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Libro de resúmenes [revisión final, 172 páginas] - UGM

Libro de resúmenes [revisión final, 172 páginas] - UGM

Libro de resúmenes [revisión final, 172 páginas] - UGM

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FÍSICA ESPACIAL Geos, Vol. 27, No. 1, Octubre, 2007FE-1SPATIAL DISTRIBUTION AND FREQUENCYSPECTRUM OF ELECTROMAGNETICRADIATION OF A STRUCTURED SPHEREBurlak GennadiyCentro <strong>de</strong> Investigación en Ingeniería y Ciencias Aplicadas, UAEMgburlak@uaem.mxThe electromagnetic radiation to a physical space of electriccurrents from a <strong>de</strong>pth of a structured multilayers sphere isstudied. One of the main properties of such structures is coherentre-reflections of the electromagnetic waves from the interfacesof the layers of the structure. That results in the collectivewave contributions and gives rise to various electromagneticeffects. We explore both frequency and radial <strong>de</strong>pen<strong>de</strong>ncesof the field radiation and have found that in the area ofthe frequency resonances the spherical structure can confinethe electromagnetic fields. Our approach is based on thedyadic Green\'s function technique, which provi<strong>de</strong>s advancedapproximation for dynamical effects in a multilayered sphere.In a system with a few numbers of layers the electromagneticeffects due to the wave re-reflections cannot be appreciated.However our numerical approach has allowed us to apply thedyadic Green\'s function technique to multilayered spheres withany structure of the solid layers. This allows us to evaluate thetotal contribution of various field states in a multilayered spherein the unified framework. We have applied such a technique toa periodic and a quasiperiodic spherical structure. We found thatthe frequency spectrum of radiation consists of series of narrowand well separated peaks. In the band of such peaks the greatpart of the field energy is located in the stack\'s structure andpractically does not leave the sphere. A weak random <strong>de</strong>viationthe thicknesses of spherical layers on a periodic case is alsodiscussed. Such a theory can be useful to study the peculiarityof the spectrum of internal source radiated from Earth to asurrounding space. This work is partially supported by CONACyTgrant 47220.FE-2A POSSIBLE MECHANISM OF MODULATION OFINTENSITY OF ALFVÉN RESONANCES AT THEEARTH’S SURFACE BEFORE EARTHQUAKESGrimalsky Vladimir 1 , Kotsarenko Anatoliy 2 ,Koshevaya Svetlana 1 y Pérez Enríquez Román 21 Universidad Autónoma <strong>de</strong>l Estado <strong>de</strong> Morelos2 Centro <strong>de</strong> Geociencias, UNAMv_grim@yahoo.comRecently, generation of the seismo-related Ultra LowFrequency (ULF, 0.1 – 10 Hz) magnetic perturbations, locallygenerated geomagnetic pulsations, changes in regular resonantstructures was confirmed experimentally by different groundbased observations (our publications). In or<strong>de</strong>r to give thepossible explanation we link mentioned phenomena with amodification of the parameters of the ionosphere (such as<strong>de</strong>nsity and the temperature), which is regularly <strong>de</strong>tected duringsatellite observations over EQ preparation areas (DEMETERProject). Namely, the both fundamental mechanisms of thelithosphere-atmosphere-ionosphere coupling (i.e. coupling throwthe changes in the atmospheric electricity produced as result ofintegrated ionization from the increased radon emanation, andthe conversion of atmospheric acoustic gravity waves (AGW) andinternal gravity (IGW) in the lower ionosphere) can lead to themodulation of the ionosphere parameters, creating transparencyof the ionosphere for a passage of the Alfvén waves, which gofrom the magnetosphere to the Earth surface.We have calculated the efficiency of the modulation of theAlfvén wave at frequencies f = 0.1 – 10 Hz, which passes fromthe magnetosphere (z > 600 km) to the ionosphere and, the to theEarth´s surface and the lithosphere. The set of equations for theelectric field components Ex,y has been solved numerically. Theboundary conditions are as follows. At z = 800 km the amplitu<strong>de</strong>of the downgoing Alfvén wave is assumed as constant (the fieldof the Alfvén resonator), at z = -30 km (in the <strong>de</strong>ep lithosphere)Ex,y = 0. The conductivity of the lithosphere vary between 10^3– 10^5 s-1. It has been obtained that the 20% modulation of theconcentration of the ion and electron concentrations at the heightsz = 200 km can lead to the same (or higher) modulation of theamplitu<strong>de</strong> of the variable magnetic field at the Earth´s surface (z= 0) at f = 0.1 – 10 Hz. Moreover, the effect <strong>de</strong>pends weakly onthe conductivity of the lithosphere. Therefore, an influence of thecoupling mechanisms on the F-layer of the ionosphere could leadto observable effects at the Earth´s surface.FE-3ENERGÍA BALSFIER: PROPUESTA,ANÁLISIS Y DISCUSIÓNTrigo Huesca AlfonsoUniversidad Nacional Autónoma <strong>de</strong> Méxicobalsfier@gmail.comSe presenta la propuesta, análisis y discusión <strong>de</strong> la energíaBalsfier, bajo la premisa <strong>de</strong> hacer confluir en un mismo paradigmalas teorias <strong>de</strong> Newton y Einstein, lo cual consiste en empatar enlas generalida<strong>de</strong>s los conceptos <strong>de</strong> ambas teorías, <strong>de</strong> maneraque empleando las leyes Newtonianas para fabricar instrumentos<strong>de</strong> medición, se realicen mediciones <strong>de</strong> parámetros relativos a lateoría <strong>de</strong> Einstein.Se propone la base teórica para que los instrumentos <strong>de</strong>registro tipo Ayax registren la perturbación en forma <strong>de</strong> ondaproducida por el cúmulo <strong>de</strong> masas que <strong>de</strong>forman el espaciotiempo en una línea <strong>de</strong>finida y constante sobre un punto<strong>de</strong> registro en la Tierra, con tanta multiplicidad como seatécnicamente posible.Esto equivale a captar la onda resultante generada por muchasotras que le prece<strong>de</strong>n y dan origen.Esta “onda” resultante no es una onda propiamente dicha, sinoun efecto <strong>de</strong> distorsión <strong>de</strong>l continuo espacio-tiempo. Sin embargo,<strong>de</strong>bido a la dualidad corpúsculo-onda operante en el Universo esposible tratar matemáticamente dichas distorsiones dándoles lacalidad <strong>de</strong> onda.Una vez implementadas los estudios propuestos se podrá<strong>de</strong>finir la capacidad teórica <strong>de</strong> aprovechar la energía primigenia<strong>de</strong>l Universo <strong>de</strong>nominada Balsfier, cuyas característicasprincipales son la continuidad y permanencia.30

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