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Instruments

Magnetometer

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A magnetometer is an instrument that measures magnetic field strength or magnetic dipole moment, used across geophysics, space science and materials research to detect and characterize magnetic fields.

Facts
Invented Year
1832 1
Carl Friedrich Gauss's 1832 instrument, a bar magnet suspended horizontally from a gold fibre to measure the strength of Earth's magnetic field, is generally credited as the first magnetometer.
Measures
Magnetic field strength, and in vector instruments, its direction. 1
Operating Principle
Detects the direction, strength or relative change of a magnetic field at a given location, historically via the deflection or oscillation of a suspended magnet and, in modern instruments, via induction, Hall-effect or fluxgate sensors. 1
Resolution
SQUID magnetometers reproducibly achieve femtotesla resolutions in optimized laboratory settings. 1
Operating Range
Earth's magnetic field varies from about 20,000 to 80,000 nanotesla depending on location. 1
Cross-Tradition Connections

Invented By

Used In

Sources
1. Magnetometer (Wikipedia)
WikipediaLead sectionView the Source
1. Magnetometer (Wikipedia)
WikipediaHistory sectionView the Source
1. Magnetometer (Wikipedia)
WikipediaOverview sectionView the Source
1. Magnetometer (Wikipedia)
WikipediaLaboratory section
Quote, Laboratory section
SQUID magnetometry is an extremely sensitive absolute magnetometry technique, reproducibly achieving femtotesla resolutions in optimized laboratory settings.
View the Source
1. Magnetometer (Wikipedia)
WikipediaIntroduction section
Quote, Introduction section
The Earth's magnetic field can vary from 20000 to 80000 nT depending on location
View the Source
1. Magnetometer (Wikipedia)
WikipediaInvented By: Carl Friedrich GaussView the Source
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