Shear Wave Velocity Calculator

Calculate the shear wave (S-wave) velocity in a material from its shear modulus and density. Essential for seismology, geotechnical engineering, and non-destructive testing.

SHEAR WAVE VELOCITY (Vs)
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Vs (m/s)
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Vs (km/s)
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Vp/Vs Ratio
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Est. P-Wave Vp
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What Is Shear Wave Velocity?

Shear wave velocity (Vs) is the speed at which shear waves (also called S-waves or secondary waves) propagate through a material. Unlike compression waves (P-waves), shear waves involve particle motion perpendicular to the direction of wave propagation and cannot travel through fluids because fluids have zero shear modulus.

Shear wave velocity is a critical parameter in seismology for characterizing earthquake ground motion, in geotechnical engineering for site classification, and in materials science for non-destructive evaluation of material properties. The Vs30 (average shear wave velocity in the top 30 meters) is widely used in building codes for seismic site classification.

The Formula

Vs = √(G / ρ)
Vp/Vs = √((2-2ν)/(1-2ν))

Where G is the shear modulus in Pa, ρ is the density in kg/m³, and ν is Poisson's ratio. The Vp/Vs ratio depends only on Poisson's ratio and is typically 1.7-1.8 for most rocks.

Typical Values for Materials

MaterialVs (m/s)Density (kg/m³)G (GPa)
Soft soil / clay100-3001,600-1,9000.02-0.2
Sand (dense)200-5001,700-2,1000.1-0.5
Sandstone800-2,0002,200-2,7004-15
Granite2,500-3,3002,600-2,80020-30
Steel3,1007,85079.3
Aluminum3,1002,70026

Applications

  • Seismic site classification: Vs30 determines the site class (A through F) in building codes like ASCE 7 and Eurocode 8.
  • Earthquake engineering: ground motion prediction equations use Vs to estimate shaking intensity.
  • Geotechnical investigation: MASW (Multichannel Analysis of Surface Waves) and downhole tests measure Vs profiles.
  • Non-destructive testing: ultrasonic shear wave measurements determine material elastic properties without cutting samples.

Frequently Asked Questions

Why can't shear waves travel through liquids?

Liquids and gases have zero shear modulus because they cannot sustain shear stress -- they simply flow. Since Vs = sqrt(G/ρ) and G = 0 for fluids, the shear wave velocity is zero. This is why S-waves from earthquakes are not detected through the Earth's liquid outer core, creating the S-wave shadow zone.

What is Vs30 and why is it important?

Vs30 is the time-averaged shear wave velocity in the upper 30 meters of soil. It is calculated as 30 divided by the total travel time of a shear wave through those 30 meters. Building codes worldwide use Vs30 to classify sites for seismic design, with higher values indicating stiffer (safer) ground conditions.

How is Vp/Vs ratio used in seismology?

The Vp/Vs ratio helps identify rock types and fluid content. Water-saturated rocks have higher Vp/Vs ratios than dry rocks. Gas-filled pores reduce Vp but barely affect Vs, lowering the ratio. This makes Vp/Vs a valuable tool in petroleum exploration and reservoir characterization.