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  • 1
    Publication Date: 2017-04-04
    Description: The horizontal pendulums of the Grotta Gigante (Giant Cave) in the Trieste Karst, are long-base tiltmeters with Z¨ollner type suspension. The instruments have been continuously recording tilt and shear in the Grotta Gigante since the date of their installation by Prof. Antonio Marussi in 1966. Their setup has been completely overhauled several times since installation, restricting the interruptions of the measurements though to a minimum. The continuous recordings, apart from some interruptions, cover thus almost 40 years of measurements, producing a very noticeable long-term tiltmeter record of crustal deformation. The original recording system, still in function, was photographic with a mechanical timing and paper-advancing system, which has never given any problems at all, as it is very stable and not vulnerable by external factors as high humidity, problems in power supply, lightning or similar. In December 2003 a new recording system was installed, based on a solid-state acquisition system intercepting a laser light reflected from a mirror mounted on the horizontal pendulum beam. The sampling rate is 30 Hz, which turns the longbase instrument to a very-broad-band tiltmeter, apt to record the tilt signal on a broad-band of frequencies, ranging from secular deformation rate through the earth tides to seismic waves. Here we describe the acquisition system and present two endline members of the instrumental observation, the up to date long-term recording, and the observation of the great Sumatra-Andaman Islands earthquake of December 26, 2004, seismic moment magnitude Mw = 9.1–9.3 [Lay, T., Kanamori, H., Ammon, C.J., Nettles, M., Ward, S.N., Aster, R.C., Beck, S.L., Bilek, S.L., Brudzinski, M.L., Butler, R., DeShon, H.R., Ekstr¨om, G., Satake, K., Sipkin, S., 2005. The Great Sumatra-Andaman Earthquake of 26 December 2004. Science. 308, 1127–1133.]. The secular-term observations indicate an average tilting over the last four decades towards NW of 23.4 nrad/year. We find evidences that this tilting is regional and has been going on since at least 125 ka. The recent earthquake of December 26, 2004 was well recorded by the pendulums.We show that the free oscillation modes were activated, including the lowest modes as e.g. 0T2, 0T3, 0T4, 0T5 and 2S1, 0S3, 0S4, 1S2.
    Description: Published
    Description: 164-174
    Description: JCR Journal
    Description: reserved
    Keywords: Geodetic underground measurements; ; Secular crustal deformation; ; Free oscillations; ; Ultra-broad-band tiltmeter; ; Sumatra-Andaman 2004 earthquake ; 04. Solid Earth::04.03. Geodesy::04.03.06. Measurements and monitoring
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2017-04-04
    Description: L’ Osservatorio Geomagnetico di Duronia (DUR) nasce nell’ ambito di un Progetto Europeo di monitoraggio elettromagnetico ambientale che coinvolge alcuni enti italiani e stranieri: il Progetto MEM (Magnetic and Electric fields Monitoring). Situato in Molise, nella provincia di Campobasso (lat. 41°39’N, Long. 14°28’E, 918m s.l.m.), l’ osservatorio di Duronia costituisce la seconda stazione di misure magnetiche dell’ Italia Centrale realizzata nell’ ambito del Progetto MEM. La prima stazione della rete è l’Osservatorio di L’ Aquila (AQU) (lat. 42°23’N, Long. 13°19’E, 682m s.l.m.) operativo dalla metà del 2005; le due stazioni di misura distano circa 130 km in linea d’ aria. La caratteristica principale del sito di Duronia è il basso rumore elettromagnetico di origine artificiale che garantisce una buona qualità del segnale misurato. Volendo studiare i segnali elettromagnetici di origine naturale è di fondamentale importanza che i segnali prodotti dall’ attività umana siano ridotti al minimo così da non ‘inquinare’ quelli provenienti dalle sorgenti naturali. I primi dati magnetici acquisiti nel sito di Duronia risalgono alla fine del 2007. Diversi tipi di magnetometri permettono una misura continua delle componenti ortogonali H, D e Z e della componente totale F del campo magnetico. La banda di frequenze esplorata copre il range che va dai mHz alle centinaia di kHz.
    Description: Unpublished
    Description: Campobasso, Italy
    Description: 1.6. Osservazioni di geomagnetismo
    Description: restricted
    Keywords: Observatories ; 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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  • 3
    Publication Date: 2017-04-04
    Description: Tra gli obiettivi del Progetto MEM vi è lo studio dei fenomeni elettromagnetici che avvengono nella cavità Terra-ionosfera. Questa regione di spazio è sede di scariche elettriche atmosferiche (fulmini) che irradiano energia sotto forma di onde elettromagnetiche. La risonanza Schumann è un fenomeno che riguarda la propagazione longitudinale di queste onde all’ interno della cavità.
    Description: Unpublished
    Description: Campobasso, Italy
    Description: 1.6. Osservazioni di geomagnetismo
    Description: restricted
    Keywords: Observatories ; Schumann resonance ; 01. Atmosphere::01.02. Ionosphere::01.02.05. Wave propagation ; 04. Solid Earth::04.05. Geomagnetism::04.05.08. Instruments and techniques
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Poster session
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