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  2. Vibrating-sample magnetometer - Wikipedia

    en.wikipedia.org/wiki/Vibrating-sample_magnetometer

    A vibrating-sample magnetometer (VSM) (also referred to as a Foner magnetometer) is a scientific instrument that measures magnetic properties based on Faraday’s Law of Induction. Simon Foner at MIT Lincoln Laboratory invented VSM in 1955 and reported it in 1959. [ 1 ]

  3. Magnetometer - Wikipedia

    en.wikipedia.org/wiki/Magnetometer

    Sample rate is the number of readings given per second. The inverse is the cycle time in seconds per reading. Sample rate is important in mobile magnetometers; the sample rate and the vehicle speed determine the distance between measurements. Bandwidth or bandpass characterizes how well a magnetometer tracks rapid changes in magnetic field.

  4. Category:Magnetometers - Wikipedia

    en.wikipedia.org/wiki/Category:Magnetometers

    Category: Magnetometers. 2 languages. ... Vibrating-sample magnetometer This page was last edited on 20 October 2018, at 11:06 (UTC). Text is available under the ...

  5. Rock magnetism - Wikipedia

    en.wikipedia.org/wiki/Rock_magnetism

    A vibrating sample magnetometer, a widely used tool for measuring magnetic hysteresis. Rock magnetism is the study of the magnetic properties of rocks, sediments and soils. The field arose out of the need in paleomagnetism to understand how rocks record the Earth's magnetic field.

  6. Lunar Traverse Gravimeter - Wikipedia

    en.wikipedia.org/wiki/Lunar_Traverse_Gravimeter

    The Lunar Traverse Gravimeter was a lunar science experiment, deployed by astronauts on the lunar surface in 1972 as part of Apollo 17.The goal of the experiment was to use relative gravity measurements to infer potential attributes about the geological substrata near the Apollo 17 landing site.

  7. Scanning SQUID microscopy - Wikipedia

    en.wikipedia.org/wiki/Scanning_SQUID_microscopy

    Operation of a scanning SQUID microscope consists of simply cooling down the probe and sample, and rastering the tip across the area where measurements are desired. As the change in voltage corresponding to the measured magnetic field is quite rapid, the strength of the bias magnetic field is typically controlled by feedback electronics.