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The Angular Frequency of a Pendulum equation calculates the angular frequency of a simple pendulum with a small amplitude.

INSTRUCTIONS: Choose the preferred units and enter the following:

(L) Length of Pendulum
(g) Acceleration due to Gravity

Angular Frequency (ω): The calculator returns the angular frequency of the pendulum.

The Math / Science

The Pendulum Angular Frequency equation is:

ω=`sqrt(k/m)`

when `k= (m*g)/L`. After substituting for k, we get the resulting equation of ω=`sqrt(g/L)`.

Acceleration Due to Gravity

g - gravitational acceleration near whatever massive body is used in this calculation. The value defaults to the acceleration due to gravity at Earth's sea level but can be set to the gravitational acceleration for any planet or other body or for slightly different values on Earth including:

Usage

This equation has g, the gravitational acceleration as an input. It defaults to the standard gravitational acceleration value for gravity at the surface of the Earth but you may modify it to any gravity you desire. This allows the user to examine the pendulum's angular frequency on various planets or even as it would react close to a more massive body.

The answer displays in1/sec, which is equivalent to Hertz, and in this particular context actually means rotations or cycles per second.

A pendulum is a weight suspended from a pivot so that it can swing freely. When a pendulum is displaced sideways from its resting equilibrium position, it is subject to a restoring force due to gravity that will accelerate it back toward the equilibrium position. When released, the restoring force combined with the pendulum's mass causes it to oscillate about the equilibrium position, swinging back and forth. The time for one complete cycle, a left swing and a right swing, is called the period. The period depends on the length of the pendulum, and also to a slight degree on the amplitude, the width of the pendulum's swing.

Types of Pendulums:

Simple Pendulum – A single mass (bob) attached to a string or rod that swings back and forth.
Compound Pendulum – A rigid body swinging about a pivot point.
Foucault Pendulum – Demonstrates the Earth's rotation by slowly changing its plane of motion.
Torsional Pendulum – Rotates around its axis instead of swinging back and forth.

Applications of Pendulums:

Used in clocks (grandfather clocks) to regulate time.
Scientific experiments (measuring gravity).
Seismometers to detect earthquakes.
Amusement park rides.

The Pendulum Calculator includes the basic physics formulas and constants for the properties of a pendulum. These include the following:

Pendulum Frequency: Computes the frequency (ƒ) of a simple pendulum based on the length (L) of the pendulum.
Period of a Pendulum: Computes the period (T) of a simple pendulum based on the length (L) of the pendulum arm and the acceleration due to gravity (g).
Pendulum Length: Computes the length (L) of a simple pendulum based on the period (T) of the pendulum arm and the acceleration due to gravity (g).
Pendulum Angular Frequency: Computes the angular frequency of a simple pendulum with a small amplitude.
Angular Frequency of a Physical Pendulum: Computes the approximate value of the angular frequency given that the amplitude of the pendulum is small based on the mass, distance from pivot point to center of mass and the moment of inertia.
Restoring Torque to a Pendulum: Computes the restoring torque (τz) on a physical pendulum based on the mass (m), acceleration due to gravity (g), distance to the center of gravity (d) and the displacement angle (θ).
Restoring Force on a Pendulum: Approximates the restoring force on a pendulum based on the mass, length of pendulum and length of arc.
Rotational Acceleration of a Physical Pendulum: Approximates the rotational acceleration of a physical pendulum based on the mass (m), acceleration due to gravity (g), distance to the center of gravity (d), impulse (I) and the angle (Θ)
(g) acceleration due to gravity

References

Young, Hugh and Freeman, Roger. University Physics With Modern Physics. Addison-Wesley, 2008. 12th Edition, (ISBN-13: 978-0321500625 ISBN-10: 0321500628 ) Pg 437, eq 13.32