Solve isotropic elasticity constants from flexible material inputs. View derived moduli, ratios, checks, and charts. Export clean results for labs, homework, reports, and notes.
Overall page stays single-column. The calculator fields use 3 columns on large screens, 2 on smaller screens, and 1 on mobile.
| Material | E (GPa) | ν | λ (GPa) | μ = G (GPa) | K (GPa) |
|---|---|---|---|---|---|
| Steel | 210.00 | 0.30 | 121.15 | 80.77 | 175.00 |
| Aluminum | 69.00 | 0.33 | 50.88 | 25.94 | 68.17 |
| Rubber-like solid | 0.010 | 0.49 | 0.164 | 0.0034 | 0.167 |
Stability for isotropic elasticity requires μ > 0 and 3λ + 2μ > 0. These conditions also imply positive shear and bulk response.
Lamé parameters are two elastic constants for isotropic linear materials. The first is λ, linked to volumetric response. The second is μ, also called shear modulus, linked to resistance against shape change.
In isotropic elasticity, the second Lamé parameter directly measures resistance to shear deformation. Because of that, μ and G describe the same physical property and always have identical numeric values.
Yes. A material can have negative λ and still remain physically admissible, provided μ stays positive and the bulk condition 3λ + 2μ > 0 also remains satisfied.
Poisson’s ratio measures lateral strain relative to axial strain. Values near 0.5 suggest nearly incompressible behavior, while lower values indicate stronger volume change under loading.
Density allows the calculator to convert elastic constants into seismic or ultrasonic wave speeds. With ρ, the page can compute shear-wave velocity Vs and compressional-wave velocity Vp.
Choose the mode that matches your available lab, textbook, or simulation data. E and ν are common in mechanics, K and G are common in constitutive models, and Vp, Vs, ρ are common in geophysics.
The P-wave modulus is M = λ + 2μ. It controls compressional wave propagation in isotropic solids and is also equal to ρVp² when density and P-wave speed are known.
They are useful in continuum mechanics, finite element modeling, acoustics, seismology, materials science, and structural analysis wherever isotropic elastic stress-strain behavior must be converted between equivalent material constants.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.