Magnetometer measures the strength and sometimes the direction of a magnetic field. An important use is the magnetometer for measuring the earth's magnetic field. By detecting irregularities in the Earth's magnetic field, a magnetometer may indicate the location of magnetic ore deposits such as iron ore, or geological formations associated with oil.
Magnetometers have been based on a number of different principles. Most magnetometers containing a magnetic device sensitive to a magnetic field. Some magnetometers use permanent magnet, an electromagnet others, and still others make use of the magnetic properties of atomic nuclei.
The magnetometer range is ± 1.000 nanoteslas (nT), and is measured by a 16 bit analog-to-digital converter, providing 0.03 nT sensitivity. With temperature compensation of the sensors and electronics, the accuracy of the instrument is 1 nT. The instruments are monitored for correct operation by adding a series of small chains attached to a set of auxiliary windings during calibration and verification weekly magnetometer proper gain and transient responses.
Doc. Clezio Marcos De Nardin - Technical-Scientific Coordination
Doc. Nilson Sant'Anna - Technical-Systems Coordination
Doc. Antônio Lopes Padilha - CEA / INPE
Doc. Emilia Correia - INPE e CRAAM / Mackenzie
Doc. José Ricardo Abalde - IP&D / UNIVAP
Doc. Nelson Jorge Schuch - CRS / INPE
Doc. Paulo Fagundes - IP&D / UNIVAP
M.Sc. Juliano Moro - CEA / INPE
M.Sc. Laysa Cristina Araújo Resende - CEA / INPE
Acad. Laís Maria Guizelli Morais - CEA / INPE
Acad. Sony Su Chen - CEA / INPE
Eng. Sinval Domingos - Chefe de Equipe
Tech. Wagner Sarjob Coura Borges - Técnico de Calibração
Tech. Francisco de Paula Vitor Mesquita
Tech. Avicena Filho
Tech. Acacio Cunha Neto
Tech. Cristiano de Castilho
Doc. Nilson Sant'Anna - Coordination
Doc. Adriano Petry - CRS / INPE
Eng. Rubens Cruz Gatto - Coordination
Information for monitoring the Earth magnetic field (graphic of variation of H, geomagnetic components and Kindex by station).
Summary of indices based on data of all South American stations. Graphs of variation of H, geomagnetic components, dH/dT and Kindex per station take into regard the calculation of QDC.