Author/Authors :
Ikeya، Motoji نويسنده , , Satoh، Hideo نويسنده , , Ikuta، Ryouya نويسنده , , Yamanaka، Chihiro نويسنده ,
Abstract :
Propagation of electromagnetic (EM) waves from an earthquake focus in the conductive Earth has been investigated using 1/1,000,000 scaling models taking earth-ionosphere and ocean-Moho plane parallel-plate waveguides into account. Microwaves at a frequency, m, a million times higher than that of seismic EM signal (SEMS), , were generated at the model focus. They are propagated in a salt solution modeling the earthʹs crust and reflected by ocean, fault planes, ionosphere and Moho plane all made by aluminum. Distribution of EM power was mapped by scanning a detector antenna over the model Earthʹs surface. The skin depth, , calculated by the exact skin depth equation, 1/=(/2)1/2 [(1+(1/omega epsilonrho)2)1/2 -1]1/2 where dielectric constant, epsilonand permeability, MUare the same but resistivity, RHO, 10-6 times smaller than that of Earth, gave 10-6 times small skin depth validating the model scaling index. Images for evanescent and wave-ripple standing waves disturbed by normal, strike-slip and dip-slip conductive fault planes have been obtained using an aluminum plate. The co-circular contour map above the epicenter due to evanescence was pushed to the north east direction from the epicenter by the presence of ocean for the Loma Prieta earthquake, while to north direction for the Kobe earthquake. The intensity of EM ULF emissions for the Loma Prieta earthquake is discussed quantitatively.
Keywords :
anticholinergics , latency , cholinergic system , startle , prepulse inhibition