Abstract
This work integrates seismic and well log data to establish a 3D reservoir model of the Q-Field, which is a prolific onshore hydrocarbon field situated in the Central Swamp Depobelt of Nigeria. The subsurface modeling focuses on the four principal clastic reservoir intervals of the Agbada Formation (D6200, D7000, D9000 and E2000), which was deposited in a deltaic to fluvio-deltaic system during Eocene. The seismic-based structural modeling inferred an extensional set-up dominated by NW–SE trending normal faults. Reservoirs are sand-dominated and laterally extensive, as interpreted from the 3D facies model. Well log-based petrophysical parameters were up-scaled and distributed stochastically using the Sequential Gaussian Simulation method to generate a 3D reservoir property model. Lateral and vertical heterogeneities of the reservoir properties were inferred from the 3D models. In general, the clastic reservoirs exhibit 18–22% porosity, 62–105 mD permeability, moderate to good net-gross thickness, and 36–74% water saturation. Hydrocarbon accumulation was primarily restricted within the anticlines. Gas-down-to exists in the upper three reservoirs (D6200, D7000 and D9000) at 10,577 ft (1 ft = 0.3048 m), 10,756 ft and 11,389 ft, respectively. Gas–oil and oil–water contacts in the E2000 reservoir were interpreted to be at 11,812 ft and 11,886 ft, respectively. Based on the hydrocarbon distribution, oil and gas-in-place volumes were estimated for all the reservoir intervals. The comprehensive 3D modeling work addressed the spatial distribution of the studied reservoir properties and can be directly useful for planning better the future wells for field development.
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Acknowledgment
We are grateful to John Carranza, Ph.D., Editor-in-Chief, Natural Resources Research and to the two reviewers for their critical suggestions and constructive reviews which benefited this manuscript. Authors acknowledge SPDC Nigeria for providing the data set. The authors extend their sincere appreciation to the Researchers Supporting Project number (RSP-2020/92), King Saud University, Riyadh, Saudi Arabia.
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Appendix
Appendix
Sequential Indicator Simulation (SIS)
SIS is used for a discrete or categorical variable. The algorithm for SIS depends on indicator kriging to infer the cumulative distribution function (CDF) of a discrete variable Z(u). It simulates in cases where data are not required to fit a normal distribution with the sequential paradigm (Remy et al. 2009). Through stochastic simulation, equally probable realizations of the distribution of an indicator variable are produced (Journel 1982; Deutsch and Journel 1998). The steps in SIS are as follows.
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(i)
Select pixels where the lithotype is unknown.
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(ii)
Identify neighboring node points with known lithotypes.
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(iii)
Assign weights to the neighboring points.
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(iv)
Construct a local (CDF) for lithotype probability from the neighbor lithotypes.
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(v)
Extraction forms the CDF of a single lithotype to occupy the empty node points.
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(vi)
Random selection of another empty node point.
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(vii)
Proceed to Step 1 and repeat until estimations have been made at all the empty node points.
Sequential Gaussian Simulation (SGS)
SGS is a stochastic modeling technique that obtains multiple realizations based on the same input data (Maleki Tehrani et al. 2012; Geboy et al. 2013). The steps of SGS consist of the following.
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(i)
Select a node point where the reservoir property under investigation is unknown.
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(ii)
Recognize adjacent node points where the property is known.
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(iii)
Then, allocate weights to the neighbors, depending on their observed relevance at empty node points.
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(iv)
Construct a local probability distribution function (pdf) at the empty node points from the neighbor values.
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(v)
Extraction forms the pdf of a single value to occupy the empty node points, a random selection of another empty node points.
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(vi)
Proceed to Step 1 and repeat until estimations have been made at all empty node points.
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Okoli, A.E., Agbasi, O.E., Lashin, A.A. et al. Static Reservoir Modeling of the Eocene Clastic Reservoirs in the Q-Field, Niger Delta, Nigeria. Nat Resour Res 30, 1411–1425 (2021). https://doi.org/10.1007/s11053-020-09804-2
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DOI: https://doi.org/10.1007/s11053-020-09804-2