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SFR661K5
The solution of Fourier’s one-dimensional steady state conduction heat flow equation for two layers-model has been solved using the analytical techniques and applied to part of Niger Delta sedimentary basin. The temperature-depth profile obtained shows a linear increase in temperature with depth. The internal properties affecting the thermal structures are the thermal conductivity and heat production. Comparison of measured and computed temperatures for some wells showed good agreement with minor variation ranging between -4.0 to 5.0 oC. This model can be used to determine thermal properties of other parts of the basin with little adjustment of the rock properties values.
Emujakporue, Godwin Omokenu. 2016. \u201cAnalytical Determination of Subsurface Temperature Using Two Layers Model in Part of Niger Delta Sedimentary Basin, Nigeria\u201d. Global Journal of Science Frontier Research - A: Physics & Space Science GJSFR-A Volume 16 (GJSFR Volume 16 Issue A3).
Crossref Journal DOI 10.17406/GJSFR
Print ISSN 0975-5896
e-ISSN 2249-4626
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Total Score: 102
Country: Nigeria
Subject: Global Journal of Science Frontier Research - A: Physics & Space Science
Authors: Emujakporue, Godwin Omokenu (PhD/Dr. count: 0)
View Count (all-time): 176
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Publish Date: 2016 05, Tue
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This study aims to comprehensively analyse the complex interplay between
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