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Rotation around a fixed axis
Rotation around a fixed axis
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Sphere rotating around one of its diameters

Rotation around a fixed axis or axial rotation is a special case of rotational motion around an axis of rotation fixed, stationary, or static in three-dimensional space. This type of motion excludes the possibility of the instantaneous axis of rotation changing its orientation and cannot describe such phenomena as wobbling or precession. According to Euler's rotation theorem, simultaneous rotation along a number of stationary axes at the same time is impossible; if two rotations are forced at the same time, a new axis of rotation will result.

This concept assumes that the rotation is also stable, such that no torque is required to keep it going. The kinematics and dynamics of rotation around a fixed axis of a rigid body are mathematically much simpler than those for free rotation of a rigid body; they are entirely analogous to those of linear motion along a single fixed direction, which is not true for free rotation of a rigid body. The expressions for the kinetic energy of the object, and for the forces on the parts of the object, are also simpler for rotation around a fixed axis, than for general rotational motion. For these reasons, rotation around a fixed axis is typically taught in introductory physics courses after students have mastered linear motion; the full generality of rotational motion is not usually taught in introductory physics classes.

Translation and rotation

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An example of rotation. Each part of the worm drive—both the worm and the worm gear—is rotating on its own axis.

A rigid body is an object of a finite extent in which all the distances between the component particles are constant. No truly rigid body exists; external forces can deform any solid. For our purposes, then, a rigid body is a solid which requires large forces to deform it appreciably.

A change in the position of a particle in three-dimensional space can be completely specified by three coordinates. A change in the position of a rigid body is more complicated to describe. It can be regarded as a combination of two distinct types of motion: translational motion and circular motion.

Purely translational motion occurs when every particle of the body has the same instantaneous velocity as every other particle; then the path traced out by any particle is exactly parallel to the path traced out by every other particle in the body. Under translational motion, the change in the position of a rigid body is specified completely by three coordinates such as x, y, and z giving the displacement of any point, such as the center of mass, fixed to the rigid body.

Purely rotational motion occurs if every particle in the body moves in a circle about a single line. This line is called the axis of rotation. Then the radius vectors from the axis to all particles undergo the same angular displacement at the same time. The axis of rotation need not go through the body. In general, any rotation can be specified completely by the three angular displacements with respect to the rectangular-coordinate axes x, y, and z. Any change in the position of the rigid body is thus completely described by three translational and three rotational coordinates.

Any displacement of a rigid body may be arrived at by first subjecting the body to a displacement followed by a rotation, or conversely, to a rotation followed by a displacement. We already know that for any collection of particles—whether at rest with respect to one another, as in a rigid body, or in relative motion, like the exploding fragments of a shell, the acceleration of the center of mass is given by where M is the total mass of the system and acm is the acceleration of the center of mass. There remains the matter of describing the rotation of the body about the center of mass and relating it to the external forces acting on the body. The kinematics and dynamics of rotational motion around a single axis resemble the kinematics and dynamics of translational motion; rotational motion around a single axis even has a work-energy theorem analogous to that of particle dynamics.

Kinematics

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Angular displacement

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Given a particle that moves along the circumference of a circle of radius , having moved an arc length , its angular position is relative to its initial position, where .

In mathematics and physics it is conventional to treat the radian, a unit of plane angle, as 1, often omitting it. Units are converted as follows:

An angular displacement is a change in angular position: where is the angular displacement, is the initial angular position and is the final angular position.

Angular velocity

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Change in angular displacement per unit time is called angular velocity with direction along the axis of rotation. The symbol for angular velocity is and the units are typically rad s−1. Angular speed is the magnitude of angular velocity.

The instantaneous angular velocity is given by

Using the formula for angular position and letting , we have also where is the translational speed of the particle.

Angular velocity and frequency are related by

Angular acceleration

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A changing angular velocity indicates the presence of an angular acceleration in rigid body, typically measured in rad s−2. The average angular acceleration over a time interval Δt is given by

The instantaneous acceleration α(t) is given by

Thus, the angular acceleration is the rate of change of the angular velocity, just as acceleration is the rate of change of velocity.

The translational acceleration of a point on the object rotating is given by where r is the radius or distance from the axis of rotation. This is also the tangential component of acceleration: it is tangential to the direction of motion of the point. If this component is 0, the motion is uniform circular motion, and the velocity changes in direction only.

The radial acceleration (perpendicular to direction of motion) is given by It is directed towards the center of the rotational motion, and is often called the centripetal acceleration.

The angular acceleration is caused by the torque, which can have a positive or negative value in accordance with the convention of positive and negative angular frequency. The relationship between torque and angular acceleration (how difficult it is to start, stop, or otherwise change rotation) is given by the moment of inertia: .

Equations of kinematics

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When the angular acceleration is constant, the five quantities angular displacement , initial angular velocity , final angular velocity , angular acceleration , and time can be related by four equations of kinematics:

Dynamics

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Moment of inertia

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The moment of inertia of an object, symbolized by , is a measure of the object's resistance to changes to its rotation. The moment of inertia is measured in kilogram metre² (kg m2). It depends on the object's mass: increasing the mass of an object increases the moment of inertia. It also depends on the distribution of the mass: distributing the mass further from the center of rotation increases the moment of inertia by a greater degree. For a single particle of mass a distance from the axis of rotation, the moment of inertia is given by

Torque

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Torque is the twisting effect of a force F applied to a rotating object which is at position r from its axis of rotation. Mathematically, where × denotes the cross product. A net torque acting upon an object will produce an angular acceleration of the object according to just as F = ma in linear dynamics.

The work done by a torque acting on an object equals the magnitude of the torque times the angle through which the torque is applied:

The power of a torque is equal to the work done by the torque per unit time, hence:

Angular momentum

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The angular momentum is a measure of the difficulty of bringing a rotating object to rest. It is given by where the sum is taken over all particles in the object.

Angular momentum is the product of moment of inertia and angular velocity: just as p = mv in linear dynamics.

The analog of linear momentum in rotational motion is angular momentum. The greater the angular momentum of the spinning object such as a top, the greater its tendency to continue to spin.

The angular momentum of a rotating body is proportional to its mass and to how rapidly it is turning. In addition, the angular momentum depends on how the mass is distributed relative to the axis of rotation: the further away the mass is located from the axis of rotation, the greater the angular momentum. A flat disk such as a record turntable has less angular momentum than a hollow cylinder of the same mass and velocity of rotation.

Like linear momentum, angular momentum is vector quantity, and its conservation implies that the direction of the spin axis tends to remain unchanged. For this reason, the spinning top remains upright whereas a stationary one falls over immediately.

The angular momentum equation can be used to relate the moment of the resultant force on a body about an axis (sometimes called torque), and the rate of rotation about that axis.

Torque and angular momentum are related according to just as F = dp/dt in linear dynamics. In the absence of an external torque, the angular momentum of a body remains constant. The conservation of angular momentum is notably demonstrated in figure skating: when pulling the arms closer to the body during a spin, the moment of inertia is decreased, and so the angular velocity is increased.

Kinetic energy

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The kinetic energy due to the rotation of the body is given by

just as in linear dynamics.

Kinetic energy is the energy of motion. The amount of translational kinetic energy found in two variables: the mass of the object () and the speed of the object () as shown in the equation above. Kinetic energy must always be either zero or a positive value. While velocity can have either a positive or negative value, velocity squared will always be positive.[1]

Vector expression

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The above development is a special case of general rotational motion. In the general case, angular displacement, angular velocity, angular acceleration, and torque are considered to be vectors.

An angular displacement is considered to be a vector, pointing along the axis, of magnitude equal to that of . A right-hand rule is used to find which way it points along the axis; if the fingers of the right hand are curled to point in the way that the object has rotated, then the thumb of the right hand points in the direction of the vector.

The angular velocity vector also points along the axis of rotation in the same way as the angular displacements it causes. If a disk spins counterclockwise as seen from above, its angular velocity vector points upwards. Similarly, the angular acceleration vector points along the axis of rotation in the same direction that the angular velocity would point if the angular acceleration were maintained for a long time.

The torque vector points along the axis around which the torque tends to cause rotation. To maintain rotation around a fixed axis, the total torque vector has to be along the axis, so that it only changes the magnitude and not the direction of the angular velocity vector. In the case of a hinge, only the component of the torque vector along the axis has an effect on the rotation, other forces and torques are compensated by the structure.

Mathematical representation

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The angle θ and axis unit vector e define a rotation, concisely represented by the rotation vector θe.

In mathematics, the axis–angle representation parameterizes a rotation in a three-dimensional Euclidean space by two quantities: a unit vector e indicating the direction of an axis of rotation, and an angle of rotation θ describing the magnitude and sense (e.g., clockwise) of the rotation about the axis. Only two numbers, not three, are needed to define the direction of a unit vector e rooted at the origin because the magnitude of e is constrained. For example, the elevation and azimuth angles of e suffice to locate it in any particular Cartesian coordinate frame.

By Rodrigues' rotation formula, the angle and axis determine a transformation that rotates three-dimensional vectors. The rotation occurs in the sense prescribed by the right-hand rule.

The rotation axis is sometimes called the Euler axis. The axis–angle representation is predicated on Euler's rotation theorem, which dictates that any rotation or sequence of rotations of a rigid body in a three-dimensional space is equivalent to a pure rotation about a single fixed axis.

It is one of many rotation formalisms in three dimensions.

Examples and applications

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Constant angular speed

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The simplest case of rotation not around a fixed axis is that of constant angular speed. Then the total torque is zero. For the example of the Earth rotating around its axis, there is very little friction. For a fan, the motor applies a torque to compensate for friction. Similar to the fan, equipment found in the mass production manufacturing industry demonstrate rotation around a fixed axis effectively. For example, a multi-spindle lathe is used to rotate the material on its axis to effectively increase the productivity of cutting, deformation and turning operations.[2] The angle of rotation is a linear function of time, which modulo 360° is a periodic function.

An example of this is the two-body problem with circular orbits.

Centripetal force

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Internal tensile stress provides the centripetal force that keeps a spinning object together. A rigid body model neglects the accompanying strain. If the body is not rigid this strain will cause it to change shape. This is expressed as the object changing shape due to the "centrifugal force".

Celestial bodies rotating about each other often have elliptic orbits. The special case of circular orbits is an example of a rotation around a fixed axis: this axis is the line through the center of mass perpendicular to the plane of motion. The centripetal force is provided by gravity, see also two-body problem. This usually also applies for a spinning celestial body, so it need not be solid to keep together unless the angular speed is too high in relation to its density. (It will, however, tend to become oblate.) For example, a spinning celestial body of water must take at least 3 hours and 18 minutes to rotate, regardless of size, or the water will separate[citation needed]. If the density of the fluid is higher the time can be less. See orbital period.[3]

Plane of rotation

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In geometry, a plane of rotation is an abstract object used to describe or visualize rotations in space.

The main use for planes of rotation is in describing more complex rotations in four-dimensional space and higher dimensions, where they can be used to break down the rotations into simpler parts. This can be done using geometric algebra, with the planes of rotations associated with simple bivectors in the algebra.[4]

Planes of rotation are not used much in two and three dimensions, as in two dimensions there is only one plane (so, identifying the plane of rotation is trivial and rarely done), while in three dimensions the axis of rotation serves the same purpose and is the more established approach.

Mathematically such planes can be described in a number of ways. They can be described in terms of planes and angles of rotation. They can be associated with bivectors from geometric algebra. They are related to the eigenvalues and eigenvectors of a rotation matrix. And in particular dimensions they are related to other algebraic and geometric properties, which can then be generalised to other dimensions.

See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
Rotation around a fixed axis is a type of rotational motion in classical mechanics in which a rigid body, which maintains its shape and size during the motion, turns about a stationary axis perpendicular to the plane of rotation. This form of motion, also known as plane rotation or two-dimensional rotation, describes scenarios such as a door swinging on its hinges or a wheel spinning on an axle, where every point on the body traces a circular path centered on the axis. The kinematics of fixed-axis parallels linear kinematics but uses angular variables: θ (measured in radians), ω = dθ/dt, and α = dω/dt. For constant , the relationships are analogous to those in , such as θ = θ₀ + ω₀t + (1/2)αt² and ω = ω₀ + αt, with the tangential linear and of a point at radial r from the axis given by v = ωr and a = αr, respectively. In dynamics, the rotational equivalent of mass is the moment of inertia I, defined as I = Σ mᵢ rᵢ² for a system of particles, which quantifies the body's resistance to and depends on the mass distribution relative to the axis. Torque τ, the rotational analog of , drives via τ = Iα, where τ = r F sinφ for a F applied perpendicularly at r from the axis. L = Iω is conserved when net is zero, a principle central to applications like balancing rotating machinery or analyzing planetary motion approximations. These concepts extend to considerations, with rotational (1/2)Iω² and work done by τ Δθ, underpinning engineering designs in turbines, engines, and gyroscopes.

Fundamentals

Translation versus Rotation

In translational motion, all points of a rigid body move in parallel paths with vectors, maintaining constant distances and orientations relative to one another, akin to the motion of a under net external forces. This type of motion simplifies because there is no internal relative displacement within the body. In contrast, rotational motion around a fixed axis involves points of the tracing circular paths centered on that axis, with each point's directed to the radial line from the axis to the point, leading to varying speeds depending on from the axis. Unlike , this motion introduces , where the body's orientation changes continuously while distances between points remain fixed. The conceptual distinction between these motion types emerged in early classical mechanics, where Isaac Newton explored rotation through examples like spinning tops and planetary orbits, viewing it as analogous to linear translation but modified by curved trajectories and environmental resistance. Building on this, Leonhard Euler advanced the understanding around 1736 by systematically decomposing rigid body motion into center-of-mass translation and pure rotation about an axis, establishing rotation as a fundamental counterpart to translation. Qualitative examples illustrate this difference clearly: the straight-line progression of a car along a road represents translation, as every component advances uniformly in the same direction without altering the vehicle's shape or facing. Conversely, a wheel rotating on its stationary axle embodies rotation around a fixed axis, with points on the rim following circular arcs while the hub remains fixed, highlighting the perpendicular velocity relative to the axis.

Fixed Axis and Rigid Body Assumptions

Rotation around a fixed axis refers to the rotational motion of a body about a stationary line in space, where the axis itself undergoes no translation. This setup constrains the motion such that the axis serves as a fixed reference, allowing the body's orientation to be described solely by the angle of rotation about it./16:_Two_Dimensional_Rotational_Kinematics/16.02:_Fixed_Axis_Rotation-_Rotational_Kinematics) The assumes the body is rigid, meaning all points within the body maintain distances from one another, with no deformation occurring during the . Under this assumption, every particle in the body follows a circular path centered on the axis, with the radius equal to its from the axis. These assumptions imply that the motion is purely rotational and confined to a plane perpendicular to the fixed axis, where the linear speed of any point varies directly with its distance from the axis. In three dimensions, this fixed-axis constraint reduces the general six degrees of freedom of a rigid body to a single degree of freedom, corresponding to the rotation angle about the axis, thereby simplifying the description from arbitrary rigid body motion.

Kinematics

Angular Displacement

Angular displacement, denoted as θ\theta, is the change in the angular position of a rotating about a fixed axis, defined as the angle swept out by a reference line (such as a radius vector from the axis to a point on the body) from its initial to final orientation. This quantity describes the rotational equivalent of linear displacement in translational motion. The primary unit of angular displacement is the radian (rad), a dimensionless measure where one radian corresponds to the angle subtended by an arc length equal to the radius of the circle. For a point at a perpendicular distance rr from the axis, the corresponding arc length ss along the path is related by the formula s=rθs = r \theta, valid when θ\theta is in radians. This relation highlights how angular displacement scales with distance from the axis, enabling the connection between rotational and linear descriptions of motion. Angular displacement can also be measured in degrees, with the conversion θrad=θdeg×π180\theta_{\mathrm{rad}} = \theta_{\mathrm{deg}} \times \frac{\pi}{180}; for instance, a full rotation is 2π2\pi radians or 360 degrees. As a signed quantity, angular displacement carries directional information: it is positive for counterclockwise rotations and negative for clockwise rotations when viewed along the axis, consistent with the convention for rotational quantities. In this rule, curling the fingers of the right hand in the direction of rotation points the thumb along the positive axis direction for positive θ\theta. For continuous motion, the infinitesimal angular displacement dθd\theta represents an arbitrarily small change in angular position, fundamental to analyzing smooth rotational paths.

Angular Velocity

In rotational kinematics about a fixed axis, quantifies the rate at which changes with time. The average , ωavg\omega_\text{avg}, over a time interval is defined as the total Δθ\Delta \theta divided by the elapsed time Δt\Delta t, expressed as ωavg=ΔθΔt\omega_\text{avg} = \frac{\Delta \theta}{\Delta t}. The instantaneous ω\omega represents the angular speed at a specific moment and is the time derivative of the θ\theta, given by ω=dθdt\omega = \frac{d\theta}{dt}. This scalar quantity has units of radians per second (rad/s), reflecting the dimensionless nature of the radian combined with inverse time. Angular velocity is often represented as a vector ω\vec{\omega}
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