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Physical Pendulum01:06

Physical Pendulum

When a rigid body is hanging freely from a fixed pivot point and is displaced, it oscillates similar to a simple pendulum and is known as a physical pendulum. The period and angular frequency of a physical pendulum are obtained by using the small-angle approximation and drawing parallels with a spring-mass system. The small-angle approximation (sinθ=θ) is valid up to about 14°.
When dealing with complicated systems, the mass moment of inertia is an important parameter, as it describes the mass...
Torsional Pendulum01:09

Torsional Pendulum

A torsional pendulum involves the oscillation of a rigid body in which the restoring force is provided by the torsion in the string from which the rigid body is suspended. Ideally, the string should be massless; practically, its mass is much smaller than the rigid body's mass and is neglected.
As long as the rigid body's angular displacement is small, its oscillation can be modeled as a linear angular oscillation. The amplitude of the oscillation is an angle. The role of mass is played by the...
Simple Pendulum01:10

Simple Pendulum

A simple pendulum consists of a small diameter ball suspended from a string, which has negligible mass but is strong enough to not stretch. In our daily life, pendulums have many uses, such as in clocks, on a swing set, and on a sinker on a fishing line.
The period of a simple pendulum depends on two factors: its length and the acceleration due to gravity. The period is completely independent of any other factors, such as mass or maximum displacement. For small displacements, a pendulum is...
Forced Oscillations01:06

Forced Oscillations

When an oscillator is forced with a periodic driving force, the motion may seem chaotic. The motions of such oscillators are known as transients. After the transients die out, the oscillator reaches a steady state, where the motion is periodic, and the displacement is determined.
Faraday Disk Dynamo01:23

Faraday Disk Dynamo

A Faraday disk dynamo is a DC generator, producing an emf that is constant in time. It consists of a conducting disk that rotates with a constant angular velocity in the magnetic field, perpendicular to the disk's plane. The rotation of the disk causes a change in magnetic flux, which induces an emf, causing opposite charges to develop on the rim and in the center of the disk. The polarity of the induced emf can be determined by the direction of the magnetic field and the direction of the...
Magnetic Damping01:17

Magnetic Damping

Eddy currents can produce significant drag on motion, called magnetic damping. For instance, when a metallic pendulum bob swings between the poles of a strong magnet, significant drag acts on the bob as it enters and leaves the field, quickly damping the motion.
If, however, the bob is a slotted metal plate, the magnet produces a much smaller effect. When a slotted metal plate enters the field, an emf is induced by the change in flux; however, it is less effective because the slots limit the...

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Related Experiment Video

Updated: Jun 6, 2026

Online Virtual Reality Networked Control Laboratory Applied in Control Engineering Education
04:15

Online Virtual Reality Networked Control Laboratory Applied in Control Engineering Education

Published on: February 23, 2024

A Foucault's pendulum design.

Horacio R Salva1, Rubén E Benavides, Julio C Perez

  • 1Centro Atómico Bariloche, C.N.E.A., Av. Bustillo 9500, 8400 Bariloche, Argentina.

The Review of Scientific Instruments
|December 8, 2010
PubMed
Summary
This summary is machine-generated.

We developed a continuously operating Foucault pendulum system to precisely measure the Earth's rotation. This innovative design successfully detected medium-intensity earthquakes up to 765 km away.

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Area of Science:

  • Physics
  • Geophysics

Background:

  • Foucault pendulums demonstrate Earth's rotation but often require manual adjustments.
  • Continuous operation and precise measurement are key for advanced geophysical studies.

Purpose of the Study:

  • To design and evaluate a Foucault pendulum system with continuous operation.
  • To achieve precise measurements of the plane of oscillation's precession.
  • To assess the system's sensitivity for detecting seismic activity.

Main Methods:

  • Construction of two Foucault pendulums with lengths of 2.835 m and 4.975 m.
  • Implementation of a following system to maintain the oscillation plane.
  • Measurement of precession speed at a specific latitude.

Main Results:

  • The system enabled continuous operation of the Foucault pendulum.
  • Precession speeds were measured with high accuracy (0.5 and 0.2 deg/h).
  • The pendulum detected medium-intensity earthquakes occurring as far as 765 km.

Conclusions:

  • The developed Foucault pendulum system offers continuous operation and precise measurements.
  • The system demonstrates potential as a sensitive seismic detection instrument.
  • This design advances the application of Foucault pendulums in geophysics.