Abstract

Seismic data and nuclear magnetic resonance (NMR) data are two of the highly trustable kinds of information in hydrocarbon reservoir engineering. Reservoir fluids influence the elastic wave velocity and also determine the NMR response of the reservoir. The current study investigates different pore types, i.e., micro, meso, and macropores’ contribution to the elastic wave velocity using the laboratory NMR and elastic experiments on coal core samples under different fluid saturations. Once a meaningful relationship was observed in the lab, the idea was applied in the field scale and the NMR transverse relaxation time (T2) curves were synthesized artificially. This task was done by dividing the area under the T2 curve into eight porosity bins and estimating each bin’s value from the seismic attributes using neural networks (NN). Moreover, the functionality of two statistical ensembles, i.e., Bag and LSBoost, was investigated as an alternative tool to conventional estimation techniques of the petrophysical characteristics; and the results were compared with those from a deep learning network. Herein, NMR permeability was used as the estimation target and porosity was used as a benchmark to assess the reliability of the models. The final results indicated that by using the incremental porosity under the T2 curve, this curve could be synthesized using the seismic attributes. The results also proved the functionality of the selected statistical ensembles as reliable tools in the petrophysical characterization of the hydrocarbon reservoirs.

Highlights

  • We explored the functionality of statistical ensembles for determining the petrophysical properties of the reservoir and compared their performance with that of the deep learning neural networks

  • We focused on Bag and Least Square Boosting (LSBoost) ensembles

  • While the liner relationship is the simplest form, the neural networks use high-order polynomial relationships, for which the cross-correlation values are much larger than the linear manner

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Summary

Introduction

We observed how the fluid saturation affects the elastic and NMR response of an individual core sample and determined the relationship between the changes of the T2 curve and compressional P-wave velocity under decreasing water saturation. Based on these observations, we used the intelligent networks to estimate the incremental NMR porosity values from seismic attributes and synthesized the NMR curves in the field scale. Corresponding area of each pore type (micro, meso, macropores) under T2 curve at three saturation states. It is worth noting that these values represent the average value as the wave propagation inside the pore space happens simultaneously in all pore types

Seismic and NMR Data from the Field
Estimating NMR CBPs from Seismic Attributes
Linear
Bag and LSBoost Ensembles
Limitations
Findings
Conclusions
Full Text
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