Capillary pressure equilibrium theory mapping of 4D seismic inversion results to predict saturation in a gas-water system

Author:

Sengupta Moumita1ORCID,Ghosh Ranjana2ORCID,Sen Amrita3,Maiti Saumen4ORCID

Affiliation:

1. Cairn Oil and Gas, Gurugram, Haryana, India. .

2. National Geophysical Research Institute, Hyderabad, India. (corresponding author).

3. C3.AI, Houston, Texas, USA. .

4. IIT (ISM) Dhanbad, Jharkhand, India. .

Abstract

Understanding the effect of fluid concentration in rocks is crucial to characterize a hydrocarbon reservoir. Monitoring of fluid concentration specifically becomes challenging during a sequestration/enhanced oil recovery program because the objective is to understand the amount of initial fluid replaced by liquid/gas injection and identify the probability of leakage with time. The prior assumption of uniform or patchy type of distribution of gas in a rock-physics theory leads to large uncertainty in the prediction of saturation. As a result, we have used the capillary pressure equilibrium theory (CPET) for creating a reservoir model that matches the physics of capillary-induced fluid invasion and avoids the uncertainty related to the type of distribution of gas in pores. We create a CPET model using the reservoir parameters of the clean and unconsolidated sandstone formation of the Sleipner field, North Sea, which is the world’s first industrial-scale CO2-injection project, assuming that there is no significant change in the rock frame throughout the field. The model is then used to analyze the fluid content from the time-lapse seismic inversion results of the Sleipner field. CO2 at higher quantities, according to our research, is analogous to a uniform distribution, whereas CO2 at lower concentrations is mostly in between patchy and uniform distribution or slightly patchy type. We predict maximum CO2 saturation from a quantitative interpretation of six time-lapse seismic data from 1999 to 2010 using the CPET as 75% of the pore space, and the footprint of the CO2 plume in the topmost layer is spreading from zero in 2001 to 7 × 105 m2 in 2010. Our model finds that injected CO2 from all layers below will migrate to the top layer approximately 50 years after the commencement of the injection.

Publisher

Society of Exploration Geophysicists

Subject

Geochemistry and Petrology,Geophysics

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