|
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 gravitational field. The main advantage over using active stabilization with propellants, gyroscopes or reaction wheels is the low use of power and resources. The idea 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 to 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 maximum moment of inertia vertically. The first experimental attempt to use the technique on a human spaceflight was performed on September 13, 1966, on the US Gemini 11 mission, by attaching the Gemini spacecraft to its Agena target vehicle by a tether. The attempt was a failure, as insufficient gradient was produced to keep the tether taut.〔 〕 The technique was first successfully used in a near-geosynchronous orbit on the Department of Defense Gravity Experiment (DODGE) satellite in July 1967.〔(Gunter's Space Page: DODGE )〕 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. An example of gravity-gradient stabilization was demonstrated during NASA's TSS-1R mission. Just prior to tether separation, the tension on the tether was about 65 N (14.6 lbs).〔NASA, (TSS-1R Mission Failure Investigation Board ), Final Report, May 31, 1996 (accessed 7 April 2011)〕 ==See also== *Gravity gradiometry *Space tether *Tidal locking 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Gravity-gradient stabilization」の詳細全文を読む スポンサード リンク
|