Abstract

This paper aims to investigate the impact of the overdetermination (data-to-unknowns) ratio on the global inversion of wireline logging data. In the course of the so-called interval inversion method, geophysical data measured in a borehole over a longer depth range is jointly inverted and the depth variation of the investigated petrophysical parameters are expanded into series using Legendre polynomials as basis functions resulting in a highly overdetermined inverse problem. A metaheuristic Particle Swarm Optimization (PSO) approach is applied as a first phase of inversion for decreasing the starting model dependence of the interval inversion procedure. In the subsequent linear inversion steps, by using the measurement error of logging tools and the covariance matrix of the estimated petrophysical parameters, we can quantify the accuracy of the model parameters. The dataset used in this study consists of nuclear, resistivity and sonic logs which are inverted to compute porosity, shale volume and water saturation along the investigated interval. For increasing the data-to-unknowns ratio of the inverse problem, shale volume is estimated separately by a PSO-based factor analysis and fixed as known parameter for the interval inversion process. Since the shale volume has been described as high degree Legendre polynomial, a significant increase of the overdetermination ratio considerably decreases the uncertainty of the remaining model parameters allowing for a more reliable calculation of hydrocarbon content.

Highlights

  • Geophysics provides several methods for the quantitative evaluation of subsurface geological structures

  • This results in an overdetermination ratio of 10, which is a 56.3% increase compared to the case detailed in chapter 5.1 where 4 model parameters were estimated by interval inversion

  • The starting model dependence of the procedure is virtually eliminated by Particle Swarm Optimization (PSO) and the switch to the linearized Damped Least Squares (DLSQ) method near the optimum greatly reduces the runtime of the inversion and allows for the calculation of estimation errors

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Summary

Introduction

Geophysics provides several methods for the quantitative evaluation of subsurface geological structures. Inversion of wireline logging data is done in a local manner, meaning that data measured at a given depth point is jointly inverted to estimate the petrophysical parameters at that same depth point (Drahos 2005; Mayer and Sibbit 1980) This usually leads to a marginally overdetermined inverse problem, since we have slightly more logging tools than unknowns, including shale volume, porosity and water saturation in the invaded zone and in the virgin zone. This can be done very quickly and delivers adequate results, the low data-to-unknowns ratio has a negative effect on the estimation accuracy of parameters. The number of observed data does not increase, but the simultaneous processing of several depth points greatly increases the relative number of data compared to series expansion coefficients as unknowns of the inverse problem

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