Gravity-gradient stabilization
Gravity-gradient stabilization (a.k.a. "tidal stabilization") is a method of stabilizing artificial satellites or space tethers in a fixed orientation using only the orbited body's mass distribution and the Earth's gravitational field. The main advantage over using active stabilization with propellants, gyroscopes or reaction wheels is the low use of power and resources.
The technique was first successfully used in a near-geosynchronous orbit on the Department of Defense Gravity Experiment (DODGE) satellite in July of 1967.[1]
It was first used for low Earth orbit and tested unsuccessfully for geosynchronous orbit in the Applications Technology Satellites ATS-2, ATS-4 and ATS-5 from 1966 until 1969.[citation needed]
The principle is to use the Earth's gravitational field and tidal forces to keep the spacecraft aligned in the desired orientation. The gravity of the Earth decreases according the inverse-square law, and by extending the long axis perpendicular to the orbit, the "lower" part of the orbiting structure will be more attracted to the Earth. The effect is that the satellite will tend to align its axis of minimum moment of inertia vertically.
An example of gravity-gradient stabilization was demonstrated during NASA's TSS-1R mission.[failed verification] Just prior to tether separation, the tension on the tether was about 65 N (14.6 lbs).[2]
See also
External links
- NASA on ATS-2
- Gunter's Space Page on ATS 2, 4 and 5
- A new kind of Earth Sensor using a proof mass on a MEMS created by EPFL students
References
- ^ Gunter's Space Page: DODGE
- ^ NASA, TSS-1R Mission Failure Investigation Board, Final Report, May 31, 1996 (accessed 7 April 2011)
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