For a given type of rock, acoustic velocity varies indirectly with porosity.
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However, the sonographic instrument assumes that the acoustic velocity is constant at 1540 m / s.
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Therefore, any sound field can be reconstructed, if sound pressure and acoustic velocity are restored on all points of the surface of its volume.
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The Christoffel Equation is essentially an eigenvalue problem which relates the elastic tensor, c _ { ijkl }, to the crystal orientation and the orientation of the incident light, \ Lambda _ { kl }, to a matrix, \ lambda _ { kl }, whose eigenvalues are equal to ?V2, where ? is density and V is acoustic velocity ..
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