97 research outputs found
The ESPERIA satellite project for detecting seismo-associated effects in the topside ionosphere. First instrumental tests in space
In recent times, ionospheric and magnetospheric perturbations constituted by radiation belt particle precipitations, variations of temperature and density of ionic and electronic components of ionospheric plasma as well as electric and magnetic field fluctuations have been detected on board of the LEO satellites and associated with earthquake preparation and occurrence. Several mechanisms have been suggested as justifying the seismoelectromagnetic phenomena observed in the upper lithosphere and in the topside ionosphere before, during and after an earthquake. Their propagation in these media has also been investigated, but physical knowledge of such processes is below standard. Consequently, coordinated space and ground-based observations based on data gathered simultaneously in space and at the Earth's surface are needed to investigate seismo-associated phenomena. To this end, the ESPERIA space mission project has been designed for the Italian Space Agency (ASI). To date, a few instruments of its payload have been built and tested in space. This paper reports on the justification, science background, and characteristics of the ESPERIA mission project as well as the description and testing of ESPERIA Instruments (ARINA and LAZIO-EGLE) in space
Groundwater helium content related to the Spitak (Armenia) and Karymsky (Russia) earthquakes
The Spitak and Karymsky earthquakes occurred with M46.9 in
Armenia and in Kamchatka (Russia), respectively. As regards the Spitak earthquake, we analysed the groundwater helium content data collected by three Georgian and one Armenian measurement sites; as regards the Karymsky earthquake, we analysed the groundwater helium content data collected by two measurement sites in Kamchatka. The first analysis has pointed out that precursory anomalies appeared in the northern area with respect to the Spitak epicentre; on the
contrary, only co-post seismic anomalies were revealed in the southern area. As regards the Karymsky earthquake, no pre-co-post seismic variation in the groundwater helium content was revealed at both the measurement sites. The
analysis of other hydrogeochemical parameters, collected in these sites, revealed that one site does not show any anomaly; on the contrary, at the other measurement site clear preseimic anomalies appeared in some hydrogeochemical parameters. A possible explanation of the quoted results is presented
Phenomenology of rupture process in homogeneous isotropic media
A statistical method is proposed for the description of the fracture pro::ess in homogeneous isotropic media. In particular, the macroscopic defects formation into a medium due to the application of an external load is studied. The instability connected with the structural transition from these multimacroscopic defects to the final rupture of the body is also discussed. To this purpose, the Volterra logistic growth law is used. The statistical interpretation of the rupture catastrophic phenomenon includes the justification of the characteristic "silent time" (which has been observed to occur in some time intervals prior to the fracture), as an indicator of the above-mentioned structural transition
Tellus Experiment. Method for Signal Conditioning and Data Acquisition System, based on Variable Amplification and Feedback Technique
In many space and ground-based applications of interest for the TELLUS Experiment
the amplitude and frequency content of analog signals to be detected is
a priori unknown and can lie in a very large range of values [1-5]. This is a particularly
challenging problem to be managed, especially when the data acquisition
and signal analysis must be carried out in extreme environments where large data
processing resources are requested together with a low power consumption and high
efficiency of the device. The method is specifically useful when power spectrum of
measured signals exhibits a very large variability in the different frequency bands
making particularly difficult the runtime signal analysis of the phenomena under
study. The method proposed within the TELLUS Experiment is of particular interest
in two applications. The first being an analysis of multi-channel analog signals
constituted by several frequency components each one of which exhibits very different
amplitudes that need to be simultaneously registered by the acquisition system.
The second application further enhances the specific characteristics of the method
when, in addition to manage multichannel analysis, we should treat multiparameter
data (i.e. data relating to signals of different nature associated with parameters or
fields different from each other) [6]
TELLUS. A new electromagnetic strainmeter for the monitoring of ground-field deformations
Tellus Experiment.A multi-instrument Payload for the investigation of the Topside Ionosphere
A new space project, which summarizes previous ones reported in several LNGS
Annual Reports, has been proposed by the TELLUS team for the investigation
of ionospheric and magnetospheric phenomena within the Earth-near-Earth space couplings. The project includes the study of natural disasters taking place in the
Earth surface (as earthquakes) and their possible deterministic prediction on the
basis of precursory phenomena to be reconciled with perturbations occurring in
the topside ionosphere. After an introductory section on the subject, technical,
scientific, and methodological details are given on the project
Method for signal conditioning and data acquisition system, based on variable amplification and feedback technique
An original method of signal conditioning and adaptive amplification is proposed for data acquisition systems of analog signals, conceived to obtain a high resolution spectrum of any input signal. The procedure is based on a feedback scheme of the signal amplification with aim at maximizing the dynamic range and resolution of the data acquisition system. The paper describes the signal conditioning, digitization, and data processing procedures applied to an a priori unknown signal in order to enucleate its amplitude and frequency content for applications in different environments: on the ground, in space, or in the laboratory. In the paper are also discussed the main fields of application and advantages of the method with respect to those known toda
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