Abstract

Abstract. This paper proposes and demonstrates improvements for the Monte Carlo simulation for uncertainty propagation (MCUP) method. MCUP is a type of Bayesian Monte Carlo method aimed at input data uncertainty propagation in implicit 3-D geological modeling. In the Monte Carlo process, a series of statistically plausible models is built from the input dataset of which uncertainty is to be propagated to a final probabilistic geological model or uncertainty index model. Significant differences in terms of topology are observed in the plausible model suite that is generated as an intermediary step in MCUP. These differences are interpreted as analogous to population heterogeneity. The source of this heterogeneity is traced to be the non-linear relationship between plausible datasets' variability and plausible model's variability. Non-linearity is shown to mainly arise from the effect of the geometrical rule set on model building which transforms lithological continuous interfaces into discontinuous piecewise ones. Plausible model heterogeneity induces topological heterogeneity and challenges the underlying assumption of homogeneity which global uncertainty estimates rely on. To address this issue, a method for topological analysis applied to the plausible model suite in MCUP is introduced. Boolean topological signatures recording lithological unit adjacency are used as n-dimensional points to be considered individually or clustered using the density-based spatial clustering of applications with noise (DBSCAN) algorithm. The proposed method is tested on two challenging synthetic examples with varying levels of confidence in the structural input data. Results indicate that topological signatures constitute a powerful discriminant to address plausible model heterogeneity. Basic topological signatures appear to be a reliable indicator of the structural behavior of the plausible models and provide useful geological insights. Moreover, ignoring heterogeneity was found to be detrimental to the accuracy and relevance of the probabilistic geological models and uncertainty index models. Highlights. Monte Carlo uncertainty propagation (MCUP) methods often produce topologically distinct plausible models. Plausible models can be differentiated using topological signatures. Topologically similar probabilistic geological models may be obtained through topological signature clustering.

Highlights

  • Input data uncertainty propagation is an essential part of risk-aware 3-D geological modeling

  • The 3-D geological model suites are built from a series of plausible datasets that are generated through input data perturbation (Fig. 1), which is a process in which alternative input datasets are stochastically generated from the original data inputs by sampling from probability distribution functions known as disturbance distributions (Pakyuz-Charrier et al, 2018a)

  • Once the plausible model suite has been segregated into clusters based on their topology, a range of statistical methods may be applied to the results to (i) evaluate the quality and relevance of the clusters, (ii) determine data leverage in relation to the clusters, (iii) perform standard Monte Carlo uncertainty propagation (MCUP) comparative analysis on the clusters and (iv) feed the clusters to an external rejection system

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Summary

Introduction

Input data uncertainty propagation is an essential part of risk-aware 3-D geological modeling MCUP methods (Fig. 1) aim to propagate the measurement uncertainty of structural input data (interface points, foliations, fold axes) through implicit 3-D geological modeling engines to produce probabilistic geological models and uncertainty index models. The standard MCUP procedure is described, the source of plausible model incompatibility is discussed, and a topological analysis method is proposed to address the issue and improve the relevance of probabilistic geological models and uncertainty index models to real world problems. Adjacency matrices qualify which geological units are in contact using Boolean logic These matrices are converted to binary signals called topological signatures that are clustered using DBSCAN. The goal is to provide MCUP practitioners with a procedure to ensure that probabilistic geological models and uncertainty index models are made of topologically similar plausible models. The method is tried and tested on two synthetic case studies to demonstrate its applicability

MCUP method
Disturbance distribution parameterization
Plausible datasets’ generation
Plausible model building
Comparative analysis
Plausible model topological heterogeneity
Plausible model topological analysis
Lithological topology
Topological clustering using DBSCAN
Post-clustering analysis
Synthetic case study
Model description and MCUP parameters
High-input data confidence run
Low-input data confidence run
Findings
Discussion
Conclusions
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