Definition

T he relationship of elastic longitudinal wave (Vp-waves) velocity to shear wave (Vs-waves) velocity or the relationship of elastic shear wave (Vs-waves) velocity to longitudinal wave (Vp-waves) velocity.

Characteristics

In engineering seismology, the velocity ratio Vp/Vs (TAU parameter) is considered as an indicator of the changes in stress state of rocks in the process of development of strong tectonic and volcanic earthquakes. It is established that deep fault zones, named gradiental zones, display rapid changes in the ratio Vp/Vs with a change of the anomalies’ sign (positive or negative). These can be considered as seismogenic zones. Relatively low values of Vp/Vs ratio indicate increases in activity in the magmatic chambers of volcanos during their activization. The ratio of Vp-waves velocity to Vs-waves velocity (Vp/Vs) is used in engineering seismology and engineering geology (Slavina et al. 2015).

The ratio of Vp-waves velocity to Vs-waves velocity (Vp/Vs) is used in engineering seismology and engineering geology. In engineering geology, the velocity ratios Vs/Vp and Vp/Vs аre used for definition of physic-technical characteristics of rocks. If the values of both ratios are known, it is possible to define dynamic modules of elasticity – Poisson’s ratio μ, the Young’s modulus E, and the shift modulus G. These characteristics are of interest at carrying out engineering surveys for construction. To define the Poisson’s ratio μ, it is necessary to know Vs/Vp or Vp/Vs ratios only; for definition of the Young’s modulus E and the shift modulus, G it is necessary to know also the density of rocks. For definition of static modulus necessary for engineering calculations, empirical ratios or special diagrams are used (Nikitin 1981; Bondarev 1997).

Cross-References