A2 l 2µ r. The first type of wave to consider when determining the epicenter of an earthquake is the P-wave. Piezometric transducers contain materials which contract and expand in response to an applied voltage.
By measuring a P-wave transmission time and an S-wave transmission time with Pundit Lab we are able to determine the P-wave modulus M and the Shear modulus G.
Dix The interval velocity Vi is the velocity in a single layer which can be determined from sonic logs or laboratory measurements on cores from. The wave velocity v is the velocity at which the shape of the wave propagates in space. Use A Poissons Ratio Of 03 Velocity Of Seismic Waves A k3 Kustiano Wa MS Ng 3 1-2v 20 2 1 Q. In this lesson we calculate v based on l and f.