Bulk Modulus Calculator

Calculate bulk modulus from pressure and volume changes or look up values for common materials. Includes compressibility and stiffness comparison chart.

Pa
Bulk Modulus (K)
2.198e+9 Pa
K = −V × ΔP / ΔV
Bulk Modulus
2.198 GPa
In gigapascals
Compressibility (β)
4.550e-10 Pa⁻¹
β = 1/K — reciprocal of bulk modulus
Volumetric Strain
0.4550%
|ΔV/V| × 100
Speed of Sound (est.)
1,482 m/s
Rough estimate: √(K/ρ) with ρ = 1000 kg/m³
K in PSI
318,764
Bulk modulus in pounds per square inch

Stiffness Comparison

Water
1.4%
Steel
100.0%
Aluminum
47.5%
Copper
87.5%
Glass
21.9%
Rubber
1.3%
Mercury
17.8%
Glycerin
2.7%
Ethanol
0.7%

Bulk Modulus of Common Materials

MaterialK (GPa)K (psi × 10⁶)
Water2.200.32
Steel160.0023.21
Aluminum76.0011.02
Copper140.0020.31
Glass35.005.08
Rubber2.000.29
Mercury28.504.13
Glycerin4.350.63
Ethanol1.060.15
Planning notes, formulas, and examples

About the Bulk Modulus Calculator

Bulk modulus (K) measures a material's resistance to uniform compression—how much pressure is needed to produce a given fractional volume change. It is defined as K = −V × ΔP / ΔV, where V is the original volume, ΔP is the pressure change, and ΔV is the resulting volume change (negative for compression).

Materials with high bulk modulus, like steel (160 GPa) and diamond (443 GPa), are nearly incompressible, while liquids like water (2.2 GPa) and gases are far more compressible. The reciprocal of bulk modulus is compressibility (β = 1/K), frequently used in fluid mechanics and reservoir engineering.

This calculator offers two modes: compute K directly from measured pressure and volume changes, or look up known bulk modulus values for common materials. Results include compressibility, volumetric strain, an estimated speed of sound, and a visual stiffness comparison across materials.

When This Page Helps

Engineers designing hydraulic systems, pressure vessels, and subsea equipment need accurate bulk modulus values to predict volume changes under pressure. Geophysicists use K to model seismic wave propagation through the Earth, and materials scientists measure K to characterize new alloys and composites.

This calculator saves time by combining direct measurement calculations with a material database and visual comparisons, eliminating the need to look up values across multiple reference sources.

How to Use the Inputs

  1. Select a preset scenario or choose a calculation mode.
  2. For "pressure & volume change" mode: enter original volume, pressure change (ΔP), and volume change (ΔV).
  3. For "material database" mode: select a material to look up its bulk modulus.
  4. Choose the appropriate pressure unit (Pa, MPa, GPa, or PSI).
  5. View the bulk modulus, compressibility, volumetric strain, and comparison chart.
  6. Use the reference table to compare your material against common substances.
Formula used
Bulk Modulus: K = −V × ΔP / ΔV (Pa or GPa). Compressibility: β = 1/K (Pa⁻¹). Volumetric strain: ε_v = ΔV/V (dimensionless). Speed of sound estimate: c ≈ √(K/ρ).

Example Calculation

Result: 2.198 × 10⁹ Pa (2.198 GPa)

For water: K = −1 × 10,000,000 / (−0.00455) = 2.198 × 10⁹ Pa ≈ 2.2 GPa, matching the known bulk modulus of water.

Tips & Best Practices

  • For hydraulic oil, K is typically 1.4–1.8 GPa; entrained air can reduce it dramatically.
  • Diamond has the highest bulk modulus of any common material at about 443 GPa.
  • Use isothermal K for slow compression and adiabatic K for rapid (acoustic) compression.
  • Bulk modulus relates to Young's modulus E and Poisson's ratio ν via K = E / (3(1−2ν)).
  • In reservoir engineering, rock compressibility β_r is typically 3–25 × 10⁻¹⁰ Pa⁻¹.
  • Pressure-dependent K values are needed for deep-earth modeling—K increases with depth.

Relationship Between Elastic Constants

For isotropic materials, only two independent elastic constants are needed. The bulk modulus K, Young's modulus E, shear modulus G, and Poisson's ratio ν are all interrelated:

- K = E / [3(1 − 2ν)] - K = 2G(1 + ν) / [3(1 − 2ν)] - G = 3KE / (9K − E)

These relationships mean that measuring any two constants determines all others—a powerful tool in materials characterization.

Bulk Modulus in Practice

**Hydraulics:** Hydraulic fluid stiffness determines system response speed. Air contamination (even 1% by volume) can halve the effective bulk modulus, causing spongy controls and delayed actuator response.

**Ocean Engineering:** At the deepest ocean trenches (≈110 MPa), water compresses roughly 5%. Equipment and instrument housings must be designed for this volume change to avoid seal failures.

**Geophysics:** Seismic P-wave velocity depends on the bulk modulus of rock: V_p = √((K + 4G/3)/ρ). Measuring wave speeds thus reveals subsurface material properties.

Temperature and Pressure Effects

Most materials become stiffer (higher K) under compression and softer (lower K) at higher temperatures. Rubbers and polymers show especially strong temperature dependence, with K dropping by 50% or more between 0 °C and 100 °C. Metals are comparatively stable, varying only 5–10% over the same range.

Sources & Methodology

Last updated:

Frequently Asked Questions

  • Young's modulus measures resistance to uniaxial stretching or compression (one direction), while bulk modulus measures resistance to uniform compression from all directions. They are related through Poisson's ratio.