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Regional comparison of absolute gravimeters, EURAMET.M.G-K2 key comparison

2017-01, Palinkas, V., Francis, O., Val'ko, M., Kostelecky, J., Van Camp, Michel, Castelein, S., Bilker-Koivula, M., Näränen, J., Lothhammer, A., Falk, R., Schilling, M., Timmen, L., Iacovone, D., Baccaro, F., Germak, Alessandro, Biolcati, E., Origlia, Claudio, Greco, Filippo, Pistorio, Antonio, De Plaen, R., Klein, G., Seil, M., Radinovic, R., Reudink, R., Dykowski, P., Sekowski, M., Próchniewicz, D., Szpunar, R., Mojzeš, M., Janák, J., Papčo, J., Engfeldt, A., Olsson, P. A., Smith, V., van Ditmarsch, Dave, Ellis, B., Lucero, B., #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#, #PLACEHOLDER_PARENT_METADATA_VALUE#

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Absolute gravity measurements at three sites characterized by different environmental conditions using two portable ballistic gravimeters

2015, Greco, F., Biolcati, E., Pistorio, A., D'Agostino, G., Germak, A., Origlia, C., Del Negro, C., Greco, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia, Biolcati, E.; Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Pistorio, A.; Dipartimento di Ingegneria Elettrica, Elettronica e Informatica, Università di Catania, Italy, D'Agostino, G.; Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Germak, A.; Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Origlia, C.; Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Del Negro, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Catania, Catania, Italia, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia, Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Dipartimento di Ingegneria Elettrica, Elettronica e Informatica, Università di Catania, Italy, Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Istituto Nazionale di Ricerca Metrologica, Torino, Italy, Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OE, Catania, Italia

The performances of two absolute gravimeters at three different sites in Italy between 2009 and 2011 is presented. The measurements of the gravity acceleration g were performed using the absolute gravimeters Micro-g LaCoste FG5#238 and the INRiM prototype IMGC-02, which represent the state of the art in ballistic gravimeter technology (relative uncertainty of a few parts in 10 9 ). For the comparison, the measured g values were reported at the same height by means of the vertical gravity gradient estimated at each site with relative gravimeters. The consistency and reliability of the gravity observations, as well as the performance and efficiency of the instruments, were assessed by measurements made in sites charac- terized by different logistics and environmental conditions. Furthermore, the various factors affecting the measurements and their uncertainty were thoroughly investigated. The measurements showed good agree- ment, with the minimum and maximum differences being 4.0 and 8.3 µGal. The normalized errors are very much lower than 1, ranging between 0.06 and 0.45, confirming the compatibility between the results. This excellent agreement can be attributed to several factors, including the good working order of gravimeters and the correct setup and use of the instruments in different conditions. These results can contribute to the standardization of absolute gravity surveys largely for applications in geophysics, volcanology and other branches of geosciences, allowing achieving a good trade-off between uncertainty and efficiency of gravity measurements.

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The new IMGC-02 transportable absolute gravimeter: measurement apparatus and applications in geophysics and volcanology

2008-02, D’Agostino, G., Desogus, S., Germak, A., Origlia, C., Quagliotti, D., Berrino, G., Corrado, G., D’errico, V., Ricciardi, G., D’Agostino, G.; Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Desogus, S.; Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Germak, A.; Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Origlia, C.; Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Quagliotti, D.; Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Berrino, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia, Corrado, G.; Dipartimento di Scienze della Terra, Università degli Studi di Napoli «Federico II», Napoli, Italy, D’errico, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia, Ricciardi, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia, Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Istituto Nazionale di Ricerca Metrologica (INRIM), Torino, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia, Dipartimento di Scienze della Terra, Università degli Studi di Napoli «Federico II», Napoli, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia, Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia

The research carried out at the Istituto Nazionale di Ricerca Metrologica (formerly Istituto di Metrologia «G. Colonnetti») aiming to develop a transportable ballistic absolute gravimeter ended with a new version of the instrument, called the IMGC-02. It uses laser interferometry to measure the symmetrical free rising and falling motion of a test mass in the gravity field. Providing the same accuracy achieved with previous versions, the instrumental improvements mainly concern size, weight, data processing algorithms and operational simplicity. An uncertainty of 9 μGal (1 μGal=1×10–8 m·s−2) can be achieved within a single observation session, lasting about 12 h, while the time series of several observation sessions show a reproducibility of 4 μGal. At this level, gravity measurements provide useful information in Geophysics and Volcanology. A wide set of dynamic phenomena, i.e. seismicity and volcanic activity, can produce temporal gravity changes, often quite small, with an amplitude ranging from a few to hundreds of microgals. Therefore the IMGC absolute gravimeter has been employed since 1986 in surveying the Italian active volcanoes. A brief history of the gravimeter and the description of the new apparatus, together with the main results of ongoing applications in Geophysics and Volcanology are presented.