AN EARTH'S FIELD MAGNETOMETER THAT UTILIZES THE FREE PRECESSION OF PROTONS

Abstract

This paper describes the instrumentation of a new type magnetometer that measures the earth's field by measuring the free precession frequency of the protons in water. Results obtained indicate that with the present equipment configuration the earth's magnetic field can be measured to within 0.00002 gauss (out of 5000 times 10 to the -5th power gauss) on an absolute basis and that changes of 1/4 times 10 to the -5th power gauss can be detected. This technique probably represents the most accurate method presently available for measuring the absolute value of the earth's magnetic field. Further, changes of much less than 1/4 times 10 to the -5th power gauss could be detected by this method if it were necessary or desirable simply by increasing the frequency of the crystal controlled source in the counting system. Possible applications include: use as a station magnetometer for a magnetic observatory, use for magnetic surveying or prospecting, and use in harbor defense and air anti-submarine work.

Open PDF

Document Details

Document Type
Technical Report
Publication Date
Jan 01, 1954
Accession Number
AD0485101

Entities

People

  • Charles H. Bowen Jr.

Organizations

  • Naval Postgraduate School

Tags

Communities of Interest

  • Air Platforms
  • Energy and Power Technologies

DTIC Thesaurus Topics

  • Amplifiers
  • Angular Momentum
  • Bandwidth
  • Circuits
  • Detectors
  • Frequency
  • Magnetic Fields
  • Magnetic Moments
  • Magnetometers
  • Materials
  • Measurement
  • Momentum
  • Nuclear Magnetic Moments
  • Optical Equipment
  • Resonant Circuits
  • Sine Waves
  • Tuned Circuits

Fields of Study

  • Physics

Readers

  • Geodesy
  • Plasma Physics / Magnetohydrodynamics