4D petroelastic modeling based on a presalt well

Author:

Silva E. P. A.1ORCID,Davólio A.2ORCID,Santos M. S.1,Schiozer D. J.2

Affiliation:

1. Petrobras, Reservoir Geophysics, Rio de Janeiro 20031-170, Brazil.(corresponding author); .

2. UNICAMP/CEPETRO, FEM, Department of Petroleum Engineering, São Paulo 13083-896, Brazil..

Abstract

After their initial discovery in 2006, followed by an accumulated production of over 2 billion barrels of oil equivalent, the presalt carbonate reservoirs of offshore Brazil are now candidates for time-lapse seismic analysis. Therefore, we have conducted a 4D feasibility study in a Brazilian presalt reservoir well, which is composed of two types of carbonate rocks: microbialite and coquina. We evaluated two petroelastic models to obtain the acoustic impedance (AI) and shear impedance (SI) needed to estimate potential time-lapse differences ([Formula: see text], [Formula: see text], and [Formula: see text]). For this, we used the Gassmann and Xu-Payne models, in which the latter considers the pore geometry of the rock in its equations. Our analysis of both models shows that changes in pressure and saturation are very similar, and we can conclude that, despite being a carbonate, the application of Gassmann’s model is sufficient for the 4D feasibility studies conducted in the deemed reservoir because it does not require pore space geometry parameters, as does the Xu-Payne model. The analysis of the time-lapse attributes provided us with a greater comprehension of the 4D scenarios modeled, some of which presented detectability of changes in the microbialite and coquina.

Publisher

Society of Exploration Geophysicists

Subject

Geology,Geophysics

Reference17 articles.

1. Abreu, E. S., 2010, Modelagens Teóricas e Empíricas Aplicadas à Investigação da Conexão entre as Propriedades Petrofísicas e Elásticas em Rochas Carbonáticas: Dissertação de Mestrado, University of Campinas.

2. Gassmann's fluid substitution and shear modulus variability in carbonates at laboratory seismic and ultrasonic frequencies

3. 4. Sonic Velocity in Carbonate Sediments and Rocks

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