Javascript must be enabled to continue!
The Absolute Gravity Reference Network of Italy
View through CrossRef
The project for realizing the reference network for absolute gravity in the Italian area is presented. This fundamental infrastructure is the general frame for all the scientific and technological activities related to the gravity field in Italy. The project is in line with the actions promoted by the International Association of Geodesy that during its 2015 General Assembly approved a resolution on the establishment of the new global gravity network the so-called International Terrestrial Gravity Reference System/Frame that will replace IGSN71.The selection of the absolute gravity station sites in Italy has been performed either taking into account the existing absolute gravity stations and to have a homogeneous distribution of points. An initial set of 30 stations has been defined over the peninsular part of Italy and the two islands of Sicily and Sardinia. Particularly, the GGOS core station of Matera (the Agenzia Spaziale Italiana Center for Space Geodesy “Bepi” Colombo) is one of the network points as required in the documents of the GGOS-Bureau of Networks and Observations. Thus, this station will provide one link between the Italian national absolute gravity network and the GGOS observation system of IAG.The project is now ongoing and will close at the beginning of 2025.As required by the international standards on gravity measurements (https://www.bipm.org/documents/20126/41442296/CCM++IAG+Strategy+for+Metrology+in+Absolute+Gravimetry/7f9bc651-a2b6-08cc-7bba-f63b0a7e9765), the absolute gravimeters used in the measurements have been compared with absolute gravimeters that participated into international comparison campaigns in order to ensure the measurements traceability.Furthermore, absolute gravity measurements have been supplemented with direct measurements of the local value of the vertical gravity gradient, in order to reduce to the ground reference level the absolute values measured by different instruments at different heights. The gravity field campaigns will be assisted by topographic survey campaigns. This will allow a precise georeferencing (of the order of 12 cm) of the gravity stations that will be so framed to the current ITRF.The collected data will be then validated and reduced following the internationally accepted standards and finally published through a dedicate web page of the project. These data will also be sent for storage to the absolute gravity database maintained by the Bureau Gravimétrique International/Bundesamt fuer Kartographie und Geodaesie where the absolute gravity data that will contribute to the new global absolute gravity reference system are collected.
Title: The Absolute Gravity Reference Network of Italy
Description:
The project for realizing the reference network for absolute gravity in the Italian area is presented.
This fundamental infrastructure is the general frame for all the scientific and technological activities related to the gravity field in Italy.
The project is in line with the actions promoted by the International Association of Geodesy that during its 2015 General Assembly approved a resolution on the establishment of the new global gravity network the so-called International Terrestrial Gravity Reference System/Frame that will replace IGSN71.
The selection of the absolute gravity station sites in Italy has been performed either taking into account the existing absolute gravity stations and to have a homogeneous distribution of points.
An initial set of 30 stations has been defined over the peninsular part of Italy and the two islands of Sicily and Sardinia.
Particularly, the GGOS core station of Matera (the Agenzia Spaziale Italiana Center for Space Geodesy “Bepi” Colombo) is one of the network points as required in the documents of the GGOS-Bureau of Networks and Observations.
Thus, this station will provide one link between the Italian national absolute gravity network and the GGOS observation system of IAG.
The project is now ongoing and will close at the beginning of 2025.
As required by the international standards on gravity measurements (https://www.
bipm.
org/documents/20126/41442296/CCM++IAG+Strategy+for+Metrology+in+Absolute+Gravimetry/7f9bc651-a2b6-08cc-7bba-f63b0a7e9765), the absolute gravimeters used in the measurements have been compared with absolute gravimeters that participated into international comparison campaigns in order to ensure the measurements traceability.
Furthermore, absolute gravity measurements have been supplemented with direct measurements of the local value of the vertical gravity gradient, in order to reduce to the ground reference level the absolute values measured by different instruments at different heights.
The gravity field campaigns will be assisted by topographic survey campaigns.
This will allow a precise georeferencing (of the order of 12 cm) of the gravity stations that will be so framed to the current ITRF.
The collected data will be then validated and reduced following the internationally accepted standards and finally published through a dedicate web page of the project.
These data will also be sent for storage to the absolute gravity database maintained by the Bureau Gravimétrique International/Bundesamt fuer Kartographie und Geodaesie where the absolute gravity data that will contribute to the new global absolute gravity reference system are collected.
Related Results
Gravity data reduction, Bouguer anomaly, and gravity disturbance
Gravity data reduction, Bouguer anomaly, and gravity disturbance
Each point on the earth has a gravity and gravity potential value. Surfaces formed by connecting points with equal gravity potential values are called equipotential surfaces or lev...
Using spherical scaling functions in scalar and vector airborne gravimetry
Using spherical scaling functions in scalar and vector airborne gravimetry
<p>Airborne gravimetry is capable to provide Earth&#8217;s gravity data of high accuracy and spatial resolution for any area of interest, in particular for ha...
Combined discrete and continuous gravity measurements at Vulcano Island (Aeolian Archipelago, Italy)
Combined discrete and continuous gravity measurements at Vulcano Island (Aeolian Archipelago, Italy)
<p>We present the preliminary results of combined discrete and continuous gravity measurements, carried out at Vulcano Island (Aeolian Archipelago, Sicily, southern I...
Research on Model, Experiment and Application of Gravity Valve
Research on Model, Experiment and Application of Gravity Valve
Abstract
In this paper, two kinds of gravity valves are designed: copper bead gravity valve and hose gravity valve. Firstly, the stress distribution on the substrate of the...
Sinking or bouncing in low gravity environments?
Sinking or bouncing in low gravity environments?
Understanding the physics of granular materials in a low gravity and vacuum environment is essential to predict the regolith behavior on the Moon and asteroids. Cohesive forces - i...
Control of the accuracy of the Molodensky's integral equation for the gravity anomalies and disturbances on the Earth's models
Control of the accuracy of the Molodensky's integral equation for the gravity anomalies and disturbances on the Earth's models
The problem of determining the anomalous potential T on the earth's surface can be solved on the basis of various initial available data: gravity anomalies Δg and gravity ...
Estimating the Parameters of Extended Gravity Theories with the Schwarzschild Precession of S2 Star
Estimating the Parameters of Extended Gravity Theories with the Schwarzschild Precession of S2 Star
After giving a short overview of previous results on constraining of Extended Gravity by stellar orbits, we discuss the Schwarzschild orbital precession of S2 star assuming the con...
Constraints on Yukawa gravity parameters from observations of bright stars
Constraints on Yukawa gravity parameters from observations of bright stars
Abstract
In this paper we investigate a Yukawa gravity modification of the Newtonian gravitational
potential in a weak field approximation. For that purpose we der...


