Calculate compressibility, bulk modulus, volume change, speed of sound, Mach number, and acoustic impedance for any material. Compare fluids, gases, and solids.
The **Compressibility Calculator** determines how much a material's volume changes under pressure. Enter the bulk modulus, density, and applied pressure change, and the calculator returns the compressibility coefficient, fractional volume change, speed of sound, Mach number, density change, acoustic impedance, and strain energy density.
Compressibility is the reciprocal of the bulk modulus — a measure of a material's resistance to uniform compression. Gases are highly compressible; liquids are nearly incompressible; solids even less so. Understanding compressibility is critical in fluid mechanics (water hammer, hydraulic systems), acoustics (sound propagation), aerodynamics (shock waves above Mach 0.3), geophysics (seismic waves), and materials science.
Use the presets for water, air, steel, oil, seawater, and rubber, and refer to the materials comparison table to see how compressibility, sound speed, and acoustic impedance vary across orders of magnitude. Seeing those outputs together is useful when you need to decide whether the incompressible assumption is still reasonable for the material and pressure range you are using.
Use this page when you need to move from bulk modulus and density to practical outputs like volume change, sound speed, Mach number, and acoustic impedance. It is a quick way to connect a material property value to the flow, wave, or loading consequences that actually matter in design checks.
Compressibility: β = 1/K Volume Change: ΔV/V = −ΔP/K Speed of Sound: c = √(K/ρ) Mach Number: Ma = v/c Acoustic Impedance: Z = ρc Strain Energy: u = ΔP²/(2K)
Result: β = 4.55×10⁻¹⁰ Pa⁻¹, ΔV/V = 0.045%, c = 1 484 m/s
Water has a bulk modulus of 2.2 GPa. A 1 MPa pressure increase compresses it by just 0.045% — effectively incompressible for most engineering purposes. Sound travels at 1 484 m/s.
Compressibility links pressure loading to volume change. In gases that effect is obvious, but in liquids and solids it is small enough that many engineering models treat them as incompressible unless pressures become large or wave motion matters.
The same stiffness that resists compression also controls how fast pressure disturbances travel. That is why bulk modulus and density combine into the speed of sound and why compressibility shows up in acoustics, hydraulics, aerodynamics, and geophysics.
A single bulk modulus is often a simplification. Real materials can have temperature dependence, pressure dependence, or nonlinear behavior. Use the result as a first-pass property calculation unless you have a material-specific equation of state.
The fractional decrease in volume per unit increase in pressure. Higher compressibility means the material squeezes more easily under the same pressure change. Low compressibility means the same pressure produces only a small volume change.
The resistance to uniform compression — the reciprocal of compressibility. Higher K means stiffer (less compressible) material. Lower K means the same pressure change produces a larger volume change.
Sound is a pressure wave. A stiffer material (higher K) transmits the wave faster: c = √(K/ρ). That is why liquids and solids usually carry sound faster than gases.
When Mach number exceeds about 0.3 and density changes are no longer negligible. Below Ma 0.3, the incompressible assumption is usually adequate for first-pass work.
Z = ρc determines how much sound is reflected at an interface between two materials. Mismatched impedance causes strong reflections, which is why interfaces matter so much in ultrasound and acoustics.
In many materials, increasing temperature reduces stiffness and increases compressibility, but the exact trend depends on the phase and material model you are using. The effect is often small in simple estimates but can matter in high-accuracy property work.