Combine petroleum-system history with a bounded pore inventory
Organic-rich source material can generate hydrocarbons during burial and heating. Migration, porous reservoir rock, a sufficiently effective seal and a trapping geometry must align in time for accumulation. Coal represents a different concentrated organic deposit history; not every fossil fuel occupies a conventional porous trap.
Learning outcome: Hold geometry fixed while changing closure history, then vary porosity under early closure. Preserve the age ordering, volume-factor direction and separate retained/recoverable quantities. List a new observation that would test the no-recharge assumption.
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Retain resource inventories, physical force and reaction boundaries, chronological alternatives and explicit decision constraints. Conditional teaching results do not certify actual site suitability.
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At porosity 0.2 and early closure, pore volume is 400000 m³; hydrocarbon capacity is 300000 reservoir m³, equivalent to 250000 surface m³. Applying recovery 0.3 gives 75000 surface m³. These units are not interchangeable.
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Can identical present-day porosity and trap shape imply different retained inventories because of timing?
Experiment
Hold geometry fixed while changing closure history, then vary porosity under early closure. Preserve the age ordering, volume-factor direction and separate retained/recoverable quantities. List a new observation that would test the no-recharge assumption.
Combine pore inventory with trap timing
Worked teaching model · synthetic values · Original reservoir bulk volume 2 million m³, water saturation 0.25, formation volume factor 1.2 reservoir m³ per surface m³. Recovery fraction 0.3. Charge pulse at 80 Ma; closure at 100 Ma (before) or 60 Ma (after). Late closure retains no pulse in this deliberately open escape model; no later recharge.
Reset keeps your prediction, captures and practice history.
Porous rock is not sufficient: source, migration, seal, trap and timing must be compatible.
The calculation stipulates full charging for the early closed trap and none for the late open one. Real migration can continue or recur; reservoir volume alone does not prove a discovery, reserve, economic viability or permission to extract.
Chronology: Closure at 100 Ma precedes charge at 80 Ma: pulse retained up to supplied capacity.
| Quantity | Value | Unit |
|---|---|---|
| Pore volume | 400000 | m³ |
| Geometric hydrocarbon-filled capacity | 300000 | reservoir m³ |
| Charge retained under supplied timing | 1 | 0 no / 1 yes |
| Retained surface-equivalent inventory | 250000 | surface m³ |
| Conditional recoverable amount | 75000 | surface m³ |
Original instructional packets and diagrams, not actual site measurements, legal limits or professional clearance.
Porous rock is not sufficient: source, migration, seal, trap and timing must be compatible.
The calculation stipulates full charging for the early closed trap and none for the late open one. Real migration can continue or recur; reservoir volume alone does not prove a discovery, reserve, economic viability or permission to extract.
Captures preserve recipes and replay their calculated results. They are synthetic model evidence, not physical measurements.
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Public practice checks a specific claim. It does not establish independent mastery.
At porosity 0.3, compare closure at 100 Ma and 60 Ma for the single 80 Ma pulse.
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