During RP1 (year 1), the activity concerned (a) the definition of the requirements for the new gravimeters (D4.1); (b) the definition of the design strategies aimed at fulfilling those requirements (D2.1); (c) the development of a numerical algorithm aimed at optimizing the configuration of the gravity imager; (d) the definition of the strategy for archiving and distributing the project’s data (D3.1).
The general rules for accessing NEWTON-g’s data and issues concerning the availability, exchange, use and maintenance of the data were discussed in D1.1 while implementation of the principles set out in D1.1 was addressed in D1.2.
During RP1 the project logo and website were published (D5.1) the kick-off workshop was organized (D5.2) the dissemination and exploitation plan was released (D5.3) and the project video was produced (D5.4).
During RP2 (month 13 to 30), the activity concerned (a) the validation of the design of MEMS (D2.2) and quantum (D2.3) gravimeters; (b) the preparation of the plan for the deployment of the gravity imager (D3.2); (c) the production of the first prototypes of MEMS and quantum devices and the validation of their performances (D2.4 and D2.5); the design and development of the field infrastructures (D3.3); the development of software tools to handle and interpret the data produced by the gravity imager (D4.2 and D4.3); the deployment of the new measurement system at Mt. Etna (D3.4).
The breakout of the COVID-19 pandemic severely affected the project implementation as of March 2020 (month 22).
During RP2, a paper focused on the rationale and objectives of NEWTON-g was published (Carbone et al., 2020).
During RP3 (month 31 to 54), activities carried out under NEWTON-g included (a) completion of the field deployments with the installation of 4 MEMS gravimeters at Mt. Etna (D4.4); (b) evaluation of the performance of the AQG-B installed at Mt. Etna in 2020 (D4.4 and Antoni-Micollier et al., 2022); (c) development of new analytical solutions to calculate the deformation-induced gravity changes caused by triaxial sources (D4.5; Nikkhoo and Rivalta, 2022; 2023); (d) study of gravity anomalies recorded at Mt. Etna, with a view to exploring the potential of gravity data for volcano hazard analysis (D4.5).
We fully demonstrated that the AQG-B provides continuous gravity data suitable for volcano monitoring purposes. Building on the successful application at Mt. Etna, other agencies and research institutions have either acquired an AQG-B, or demonstrated interest to acquire one of this devices in the future. This represents the achievement of one of the objectives of NEWTON-g, i.e. shifting the production of gravimeters for geophysical applications from North America to Europe.
Even though, mostly because of COVID-19-related delays, it was not possible to make the original idea of “gravity imager” came completely true, we performed field tests with the MEMS gravimeters that have provided crucial information for further upgrades.
The new analytical solutions, developed in the framework of WP4, fill a recognized gap in volcano geodesy and will make the joint analysis and inversion of ground deformation and gravity data easier and more accurate.
The data produced under NEWTON-g have been integrated within the EIDA archive, an infrastructure compliant with the FAIR principles.
Finally, several papers were published in peer-reviewed journals during RP3, where results from different project activities are presented.