Propagation of Love wave is influenced by initial stress parameters, corrugation parameter and porosity of half-space.
In this theoretical study, we investigate the propagation of Love waves in a layered structure consisting of two different homogenous piezoelectric materials, an upper layer and a substrate.
The effects of fracture porosity and fracture permeability on the behavior of the propagation of Love waves are investigated in detail.
The propagation of Love waves in layered structures is investigated for two cases: a piezomagnetic (PM) layer on a piezoelectric (PE) half-space and the reverse configuration.
Based on the control equations for double-porosity media extended from Biot's theory, the propagation of Love waves is discussed in this paper.
To clarify the cause of the observed stable propagation of Love waves in the inhomogeneous Kanto Basin, we examined the detailed period dependency of the Love wave group velocity beneath the linear array.
The Direct Sturm Liouville Problem that describes the propagation of Love waves in nonhomogeneous elastic functionally graded materials is formulated and solved by using two methods: i.e., (1) Finite Difference Method, and (2) Haskell-Thompson Transfer Matrix Method.
Synaptically activated, IP 3-mediated propagation of Ca 2+ release has been observed in pyramidal neurons in the rodent hippocampus (CA1 and CA3 regions), medial prefrontal cortex and principal neurons in the amygdala.
The latter three values are basically consistent with the propagation of the Earth's surface waves reported in several previous studies.
Most papers reported that the disturbances propagated away from the epicenter with a velocity of 2 4 km/s, corresponding to the propagation of the Earth's surface waves (Rayleigh waves).
