whats up here? Hrvoje Zujić, Mr.E.Eng. June, 2013. Independent researcher, Osijek, Croatia ELECTROMAGNETIC MECHANISM OF THE ULTRASOUNDON THE BOSNIAN PYRAMID OF THE SUN (VISOČICA HILL) ABSTRACT Dr. Slobodan Mizdrak registered the EM signal at 28 kHz at the top of The Bosnian Pyramid of The Sun(Visočica) in April of 2011. After him, researchers Dr. Paolo Debertolis, Heikki Savolainen B.E.E., Davor Jadrijević B.E.E., Goran Marjanović B.E.E., Goran Samouković B.E.E. and others confirmed the results of dr.Mizdrak. Computer simulations of electric potential, direction and magnitude of electric field reveal to us anelectromagnetic mechanism that generates the ultrasound. The computer simulations were made with ANSOFTMAXWELL ® 2D version 14.0. KEY TAGS: Ultrasound, VLF-atmospheric, 28 kHz, Bosnian Pyramid of The Sun, pyramid, Visoko, Visočica,Slobodan Mizdrak, Paolo Debertolis, Hrvoje Zujić, Disk, Ansoft, Maxwell, Tesla, Klaus Dona, Probe 10 ABOUT THE AUTOR Born 1970 in Osijek,Croatia; master degree of electrical engineering from the University of Zagreb;authorized engineer of electrical engineering for the design and control of electric installations;member of the Class of electrical engineers of Croatian Chamber of Engineers.Specialties: electrical resistivity tomography (ERT), spontaneous potential (SP), tomography of aeroionic current density, computer simulations of electromagnetic processes with the applicationsANSOFT MAXWELL, AUTODESK MAYA, 3D MAX. INTRODUCTION I hypothesize that the source of the registered EM signal of 28kHz is the VLF-atmospheric. VLF-atmospherics are electromagnetic impulses that are emitted during thunderstorms. Generated by lightningdischarges, they propagate with approximately the speed of light through the atmospheric waveguide which isformed by the earth’s surface and the lower ionosphere. During their propagation, VLF-atmospherics undergo pronounced changes with regard to their amplitude and frequency composition, due to dispersion and dampeningeffects. With increasing distance from their place of origin, both the higher and the lower frequency componentsdecrease. Since the VLF-atmospheric waveguide functions similar to that of a band pass filter for frequenciesaround 10 kHz, this component undergoes minimal attenuation during the signal’ s propagation.Atmospherics are characterized by very low amplitudes and short durations. Common signal intensities arein the nano Tesla range. The duration of a VLF-atmospherics impulse is on average 0.5 ms (Betz et al., 1996). Thesignal features such as amplitude, frequency composition, waveform and duration primarily depend upon the kindof discharge, the distance between source and detector, and the conditions of transmission within the atmosphere.Due to their origin in atmospheric discharges, atmospherics can be used for detection of lightning and localizationof thunderstorm areas. The number of recorded impulses per time unit is an indicator of thunderstorm activity,which shows typical daily as well as seasonal variations. The highest pulse frequencies in mid-European countriescan be registered during summer afternoons. A second peak occurs around midnight, which is present for most of the year (see Figure 1 bpblognews.blogspot.nl/
Posted on: Thu, 21 Nov 2013 06:32:27 +0000
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