Formation dynamics of subsurface hydrocarbon intrusions following the Deepwater Horizon blowout
Geophysical Research Letters
By: S.A. Socolofsky, E.E. Adams, and C. R. Sherwood
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Abstract
Hydrocarbons released following the Deepwater Horizon (DH) blowout were found in deep, subsurface horizontal intrusions, yet there has been little discussion about how these intrusions formed. We have combined measured (or estimated) observations from the DH release with empirical relationships developed from previous lab experiments to identify the mechanisms responsible for intrusion formation and to characterize the DH plume. Results indicate that the intrusions originate from a stratification-dominated multiphase plume characterized by multiple subsurface intrusions containing dissolved gas and oil along with small droplets of liquid oil. Unlike earlier lab measurements, where the potential density in ambient water decreased linearly with elevation, at the DH site it varied quadratically. We have modified our method for estimating intrusion elevation under these conditions and the resulting estimates agree with observations that the majority of the hydrocarbons were found between 800 and 1200 m. Copyright ?? 2011 by the American Geophysical Union.
Suggested Citation
Socolofsky, S., Adams, E., and Sherwood, C.R., 2011, Formation dynamics of subsurface hydrocarbon intrusions following the Deepwater Horizon blowout: Geophysical Research Letters, v. 38, no. 9, https://doi.org/10.1029/2011GL047174.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Formation dynamics of subsurface hydrocarbon intrusions following the Deepwater Horizon blowout |
| Series title | Geophysical Research Letters |
| DOI | 10.1029/2011GL047174 |
| Volume | 38 |
| Issue | 9 |
| Publication Date | May 12, 2011 |
| Year Published | 2011 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Geophysical Research Letters |