving reliability without requiring a completely separate complex model

Inventive Principle:
Principle #5Merging (Combining)

Solution Approach 2:

The model transitions from a static deterministic framework to a dynamic stochastic framework where particle displacement is continuously updated with random perturbations at each time step. This dynamic approach allows the simulation to adapt to local variations in flow conditions and depositional environments, improving the realism and accuracy of fluvial zone formation simulation

Inventive Principle:
Principle #15Dynamics

2Measurement precision

If observation data is extensively used to parameterize the model, then the simulation accuracy improves, but the difficulty of model calibration and implementation increases

Engineering Contradiction:
Improvemodel calibration precisionVSAvoidmodel implementation ease
Core Design Contradiction:
Measurement precisionVSEase of manufacture

Solution Approach 1:

The patent transforms complex geological parameters into simplified model parameters that can be directly calibrated from observation data. By changing the parameterization approach to use measurable quantities like mean flow velocity and turbulent diffusion coefficients, the model becomes both more accurate (using real observation data) and easier to implement (using standard hydrological parameters rather than complex geological constants)

Inventive Principle:
Principle #35Parameter changes

3Reliability

If particle interactions (separation, joining, disappearance) are modeled, then the simulation realism improves, but the computational complexity increases

Engineering Contradiction:
Improvegeological process realismVSAvoidcomputational complexity
Core Design Contradiction:
ReliabilityVSDevice complexity

Solution Approach 1:

The particle system automatically handles separation, joining, and disappearance events based on predefined probabilistic rules that reflect natural geological processes. Rather than requiring complex external control mechanisms, the particles self-organize and interact according to simple stochastic rules, improving realism while keeping computational requirements manageable through local, event-driven updates

Inventive Principle:
Principle #25Self-service

Data Source

PatentUS10007741B2Method for simulating the geological formation of a river zone
Publication Date: 2018.06.26 TOTALENERGIES ONETECH
  • US10007741B2 patent drawing
  • US10007741B2 patent drawing
  • US10007741B2 patent drawing

AI summary

Systems and methods for simulating a geological formation of a fluvial zone by using observation data and a spatial model of the fluvial zone. The displacement of particles in the spatial model is simulated by superimposing a deterministic term defined by the observation data and a stochastic term parameterized by the observation data. By virtue of this method, it is possible to take into account both the fluid flow of the particles in the fluvial zone and introduce a probabilistic perturbation.