Terrestrial and Airborne Gravimetry

Head: Dr. Christoph Förste

Terrestrial gravimetry has a long tradition on the Telegraphenberg hill in Potsdam, where the former Geodetic Institute started to carry out pendulum and gravimeter measurements more than 100 years ago. Today in our Section 1.2 at GFZ we apply two modern gravimetric techniques: Superconducting and Airborne Gravimetry.

According to Newton’s law the acceleration of free fall of a dropped body is proportional to its mass. That means the acceleration of free fall and the gravitational attractive force are equivalent. Therefore in Geodesy and Geophysics the acceleration of free fall is used as a measure for the gravity field.

Terrestrial gravity observations comprise the measurement of the vertical component of the  acceleration of free fall g (g = Gravity) on the Earth's surface to determine spatial as well as temporal gravity variations. In this context one has to take into account that Gravity on the Earth’s surface is a superposition of the gravitational attraction of masses (Newton’s law) and the significantly smaller but outwards directed centrifugal acceleration due to the rotation of the Earth. Furthermore, mass density inhomogeneities as well as temporal mass displacements cause spatial and temporal variations of the gravitational attraction on the Earth’s surface which can be detected with gravity meters. In this context, spatial gravity observations can be used to derive information about geological structures such as fault zones, salt domes and volcanic structures or to explore ore deposits.

The largest signals of gravity variations are caused by the periodic changes of the relative positions between the Earth, the Moon and the Sun and the thereby induced deformations of the Earth's body (for instance Ocean and Earth tides and Ocean tide induced loading effects).

Examples of gravity variations on the Earth’s surface are (expressed as acceleration of free fall):

  • The gravity difference between pole and equator due to Earth’s oblateness (the poles are closer to the Earth’s centre of mass and the centrifugal acceleration due the Earth’s rotation is zero at the poles and maximum at the equator):
    Δg ~ 5•10-2 m/s²
  • Gravity differences between deep sea and highest mountains: Δg ~ 5•10-2 m/s²
  • Earth tides: up to Δg ~ 3•10-6 m/s²
  • Gravity changes by mass redistribution in the atmosphere: up to Δg ~ 2•10-7 m/s²
  • Gravity changes by long-term terrestrial mass displacements: in the order of Δg ~10-7 m/s2
  • Increase of Gravity due to 1 m groundwater rise:  Δg ~ 4•10-8 m/s2

Superconducting Gravimetry

Temporal gravity variations can be recorded by using absolute and relative gravimeters. The most accurate and stabile relative gravimeters are Superconducting Gravimeters (SG). These instruments belong to the family of relative spring-mass gravimeters. In contrast to classical spring-mass gravimeters the SG has no spring. It’s replaced by a “virtual spring design” where a liquium helium cooled diamagnetic superconducting sphere is levitating in the super-stable magnetic field of a superconducting electromagnet.

As all gravity sensors a Superconducting Gravity meter is an integrating sensor measuring the sum of all gravity variations in its near and far environments. Therefore, the SG recordings include gravity effects of different sources. Due to the equivalence of gravitational and inertial mass (i.e. Einstein’s equivalence principle) the sensor inside a gravimeter (a test mass) is sensitive to temporal variations of Gravitational forces (Newtonian attraction) caused by redistribution and density variations of all surrounding masses as well as Inertial forces caused by accelerations, i.e. the second time derivative of the vertical position of the gravimeter site.

For the separation of the different gravity constituents sophisticated modelling and analysing techniques together with additional data (e.g. meteorological and hydrological data) are necessary. Research topics in this context are among others:

  • Gravity changes induced by mass redistribution in the atmosphere and hydrosphere
  • Comparison and Interpretation of satellite derived gravity variations
  • Evaluation of ocean tide models and Hydrological models
  • Inner core translation (Slichter Triplet)
  • Core resonance in the tidal band (Nearly Diurnal Free Wobble)
  • Polar motion and Free oscillations of the Earth

Presently about 30 superconducting gravimeters are worldwide operated within the IAG service International Geodynamics and Earth Tide Service (IGETS). “GFZ hosts the IGETS data base and contributes with the data of its own two superconducting gravimeters from the geodynamic observatories SAGOS (South African Geodynamic Observatory Sutherland) and ZUGOG (Zugspitze Geodynamic Observatory Germany).

South African Geodynamic Observatory Sutherland (SAGOS)

The South African Geodynamic Observatory Sutherland (SAGOS) of GFZ was established during the years 1998 – 2000 based on an Agreement on Cooperative Activities between the National Research Foundation (NRF) and GFZ, signed in August 1998.  SAGOS is located at the site of the South African Astronomical Observatory (SAAO). The operation and maintenance of the SAGOS instrumentation is jointly done by staff of SAAO and GFZ.

The SAGOS observatory is located about 350 km north-east of Cape Town (longitude: 20.81 E, latitude: 32.38 S, altitude: 1755 m). The shortest distance to the South Atlantic coastline is about 200 kilometres. The area is located in a tectonically quiet zone far away from the African rift. Geologically, the setting is a huge dolerite plateau with a several kilometres thick layer of dolerite. This bedrock allows a good coupling of the Superconducting gravimeter (SG) pillars to the ground. The environment is a remote area with no industry and low seismicity. The climate at this place is determined by the border between summer and winter rainfall zones so that temperature fluctuations are not too rough. The observatory is also built into the ground to protect it against environmental effects like strong winds and temperature changes. All rooms are thermally insulated. An air condition system controls the temperature inside the measurement chamber, which is equipped with three concrete pillars embedded into the dolerite bedrock. Two of the pillars are constructed for Superconducting gravimeters or other geophysical instruments. The third pillar is dedicated for absolute gravimeters for the calibration of the Superconducting gravimeters. In the vicinity of the observatory four further pillars were set up for various other geodetic antennas and instrumentation.

SAGOS is a high precision geodynamic observatory comprising space techniques and ground instruments. Presently the observatory is equipped with

  • One Superconducting Gravimeter (OSG D037), which is integrated in the IAG service International Geodynamics and Earth Tide Service IGETS. A second superconducting gravimeter (OSG 052) has been recording data between 2008 and 2017, before it was deinstalled in September 2017 for the operation at Zugspitze (ZUGOG). The data from these SGs are available for registered users from the IGETS data base hosted by GFZ. When using this dataset please cite it as follows
    Förste, C., Voigt, C., Abe, M., Kroner, C., Neumeyer, J., Pflug, H., Fourie, P. (2016) Superconducting Gravimeter Data from Sutherland – Level 1. GFZ Data Services. http://doi.org/10.5880/igets.su.l1.001

    SGs allow a stationary, continuous high-resolution monitoring of temporal changes of the Earth's gravity field. Main objectives are studying mass transport in the earth's system related to atmosphere, hydrosphere and analysing global geodynamic gravity processes such as polar motion, core modes, Earth & ocean tides and non-tidal loading effects. 
  • A local network of hydrological sensors (soil moisture, groundwater level, meteorology) in cooperation with Section 5.4 which are essentially needed for the interpretation of the SG measurements
  • One permanent GNSS station (station ID: sutm) as a core station of the International GNSS Service (IGS). The data of this station are worldwide used within the geodetic science community for the determination of global and regional reference systems, for the investigation of crustal dynamics, for satellite orbit determination and others.
  • One Triaxial Magnetometer, mainly used for investigations of the magnetic oscillation. Additionally, it is used as ground truth for satellite observations. The magnetometer has been installed in co-operation with the Hermanus Geomagnetic Observatory which permanently uses its data for instance in the international PLASMON project (coordinated by the Eötvös Loránd University, Hungary)

ZUGOG

The Zugspitze Geodynamic Observatory Germany (ZUGOG) is being established at the end of 2017 on top of mountain Zugspitze in the German Alps, with the dual targets of validation and calibration of GRACE-FO and supporting research into alpine mountain building processes and climate-relevant hydrological studies connected to the Environmental Research Station Schneefernerhaus. This second geodynamic observatory of GFZ includes the superconducting gravimeter OSG 052 and starts to measure in spring 2018.

Airborne and Ship Gravimetry

Satellite-based gravity field determination can map the gravity field of the Earth in a very homogeneous way, however, with limited spatial resolution due to the altitude of the orbits. On the other hand, traditional terrestrial gravimetry on ground can measure the gravity with high resolution, but its data are often inhomogeneous and such measurements can be limited by difficult environmental conditions like high mountains, glaciers, mush or jungle. Furthermore, traditional terrestrial gravimeters cannot be used on sea. Air- and shipborne gravimetry measurements can be used to fill data gaps of the traditional gravimetry on ground and the satellite techniques. Thanks to the development of GNSS, air- and shipborne gravimetry nowadays can operate routinely not only for research, but also for resource investigation etc. Regional gravity field models can be developed on the basis of this technique.

Current Gravimeters used for air- and shipborne gravimetry are specifically constructed mobile spring-mass gravimeters which are mounted on gyro stabilized platforms. Furthermore, recordings of GNSS receivers and Inertial Navigation Systems enables for the reduction of the disturbing non-gravitational accelerations of the measurement platform.

GFZ’s instrumentation for air- and shipborne gravimetry are a mobile gravimeter Chekan-AM made by CSRI "Elektropribor" , an Inertial Navigation System (INS) AEROcontrol-II and 4 GPS receiver JAVAD Delta G3T. This equipment has been recently used for airborne gravimetry onboard the German High Altitude and LOng Range Research Aircraft (GEOHALO). Currently, GFZ is running shipborne gravimetry on the Baltic Sea within the FAMOS project.

Literature

Abe, M., Kroner, C., Förste, C., Petrovic, S., Barthelmes, F., Weise, A., Güntner, A., Creutzfeldt, B., Jahr, T., Jentzsch, G., Wilmes, H., Wziontek, H. (2012): A comparison of GRACE-derived temporal gravity variations with observations of six European superconducting gravimeters. Geophysical Journal International, 191, 2, p. 545-556, doi.org/10.1111/j.1365-246X.2012.05641.x

Weise, A., Kroner, C., Abe, M., Creutzfeldt, B., Förste, C., Güntner, A., Ihde, J., Jahr, T., Jentzsch, G., Wilmes, H., Wziontek, H., Petrovic, S. (2012): Tackling mass redistribution phenomena by time-dependent GRACE- and terrestrial gravity observations. Journal of Geodynamics, 59-60, p. 82-91, doi.org/10.1016/j.jog.2011.11.003

Neumeyer, J. (2010): Superconducting Gravimetry. In: G. Xu (eds.), Sciences in Geodesy - I, Springer-Verlag Berlin Heidelberg, doi:10.1007/978-3-642-11741-1_10

Contact

Christoph Förste
Group Leader
Dr. Christoph Förste
Global Geomonitoring and Gravity Field
Telegrafenberg
Building A 17 , Room 00.15
14473 Potsdam
+49 331 288-1737
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