How to compute the energy released by an earthquake.

How to compute the energy released by an earthquake.

To determine the total seismic energy radiated from an earthquake one would have to integrate the energy radiated at all frequencies over the entire focal sphere. The spectrum of the average radiation over the focal sphere can be approximated by a constant level at low frequencies (which is proportional to the moment, M_o) and a uniform decrease with increasing frequency above some corner frequency (F_c), so the seismic energy is a function of both M_o and F_c. For a given moment, the radiated energy will increase as F_c increases. Consider, for example, two earthquakes with the same displacement and rupture area that occur within rocks with the same shear modulus. They would have the same moment, which can be computed from:

M_o = u D A

where:

          u = shear modulus (3 - 6 x 10¹¹) dyn/cm²

          D = average displacement

          A = area of rupture

If one event were a "slow" earthquake with "more or less creep-like deformation" (Kanamori, H., 1972, Mechanism of Tusnami Earthquakes, Phys. Earth Planet. Interiors, v6, p. 346-359) while the other had a more typical rupture velocity near the shear wave velocity, much more energy would be radiated from the latter earthquake due to its rich high frequency radiation corresponding larger F_c than from the "slow" event.

Having said this, however, if only an earthquake's moment is known the radiated seismic energy can still be approximated because, if a large set of earthquakes is considered, the average corner frequency varies systematically with the moment. For the average earthquake, the seismic wave energy (E), moment (M_o) and moment magnitude (M_W) are related by the following equations (Kanamori, H., 1977, The Energy Release in Great Earthquakes, Journal of Geophysical Research, v82, p. 2981- 2987):

     E = M_o/(2 x 10⁴) erg   (1 erg = 1 dyn cm)

     log E = 1.5 M_W + 11.8 (Gutenberg-Richter magnitude-energy relation)

Then:

     log M_o - log(2 x 10⁴) = 1.5 M_W + 11.8

     M_w = (log M_o - 16.1) / 1.5

The energy released by TNT (trinitrotoluene) and the TNT equivalent of the Hiroshima nuclear bomb (McGraw-Hill Encyclopedia of Science and Technology, 1992):

     Energy per ton of TNT     = 4.18 x 10⁹ Joules

                               = 4.18 x 10¹⁶ ergs

     Energy per megaton of TNT = 4.18 x 10¹⁵ Joules

According to the Sandia National Laboratories' web site, the energy equivalent of the Hiroshima fission bomb was 15,000 tons of TNT.

Example -- consider an earthquake with moment magnitude Mw = 4.0

The total seismic energy radiated from the source, E(4), would be:

        E(4) = 10**(1.5*4 + 11.8) = 10**17.8 ergs = 10**10.8 Joules = 6.3 x 10¹¹ Joules

The moment, Mo(4), would be:

        Mo(4) = E x (2 x 10⁴) = 1.26 x 10¹⁶ Joules

It has been found that a 1 kton explosion will generate seismic waves approximately equivalent to a magnitude 4 earthquake.  Therefore, the amount of energy dissipated by TNT to yield seismic waves similar to a magnitude 4 is:

        Energy of TNT(4) = 4.18 x 10¹² Joules

Reference:  http://www.cwp.mines.edu/~john/empirical/node4.html