Difference between revisions of "Saturations required for hydrocarbon flow"
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| part = Predicting the occurrence of oil and gas traps | | part = Predicting the occurrence of oil and gas traps | ||
| chapter = Evaluating top and fault seal | | chapter = Evaluating top and fault seal | ||
− | | frompg = 10- | + | | frompg = 10-85 |
− | | topg = 10- | + | | topg = 10-85 |
| author = Grant M. Skerlec | | author = Grant M. Skerlec | ||
| link = http://archives.datapages.com/data/specpubs/beaumont/ch10/ch10.htm | | link = http://archives.datapages.com/data/specpubs/beaumont/ch10/ch10.htm | ||
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==Traditional definitions== | ==Traditional definitions== | ||
− | Hydrocarbons flow through a water-wet seal when there is a continuous, interconnected pathway of hydrocarbon-filled pore space. Flow through a seal occurs with saturations of 4.5–17% of the rock pore volume, averaging 10%.<ref name=ch10r67>Schowalter, T., T., 1979, [http://archives.datapages.com/data/bulletns/1977-79/data/pg/0063/0005/0700/0723.htm Mechanics of secondary hydrocarbon migration and entrapment]: AAPG Bulletin, vol. 63, no. 5, p. 723–760.</ref> This is one reason displacement pressure is defined at 10% saturation. | + | Hydrocarbons flow through a water-wet seal when there is a continuous, interconnected pathway of hydrocarbon-filled pore space. Flow through a seal occurs with saturations of 4.5–17% of the rock pore volume, averaging 10%.<ref name=ch10r67>Schowalter, T., T., 1979, [http://archives.datapages.com/data/bulletns/1977-79/data/pg/0063/0005/0700/0723.htm Mechanics of secondary hydrocarbon migration and entrapment]: AAPG Bulletin, vol. 63, no. 5, p. 723–760.</ref> This is one reason [[displacement pressure]] is defined at 10% saturation. |
==Possible modifications== | ==Possible modifications== | ||
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==See also== | ==See also== | ||
− | * [[ | + | * [[Seal capacity: pitfalls and limitations of estimation]] |
− | * [[ | + | * [[Displacement pressure of a seal: difficulty of characterization]] |
− | * [[ | + | * [[Displacement pressure: does the theory predict reality?]] |
* [[Seal capacity of breached and hydrocarbon-wet seals]] | * [[Seal capacity of breached and hydrocarbon-wet seals]] | ||
* [[Hydrodynamic flow and pressure transients]] | * [[Hydrodynamic flow and pressure transients]] | ||
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[[Category:Predicting the occurrence of oil and gas traps]] | [[Category:Predicting the occurrence of oil and gas traps]] | ||
[[Category:Evaluating top and fault seal]] | [[Category:Evaluating top and fault seal]] | ||
+ | [[Category:Treatise Handbook 3]] |
Latest revision as of 13:57, 1 April 2022
Exploring for Oil and Gas Traps | |
Series | Treatise in Petroleum Geology |
---|---|
Part | Predicting the occurrence of oil and gas traps |
Chapter | Evaluating top and fault seal |
Author | Grant M. Skerlec |
Link | Web page |
Store | AAPG Store |
Traditional definitions
Hydrocarbons flow through a water-wet seal when there is a continuous, interconnected pathway of hydrocarbon-filled pore space. Flow through a seal occurs with saturations of 4.5–17% of the rock pore volume, averaging 10%.[1] This is one reason displacement pressure is defined at 10% saturation.
Possible modifications
Other experiments, including lower porosity rocks, indicate much higher oil saturations of 25–91% may be required.[2] The current assumption that seal capacity is based upon the displacement pressure at only 10% saturation could be very misleading. The value could be two or more orders of magnitude greater than that predicted at 10% saturation.
See also
- Seal capacity: pitfalls and limitations of estimation
- Displacement pressure of a seal: difficulty of characterization
- Displacement pressure: does the theory predict reality?
- Seal capacity of breached and hydrocarbon-wet seals
- Hydrodynamic flow and pressure transients
References
- ↑ Schowalter, T., T., 1979, Mechanics of secondary hydrocarbon migration and entrapment: AAPG Bulletin, vol. 63, no. 5, p. 723–760.
- ↑ England, W., A., Mackenzie, A., S., Mann, D., M., Quickley, T., M., 1987, The movement and entrapment of petroleum fluids in the subsurface: Journal of the Geological Society, London, vol. 144, no. 2, p. 327–347.