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Flexural rigidity of a bar
Flexural rigidity of a plate (e.g. the lithosphere)
The thin lithospheric plates which cover the surface of the Earth are also subject to flexure, when a load or force is applied to them. On a geological timescale, the lithosphere behaves elastically (in first approach) and can therefore bend under loading by mountain chains, volcanoes and so on.
The flexure of the plate depends on:
- The plate thickness (usually referred to as mechanical thickness of the lithosphere).
- The elastic properties of the plate
- The applied load or force
As flexural rigidity of the plate is determined by the Young's modulus, Poisson's ratio and cube of the plate's elastic thickness, it is a governing factor in both (1) and (2).
= Young's Modulus
= elastic thickness (~10–15 km)
= Poisson's Ratio
Flexural rigidity of a plate has units of Pa·m3, i.e. one dimension of length less from the one for the rod, as it refers to the moment per unit length per unit of curvature, and not the total moment. I is termed as moment of inertia.J is denoted as 2nd moment of inertia/polar moment of inertia.
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