Theory

Rock Compressibility Correlations

Overview

Rock compressibility (cfc_f) 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:

cf=βˆ’1Vp(βˆ‚Vpβˆ‚p)Tc_f = -\frac{1}{V_p} \left(\frac{\partial V_p}{\partial p}\right)_T

Where:

  • cfc_f = formation (rock) compressibility, psi⁻¹
  • VpV_p = pore volume, ftΒ³
  • pp = pressure, psia
  • TT = temperature (constant)

The negative sign ensures cfc_f is positive, as pore volume decreases with increasing pressure.


Physical Significance

Rock compressibility varies widely:

Rock TypeTypical cfc_f Range (10⁻⁢ psi⁻¹)Behavior
Consolidated sandstone3-10Relatively stiff, low compressibility
Friable sandstone10-25Moderate compressibility
Unconsolidated sand25-100+Highly compressible, stress-sensitive
Dense limestone1-5Very stiff, minimal compressibility
Vuggy/fractured carbonate5-15Fracture closure dominates
Chalk10-50High 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:

ct=cf+Soco+Swcw+Sgcgc_t = c_f + S_o c_o + S_w c_w + S_g c_g

Where:

  • ctc_t = total system compressibility, psi⁻¹
  • coc_o, cwc_w, cgc_g = oil, water, gas compressibility, psi⁻¹
  • SoS_o, SwS_w, SgS_g = oil, water, gas saturation, fraction

Typical Magnitudes:

  • Oil: coβ‰ˆ10βˆ’20Γ—10βˆ’6c_o \approx 10-20 \times 10^{-6} psi⁻¹
  • Water: cwβ‰ˆ3Γ—10βˆ’6c_w \approx 3 \times 10^{-6} psi⁻¹
  • Gas: cgβ‰ˆ100βˆ’1000Γ—10βˆ’6c_g \approx 100-1000 \times 10^{-6} psi⁻¹ (highly pressure-dependent)
  • Rock: cfβ‰ˆ3βˆ’25Γ—10βˆ’6c_f \approx 3-25 \times 10^{-6} psi⁻¹

Important: In gas reservoirs, cg≫cfc_g \gg c_f so rock compressibility is often negligible. In oil reservoirs, cfc_f can be significant, especially for unconsolidated formations.


Hall (1953) Correlation

Hall developed an early cfc_f-Ο•\phi correlation using limited data. This correlation is included for historical completeness but has been superseded by Newman's more comprehensive work.

cf=1.86Γ—10βˆ’6Ο•βˆ’0.415c_f = 1.86 \times 10^{-6} \phi^{-0.415}

Where:

  • cfc_f = formation compressibility, psi⁻¹
  • Ο•\phi = formation porosity, fraction

Data Range:

  • Porosity: 0.20<Ο•<0.260.20 < \phi < 0.26
  • 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:

cf=a(1+bcΟ•)1/bc_f = \frac{a}{(1 + bc\phi)^{1/b}}

Where:

  • a=97.3200Γ—10βˆ’6a = 97.3200 \times 10^{-6}
  • b=0.699993b = 0.699993
  • c=79.8181c = 79.8181
  • Ο•\phi = formation porosity, fraction
  • cfc_f = formation compressibility, psi⁻¹

Data Range:

  • Porosity: 0.02<Ο•<0.230.02 < \phi < 0.23
  • 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:

cf=a(1+bcΟ•)1/bc_f = \frac{a}{(1 + bc\phi)^{1/b}}

Where:

  • a=0.853531a = 0.853531
  • b=1.07538b = 1.07538
  • c=2.30304Γ—106c = 2.30304 \times 10^6
  • Ο•\phi = formation porosity, fraction
  • cfc_f = formation compressibility, psi⁻¹

Data Range:

  • Porosity: 0.02<Ο•<0.330.02 < \phi < 0.33
  • 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

βœ… Recommended:

  • Preliminary reservoir studies
  • Material balance calculations when lab data unavailable
  • Sensitivity analysis on cfc_f impact
  • Quick estimates for well test analysis

❌ 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 cfc_f 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

FunctionDescriptionReturns
CfNewmanSNewman sandstone formation compressibilitycfc_f, psi⁻¹
CfNewmanLNewman limestone formation compressibilitycfc_f, psi⁻¹

Note: Excel function syntax and parameter details are available on individual function pages.



References

  1. McCain, W.D., Jr. (1991). "Reservoir-Fluid Property Correlationsβ€”State of the Art." SPE Reservoir Engineering, May 1991, 266-272. [Available: theory/references/classes/PDF_P324_06A_(for_class)_Lec_Mod1_02a_FluidProp.md]

  2. Hall, H.N. (1953). "Compressibility of Reservoir Rocks." Transactions of the AIME, 198, 309-311.

  3. 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.

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 DescriptionPorosity (%)Typical cfc_f (10⁻⁢ psi⁻¹)
Very consolidated sandstone10-153-6
Consolidated sandstone15-206-10
Moderately consolidated sandstone20-2510-15
Friable sandstone25-3015-25
Unconsolidated sand30-4025-100
Dense limestone/dolomite5-101-4
Limestone10-204-10
Vuggy carbonate15-258-15
Chalk20-4010-50

Source: Typical ranges from industry experience. Use Newman correlations for more specific estimates.


Document Status

AspectStatus
Functions identifiedβœ… Complete (2 functions)
Primary referencesβœ… Available in class materials
Equations documentedβœ… Complete
Examples provided⏳ To be added
Typical values tableβœ… Provided for quick reference
Last updated2025-12-03

Status: πŸ‘€ Ready for Review β€” Correlations documented from McCain class materials. Awaiting technical review and validation against implementation.

Special Core Analysis
scalrock-compressibilitypore-compressibilitynewmanformation-compressibility

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2 items

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