Print

Iaga Workshop 2016

XVIIth IAGA Workshop on Geomagnetic Observatory Instruments, Data acquisition and Processing 

September 4-10, 2016

Royal Meteorological Institute of Belgium, Dourbes Magnetic Observatory

 

Results of the Instruments Inter-comparison and Checking

Two types of instruments were tested: 

  • Proton precession  magnetometers and 
  • DIflux theodolites.

You can find the pdf file with the results  here :  results

Our apologies for the late publication.

J. Rasson and A. Gonsette

Print

Geomagnetic observations and instruments

 

For pratical use and scientific research, Belgium must know the value of continuous variations and the geomagnetic field.This is one case for magnetic declination: it is used to find the direction of north with the compass. This is done using the Magnetic Observatories of Dourbes and Manhay. A complete measure of geomagnetic vector is recorded every minute.

Print

Environmental Magnetism

 


Recent projects

2019 - 2024: Convention of cooperation with the Wallonia Heritage Agency  "Development of archaeomagnetic research in Wallonia".

2018 - 2022: COST Action CA17131: "The Soil Science & Archaeo-Geophysics Alliance: going beyond prospection."

2017 - 2020: EMPIR joint research project: "MagNaStand" for supporting the  development of new ISO standards for magnetic nanoparticles and products containing magnetic nanoparticles.

2014 - 2018: COST Action TD1402  "Multifunctional Nanoparticles for Magnetic Hyperthermia and Indirect Radiation Therapy (RADIOMAG)." Project website: www.cost-radiomag.eu

2014 - 2018: "Archaeomagnetic Network for the Rescue of Cultural Heritage in Northern Africa (RAPSCA)." supported by BELSPO


 

Palaeo- and Archaeomagnetism is the study of geomagnetic field variations during geological and archaeological periods, respectively. Rocks, sediments and baked material acquire a magnetisation during their formation or during cooling from high temperatures. This magnetisation lasts over millions of years (remanent magnetisation) and is aligned parallel to the ambient magnetic field at the time of acquisition.