Difference between revisions of "Postaccumulation cementation"
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| part = Predicting the occurrence of oil and gas traps | | part = Predicting the occurrence of oil and gas traps | ||
| chapter = Predicting preservation and destruction of accumulations | | chapter = Predicting preservation and destruction of accumulations | ||
| − | | frompg = 11- | + | | frompg = 11-11 |
| − | | topg = 11- | + | | topg = 11-11 |
| author = Alton A. Brown | | author = Alton A. Brown | ||
| link = http://archives.datapages.com/data/specpubs/beaumont/ch11/ch11.htm | | link = http://archives.datapages.com/data/specpubs/beaumont/ch11/ch11.htm | ||
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| isbn = 0-89181-602-X | | isbn = 0-89181-602-X | ||
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| − | Although the presence of a petroleum phase may retard diagenesis in an accumulation, sooner or later [[reservoir quality]] decreases with increasing age and burial.<ref name=ch11r5>Bloch, S., 1991, Empirical prediction of | + | Although the presence of a petroleum phase may retard [[diagenesis]] in an [[accumulation]], sooner or later [[reservoir quality]] decreases with increasing age and burial.<ref name=ch11r5>Bloch, S., 1991, [http://archives.datapages.com/data/bulletns/1990-91/data/pg/0075/0007/0000/1145.htm Empirical prediction of porosity and permeability in sandstones]: AAPG Bulletin, vol. 75, p. 1145–1160.</ref> |
==The process== | ==The process== | ||
| − | As the pore volume within a trap decreases due to burial cementation, several phenomena combine to destroy the economic accumulation. | + | As the pore volume within a trap decreases due to [[burial cementation]], several phenomena combine to destroy the economic accumulation. |
| − | + | # Petroleum is displaced from the [[trap]] at the [[spill point]] as the pore volume within the structural closure decreases. If [[porosity]] is lowered sufficiently, the [[accumulation]] may be subeconomic in size. | |
| − | + | # Reduced porosity may result in lower [[permeability]] so that production rates are subeconomic, even where economic quantities of petroleum are still trapped. | |
| − | + | # As pore size decreases in a petroleum-filled reservoir, the [[capillary pressure]] of the petroleum phase must increase to occupy the pore spaces (assuming no change in [[wettability]]). In low-permeability [[tight gas reservoirs: evaluation|tight sands]] or carbonates, the capillary [[displacement pressure]] in the reservoir rock may approach that of moderate-quality seals. As a result, a lithology that could seal an accumulation at shallow depth may no longer be effective at deeper depths because it differs little from the reservoir rock. | |
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==Predicting spillage by cementation== | ==Predicting spillage by cementation== | ||
| − | Reduced porosity can be predicted from | + | Reduced porosity can be predicted from empirical or statistical evaluation of porosity data for reservoir intervals with similar composition and burial history as the prospect.<ref name=ch11r31>Schmoker, J. W., and D. L. Gautier, 1988, Sandstone porosity as a function of thermal maturity: Geology, vol. 16, p. 1007–1010, DOI: [http://geology.gsapubs.org/content/16/11/1007.full.pdf 10.1130/0091-7613(1988)016<1007:SPAAFO>2.3.CO;2].</ref><ref name=ch11r5 /> In general, porosity decreases with increasing age, depth, and temperature. Numerical modeling techniques are not yet refined enough to quantitatively predict prospect reservoir quality loss. |
==See also== | ==See also== | ||
* [[Trap spillage]] | * [[Trap spillage]] | ||
* [[Changes in trapping geometry]] | * [[Changes in trapping geometry]] | ||
| − | * [[ | + | * [[Hydrodynamics: change in configuration]] |
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==References== | ==References== | ||
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[[Category:Predicting the occurrence of oil and gas traps]] | [[Category:Predicting the occurrence of oil and gas traps]] | ||
[[Category:Predicting preservation and destruction of accumulations]] | [[Category:Predicting preservation and destruction of accumulations]] | ||
| + | [[Category:Treatise Handbook 3]] | ||
Latest revision as of 15:35, 1 February 2022
| Exploring for Oil and Gas Traps | |
| |
| Series | Treatise in Petroleum Geology |
|---|---|
| Part | Predicting the occurrence of oil and gas traps |
| Chapter | Predicting preservation and destruction of accumulations |
| Author | Alton A. Brown |
| Link | Web page |
| Store | AAPG Store |
Although the presence of a petroleum phase may retard diagenesis in an accumulation, sooner or later reservoir quality decreases with increasing age and burial.[1]
The process
As the pore volume within a trap decreases due to burial cementation, several phenomena combine to destroy the economic accumulation.
- Petroleum is displaced from the trap at the spill point as the pore volume within the structural closure decreases. If porosity is lowered sufficiently, the accumulation may be subeconomic in size.
- Reduced porosity may result in lower permeability so that production rates are subeconomic, even where economic quantities of petroleum are still trapped.
- As pore size decreases in a petroleum-filled reservoir, the capillary pressure of the petroleum phase must increase to occupy the pore spaces (assuming no change in wettability). In low-permeability tight sands or carbonates, the capillary displacement pressure in the reservoir rock may approach that of moderate-quality seals. As a result, a lithology that could seal an accumulation at shallow depth may no longer be effective at deeper depths because it differs little from the reservoir rock.
Predicting spillage by cementation
Reduced porosity can be predicted from empirical or statistical evaluation of porosity data for reservoir intervals with similar composition and burial history as the prospect.[2][1] In general, porosity decreases with increasing age, depth, and temperature. Numerical modeling techniques are not yet refined enough to quantitatively predict prospect reservoir quality loss.
See also
References
- ↑ 1.0 1.1 Bloch, S., 1991, Empirical prediction of porosity and permeability in sandstones: AAPG Bulletin, vol. 75, p. 1145–1160.
- ↑ Schmoker, J. W., and D. L. Gautier, 1988, Sandstone porosity as a function of thermal maturity: Geology, vol. 16, p. 1007–1010, DOI: 10.1130/0091-7613(1988)016<1007:SPAAFO>2.3.CO;2.
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