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Schuler tuning
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==Application== A pendulum the length of the Earth's radius is impractical, so Schuler tuning doesn't use physical pendulums. Instead, the electronic control system of the [[inertial navigation system]] is modified to make the platform behave as if it were attached to a pendulum. The inertial platform is mounted on [[gimbal]]s, and an [[Electronics|electronic]] [[control system]] keeps it pointed in a constant direction with respect to the three axes. As the vehicle moves, the gyroscopes detect changes in orientation, and a [[feedback loop]] applies signals to torquers to rotate the platform on its gimbals to keep it pointed along the axes. To implement Schuler tuning, the feedback loop is modified to tilt the platform as the vehicle moves in the north–south and east–west directions, to keep the platform facing "down".<ref>{{cite journal | last = King | first = A.D. | authorlink = | title = Inertial Navigation - Forty Years of Evolution | journal = GEC Review | volume = 13 | issue = 3 |page=141 | year = 1998 | url = http://www.imar-navigation.de/downloads/papers/inertial_navigation_introduction.pdf | doi = | id = | accessdate = 2010-09-27}}</ref> To do this, the torquers that rotate the platform are fed a signal proportional to the vehicle's north–south and east–west [[velocity]]. The turning rate of the torquers is equal to the velocity divided by the radius of Earth ''R'': :<math>\dot{\theta} = v/R</math> So: :<math>\ddot{\theta} = a/R</math> The acceleration {{math|'''''a'''''}} is a combination of the actual vehicle acceleration and the acceleration due to gravity acting on the tilting inertial platform. It can be measured by an accelerometer mounted fixed on the platform, in either the north–south or east west direction, horizontally. So this equation can be seen as a version of the equation for a simple gravity [[pendulum]] with a length equal to the radius of Earth. The inertial platform acts as if it were attached to such a pendulum. An inertial navigation system is tuned by letting it sit motionless for one Schuler period. If its coordinates deviate too much during the period or it does not return to its original coordinates at its end it must be tuned to the correct coordinates. Schuler's time constant appears in other contexts. Suppose a tunnel is dug from one end of the Earth to the other end straight through its center. A stone dropped in such a tunnel oscillates harmonically with Schuler's time constant. It can also be proved that the time is the same constant for a tunnel that is not through the center of Earth. Such a tunnel has to be an Earth-centered ellipse, the same shape as the path of the stone. These thought experiments (or rather the results of the corresponding calculations) rely on an assumption of uniform density throughout the Earth. Since the density is not actually uniform, the "true" periods would deviate from Schuler's time constant.
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