Rock Compressibility Correlations
Overview
Rock compressibility () quantifies the change in pore volume with pressure. It is a critical parameter for:
- Material balance calculations β affects OOIP/OGIP estimates
- Pressure transient analysis β controls total system compressibility
- Reservoir simulation β impacts fluid expansion and pressure behavior
- Stress-sensitive reservoirs β unconsolidated sands and high-porosity formations
- Compaction drive β contributes to reservoir energy
This document covers empirical correlations for estimating formation compressibility from basic rock properties.
Theory
Definition
Rock compressibility is defined as the fractional change in pore volume per unit change in pressure:
Where:
- = formation (rock) compressibility, psiβ»ΒΉ
- = pore volume, ftΒ³
- = pressure, psia
- = temperature (constant)
The negative sign ensures is positive, as pore volume decreases with increasing pressure.
Physical Significance
Rock compressibility varies widely:
| Rock Type | Typical Range (10β»βΆ psiβ»ΒΉ) | Behavior |
|---|---|---|
| Consolidated sandstone | 3-10 | Relatively stiff, low compressibility |
| Friable sandstone | 10-25 | Moderate compressibility |
| Unconsolidated sand | 25-100+ | Highly compressible, stress-sensitive |
| Dense limestone | 1-5 | Very stiff, minimal compressibility |
| Vuggy/fractured carbonate | 5-15 | Fracture closure dominates |
| Chalk | 10-50 | High compressibility, prone to compaction |
Key Dependencies:
- Decreases with pressure β pore space becomes stiffer as it compacts
- Increases with porosity β higher porosity = more compressible
- Depends on lithology β grain packing and cementation
- Affected by overburden stress β shallow reservoirs more compressible
Total System Compressibility
In reservoir engineering, formation compressibility combines with fluid compressibility:
Where:
- = total system compressibility, psiβ»ΒΉ
- , , = oil, water, gas compressibility, psiβ»ΒΉ
- , , = oil, water, gas saturation, fraction
Typical Magnitudes:
- Oil: psiβ»ΒΉ
- Water: psiβ»ΒΉ
- Gas: psiβ»ΒΉ (highly pressure-dependent)
- Rock: psiβ»ΒΉ
Important: In gas reservoirs, so rock compressibility is often negligible. In oil reservoirs, can be significant, especially for unconsolidated formations.
Hall (1953) Correlation
Hall developed an early - correlation using limited data. This correlation is included for historical completeness but has been superseded by Newman's more comprehensive work.
Where:
- = formation compressibility, psiβ»ΒΉ
- = formation porosity, fraction
Data Range:
- Porosity:
- Sample size: 12 samples (7 limestones, 5 sandstones)
Limitations: Limited data range and poor to fair accuracy. Use Newman's correlations for better results.
Newman (1973) Correlations
Newman developed empirical correlations for pore volume compressibility using extensive laboratory data on consolidated sandstones and limestones. The data were fit with hyperbolic equations providing improved accuracy over earlier correlations.
Newman Sandstone Correlation
For consolidated sandstones, Newman used 79 samples to develop:
Where:
- = formation porosity, fraction
- = formation compressibility, psiβ»ΒΉ
Data Range:
- Porosity:
- Sample size: 79 consolidated sandstone samples
- Average absolute error: 2.60%
Application: Best for consolidated sandstones with moderate to low porosity. For unconsolidated sands, expect higher compressibility than predicted.
Newman Limestone Correlation
For limestones (carbonates), Newman developed a separate correlation:
Where:
- = formation porosity, fraction
- = formation compressibility, psiβ»ΒΉ
Data Range:
- Porosity:
- Sample size: Limestone samples
- Average absolute error: 11.8%
Application: Suitable for dense to moderately porous limestones. Higher error reflects natural variability in carbonate pore structures (vugs, fractures).
Applicability and Limitations
When to Use Correlations
β Recommended:
- Preliminary reservoir studies
- Material balance calculations when lab data unavailable
- Sensitivity analysis on impact
- Quick estimates for well test analysis
β Not Recommended:
- Critical compaction drive reservoirs (use lab measurements)
- Geomechanical modeling (requires stress-strain curves)
- Subsidence prediction (needs comprehensive geomechanics)
Laboratory Measurements Preferred
For accurate values, laboratory measurements on core samples are essential:
- Uniaxial strain test β simulates overburden conditions
- Hydrostatic test β equal confining pressure on all sides
- Stress cycling β captures hysteresis effects
Newman correlations provide estimates only. Use lab data when available.
Functions Covered
| Function | Description | Returns |
|---|---|---|
| CfNewmanS | Newman sandstone formation compressibility | , psiβ»ΒΉ |
| CfNewmanL | Newman limestone formation compressibility | , psiβ»ΒΉ |
Note: Excel function syntax and parameter details are available on individual function pages.
Related Topics
- SCAL Overview β Special core analysis property selection
- Oil Compressibility β Oil compressibility correlations
- PTA Dimensionless Variables β Total compressibility in well testing
References
-
McCain, W.D., Jr. (1991). "Reservoir-Fluid Property CorrelationsβState of the Art." SPE Reservoir Engineering, May 1991, 266-272. [Available: theory/references/classes/PDF_P324_06A_(for_class)_Lec_Mod1_02a_FluidProp.md]
-
Hall, H.N. (1953). "Compressibility of Reservoir Rocks." Transactions of the AIME, 198, 309-311.
-
Newman, G.H. (1973). "Pore-Volume Compressibility of Consolidated, Friable, and Unconsolidated Reservoir Rocks Under Hydrostatic Loading." Journal of Petroleum Technology, June 1973, SPE-3835-PA.
Related Reading
For background on rock compressibility:
- Craft, B.C., Hawkins, M., and Terry, R.E. (2014). Applied Petroleum Reservoir Engineering. Prentice Hall.
- Ahmed, T. (2019). Reservoir Engineering Handbook. Gulf Professional Publishing.
- Dake, L.P. (1978). Fundamentals of Reservoir Engineering. Elsevier.
- Zimmerman, R.W. (1991). Compressibility of Sandstones. Elsevier.
Typical Values Reference Table
For quick reference when lab data and correlations are unavailable:
| Formation Description | Porosity (%) | Typical (10β»βΆ psiβ»ΒΉ) |
|---|---|---|
| Very consolidated sandstone | 10-15 | 3-6 |
| Consolidated sandstone | 15-20 | 6-10 |
| Moderately consolidated sandstone | 20-25 | 10-15 |
| Friable sandstone | 25-30 | 15-25 |
| Unconsolidated sand | 30-40 | 25-100 |
| Dense limestone/dolomite | 5-10 | 1-4 |
| Limestone | 10-20 | 4-10 |
| Vuggy carbonate | 15-25 | 8-15 |
| Chalk | 20-40 | 10-50 |
Source: Typical ranges from industry experience. Use Newman correlations for more specific estimates.
Document Status
| Aspect | Status |
|---|---|
| Functions identified | β Complete (2 functions) |
| Primary references | β Available in class materials |
| Equations documented | β Complete |
| Examples provided | β³ To be added |
| Typical values table | β Provided for quick reference |
| Last updated | 2025-12-03 |
Status: π Ready for Review β Correlations documented from McCain class materials. Awaiting technical review and validation against implementation.