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Large pendulum that is free to swing in any direction. As it swings back and forth, the earth rotates beneath it, so its perpendicular plane of swing rotates in relation to the earth's surface. Devised by J.-B.-L. Foucault in 1851, it provided the first laboratory demonstration that the earth spins on its axis. A Foucault pendulum always rotates clockwise in the Northern Hemisphere and counterclockwise in the Southern Hemisphere (a consequence of the Coriolis force). The rate of rotation depends on the latitude, becoming slower as the pendulum is placed closer to the equator; at the equator, a Foucault pendulum does not rotate.

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Encyclopedia Britannica, 2008. Encyclopedia Britannica Online.

The Foucault pendulum ("foo-KOH"), or Foucault's pendulum, named after the French physicist Léon Foucault, was conceived as an experiment to demonstrate the rotation of the Earth.

In 1851 it was well known that Earth rotated: observational evidence included Earth's measured polar flattening and equatorial bulge. However, Foucault's pendulum was the first dynamic proof of the rotation in an easy-to-see experiment, and it created a sensation in both the learned and everyday worlds.

At either the North Pole or South Pole, the plane of oscillation of a pendulum remains fixed with respect to the fixed stars while Earth rotates underneath it, taking one sidereal day to complete a rotation. So relative to Earth, the plane of oscillation of a pendulum at the North or South Pole undergoes a full clockwise or counterclockwise rotation during one day, respectively. When a Foucault pendulum is suspended on the equator, the plane of oscillation remains fixed relative to Earth. At other latitudes, the plane of oscillation precesses relative to Earth, but slower than at the pole; the angular speed, $alpha$ (measured in clockwise degrees per sidereal day), is proportional to the sine of the latitude, $phi$:

- $alpha=360,sin(phi).$

Here, latitudes north and south of the equator are defined as positive and negative, respectively. For example, a Foucault pendulum at 30° south latitude, viewed from above by an earthbound observer, rotates counterclockwise 180° in one day.

In order to demonstrate the rotation of the Earth without the philosophical complication of the latitudinal dependence, Foucault named the gyroscope in 1852. The gyroscope's spinning rotor tracks the stars directly. Its axis of rotation is observed to return to its original orientation with respect to the earth after one day whatever the latitude, unaffected by the sine factor.

A Foucault pendulum requires care to set up because imprecise construction can cause additional veering which masks the terrestrial effect. The initial launch of the pendulum is critical; the traditional way to do this is to use a flame to burn through a thread which temporarily holds the bob in its starting position, thus avoiding unwanted sideways motion. Air resistance damps the oscillation, so Foucault pendulums in museums often incorporate an electromagnetic or other drive to keep the bob swinging; others are restarted regularly. In the latter case, a launching ceremony may be performed as an added show.

From the perspective of an inertial frame outside of Earth, the suspension point of the pendulum traces out a circular path during one sidereal day. No forces act to make the plane of oscillation of the pendulum rotate - the plane contains the plumb line, so the force acting on the pendulum is parallel to the plane of oscillation at all times. But the plane satisfies the constraint that it contains the plumb line. Thus the plane of oscillation undergoes parallel transport. The difference between initial and final orientations is $alpha=-2pi,sin(phi)$ as given by the Gauss-Bonnet theorem. $alpha$ is also called the holonomy or geometric phase of the pendulum. Thus, when analyzing earthbound motions, the Earth frame is not an inertial frame, but rather rotates about the local vertical at an effective rate of $2pi,sin(phi)$ radians per day, which is the magnitude of the projection of the angular velocity of Earth onto the normal direction to Earth.

From the perspective of an Earth-bound coordinate system with its $x$-axis pointing east and its $y$-axis pointing north, the precession of the pendulum is explained by the Coriolis force. Consider a planar pendulum with natural frequency $omega$ in the small angle approximation. There are two forces acting on the pendulum bob: the restoring force provided by gravity and the wire, and the Coriolis force. The Coriolis force at latitude $phi$ is horizontal in the small angle approximation and is given by

- $$

The restoring force, in the small angle approximation, is given by

- $$

Using Newton's laws of motion this leads to the system of equations

- $$

Switching to complex coordinates $z=x+iy$ the equations read

- $$

To first order in $Omega/omega$ this equation has the solution

- $$

If we measure time in days, then $Omega=2pi$ and we see that the pendulum rotates by an angle of $-2pi,sin(phi)$ during one day.

There are many physical systems that precess in a similar manner to a Foucault pendulum. In 1851, Charles Wheatstone described an apparatus that consists of a vibrating spring that is mounted on top of a disk so that it makes a fixed angle $phi$ with the disk. The spring is struck so that it oscillates in a plane. When the disk is turned, the plane of oscillation changes just like the one of a Foucault pendulum at latitude $phi$.

Similarly, consider a non-spinning perfectly balanced bicycle wheel mounted on a disk so that its axis of rotation makes an angle $phi$ with the disk. When the disk undergoes a full clockwise revolution, the bicycle wheel will not return to its original position, but will have undergone a net rotation of $2pi,\; sin(phi)$.

Another system behaving like a Foucault pendulum is a South Pointing Chariot that is run along a circle of fixed latitude on a globe. If the globe is not rotating in an inertial frame, the pointer on top of the chariot will indicate the direction of swing of a Foucault Pendulum that is traversing this latitude.

In physics, these systems are referred to as geometric phases. Mathematically they are understood through parallel transport.

There are numerous Foucault pendula around the world, mainly at universities, science museums and planetariums. The experiment has even been carried out at the South Pole.

- Persson, A. The Coriolis Effect: Four centuries of conflict between common sense and mathematics, Part I: A history to 1885 History of Meteorology 2 (2005)
- Phillips, N. A., What Makes the Foucault Pendulum Move among the Stars? Science and Education, Volume 13, Number 7, November 2004, pp. 653-661(9)
- Classical dynamics of particles and systems, 4ed, Marion Thornton (ISBN 0-03-097302-3 ), P.398-401.
- John B. Hart, Raymond E. Miller and Robert L. Mills A simple geometric model for visualizing the motion of a Foucault pendulum, American Journal of Physics -- January 1987 -- Volume 55, Issue 1, pp. 67-70
- Frank Wilczek and Alfred Shapere, "Geometric Phases in Physics", World Scientific, 1989
- Charles Wheatstone Wikisource: "Note relating to M. Foucault's new mechanical proof of the Rotation of the Earth", pp 65--68
- Julian Rubin, The Invention of the Foucault Pendulum, Following the Path of Discovery, 2007, retrieved 2007-10-31. Directions for repeating Foucault's experiment, on amateur science site.

- Wolfe, Joe, " A derivation of the precession of the Foucault pendulum".
- " The Foucault Pendulum", derivation of the precession in polar coordinates.

Visualisations, video imaging and models

- " The Foucault Pendulum" By Joe Wolfe, with film clip and animations.
- " Foucault's Pendulum" by Jens-Peer Kuska with Jeff Bryant, The Wolfram Demonstrations Project: a computer model of the pendulum allowing manipulation of pendulum frequency, Earth rotation frequency, latitude, and time.
- " Webcam Kirchhoff-Institut für Physik, Universität Heidelberg".
- California academy of sciences, CA Foucault pendulum explanation, in friendly format
- Foucault pendulum model Exposition including a tabletop device that shows the Foucault effect in seconds.

History

- Foucault, M. L., Physical demonstration of the rotation of the Earth by means of the pendulum, Franklin Institute, 2000, retrieved 2007-10-31. Translation of his paper on Foucault pendulum.
- Tobin, William " The Life and Science of Léon Foucault".

Notable

- " South Pole Foucault Pendulum". Winter, 2001.

Educational supplies

- " Science Design's Small Portable Foucault Pendulum" A company selling a Foucault Pendulum for the classroom.

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Last updated on Friday September 26, 2008 at 14:03:40 PDT (GMT -0700)

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This article is licensed under the GNU Free Documentation License.

Last updated on Friday September 26, 2008 at 14:03:40 PDT (GMT -0700)

View this article at Wikipedia.org - Edit this article at Wikipedia.org - Donate to the Wikimedia Foundation

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