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acceleration
please note:
- the content below is remote from Wikipedia
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{{about|acceleration in physics|other uses|Acceleration (disambiguation)|and|Accelerate (disambiguation)}}{{Use British English|date=February 2016}}- the content below is remote from Wikipedia
- it has been imported raw for GetWiki
factoids | |
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Definition and properties
(File:Kinematics.svg|thumb|300px|Kinematic quantities of a classical particle: mass m, position r, velocity v, acceleration a.)Average acceleration
File:Acceleration as derivative of velocity along trajectory.svg|right|thumb|Acceleration is the rate of change of velocity. At any point on a trajectory, the magnitude of the acceleration is given by the rate of change of velocity in both magnitude and direction at that point. The true acceleration at time t is found in the limit as time intervaltime intervalAn object's average acceleration over a period of time is its change in velocity ( Delta mathbf{v}) divided by the duration of the period ( Delta t). Mathematically,
bar{mathbf{a}} = frac{Delta mathbf{v}}{Delta t}.
Instantaneous acceleration
File:1-D kinematics.svg|thumb|right|From bottom to top: {{bulleted list
| an acceleration function a(t);
| the integral of the acceleration is the velocity function v(t);
| and the integral of the velocity is the distance function s(t).
}}Instantaneous acceleration, meanwhile, is the limit of the average acceleration over an infinitesimal interval of time. In the terms of calculus, instantaneous acceleration is the derivative of the velocity vector with respect to time:
| the integral of the acceleration is the velocity function v(t);
| and the integral of the velocity is the distance function s(t).
mathbf{a} = lim_{{Delta t}to 0} frac{Delta mathbf{v}}{Delta t} = frac{dmathbf{v}}{dt}
(Here and elsewhere, if motion is in a straight line, vector quantities can be substituted by scalars in the equations.)It can be seen that the integral of the acceleration function {{math|a(t)}} is the velocity function {{math|v(t)}}; that is, the area under the curve of an acceleration vs. time ({{math|a}} vs. {{math|t}}) graph corresponds to velocity.
mathbf{v} = int mathbf{a} dt
As acceleration is defined as the derivative of velocity, {{math|v}}, with respect to time {{math|t}} and velocity is defined as the derivative of position, {{math|x}}, with respect to time, acceleration can be thought of as the second derivative of {{math|x}} with respect to {{math|t}}:
mathbf{a} = frac{dmathbf{v}}{dt} = frac{d^2mathbf{x}}{dt^2}
Units
Acceleration has the dimensions of velocity (L/T) divided by time, i.e. L Tâˆ’2. The SI unit of acceleration is the metre per second squared (m sâˆ’2); or "metre per second per second", as the velocity in metres per second changes by the acceleration value, every second.Other forms
An object moving in a circular motion—such as a satellite orbiting the Earth—is accelerating due to the change of direction of motion, although its speed may be constant. In this case it is said to be undergoing centripetal (directed towards the center) acceleration.Proper acceleration, the acceleration of a body relative to a free-fall condition, is measured by an instrument called an accelerometer.In classical mechanics, for a body with constant mass, the (vector) acceleration of the body's center of mass is proportional to the net force vector (i.e. sum of all forces) acting on it (Newton's second law):
mathbf{F} = mmathbf{a} quad to quad mathbf{a} = frac{mathbf{F}}{m}
where F is the net force acting on the body, m is the mass of the body, and a is the center-of-mass acceleration. As speeds approach the speed of light, relativistic effects become increasingly large.Tangential and centripetal acceleration
(File:Oscillating pendulum.gif|thumb|left|An oscillating pendulum, with velocity and acceleration marked. It experiences both tangential and centripetal acceleration.)(File:Acceleration components.JPG|right|thumb|Components of acceleration for a curved motion. The tangential component at is due to the change in speed of traversal, and points along the curve in the direction of the velocity vector (or in the opposite direction). The normal component (also called centripetal component for circular motion) ac is due to the change in direction of the velocity vector and is normal to the trajectory, pointing toward the center of curvature of the path.){{see also|Centripetal force#Local coordinates|l1=Local coordinates}}The velocity of a particle moving on a curved path as a function of time can be written as:
mathbf{v} (t) =v(t) frac {mathbf{v}(t)}{v(t)} = v(t) mathbf{u}_mathrm
(t) , with v(t) equal to the speed of travel along the path, and
mathbf{u}_mathrm = frac {mathbf{v}(t)}{v(t)} ,
a unit vector tangent to the path pointing in the direction of motion at the chosen moment in time. Taking into account both the changing speed v(t) and the changing direction of ut, the acceleration of a particle moving on a curved path can be written using the chain rule of differentiationWEB, Weisstein, Eric W., Chain Rule,weblink Wolfram MathWorld, Wolfram Research, 2 August 2016, for the product of two functions of time as:
begin{alignat}{3}
mathbf{a} & = frac{mathrm{d} mathbf{v}}{mathrm{d}t}
& = frac{mathrm{d}v }{mathrm{d}t} mathbf{u}_mathrm +v(t)frac{d mathbf{u}_mathrm}{dt}
& = frac{mathrm{d}v }{mathrm{d}t} mathbf{u}_mathrm+ frac{v^2}{r}mathbf{u}_mathrm{n} ,
end{alignat}where un is the unit (inward) normal vector to the particle's trajectory (also called the principal normal), and r is its instantaneous radius of curvature based upon the osculating circle at time t. These components are called the tangential acceleration and the normal or radial acceleration (or centripetal acceleration in circular motion, see also circular motion and centripetal force).Geometrical analysis of three-dimensional space curves, which explains tangent, (principal) normal and binormal, is described by the Frenetâ€“Serret formulas.BOOK, Mathematical Techniques for Engineers and Scientists, Larry C. Andrews, Ronald L. Phillips, 164,weblinkpublisher = SPIE Press AUTHOR1=CH V RAMANA MURTHY ISBN = 978-81-219-2082-7PUBLISHER = S. CHAND & CO. LOCATION = NEW DELHI, & = frac{mathrm{d}v }{mathrm{d}t} mathbf{u}_mathrm+ frac{v^2}{r}mathbf{u}_mathrm{n} ,
Special cases
Uniform acceleration
(File:Strecke und konstante Beschleunigung.png|thumb|Calculation of the speed difference for a uniform acceleration)Uniform or constant acceleration is a type of motion in which the velocity of an object changes by an equal amount in every equal time period.A frequently cited example of uniform acceleration is that of an object in free fall in a uniform gravitational field. The acceleration of a falling body in the absence of resistances to motion is dependent only on the gravitational field strength g (also called acceleration due to gravity). By Newton's Second Law the force mathbf{F_g} acting on a body is given by:
mathbf{F_g} = m mathbf{g}
Because of the simple analytic properties of the case of constant acceleration, there are simple formulas relating the displacement, initial and time-dependent velocities, and acceleration to the time elapsed:BOOK, Physics for you: revised national curriculum edition for GCSE, Keith Johnson, Nelson Thornes, 2001, 4th, 135,weblink 978-0-7487-6236-1,
mathbf{s}(t) = mathbf{s}_0 + mathbf{v}_0 t+ tfrac{1}{2} mathbf{a}t^2 = mathbf{s}_0 + frac{mathbf{v}_0+mathbf{v}(t)}{2}t
mathbf{v}(t) = mathbf{v}_0 + mathbf{a} t
{v^2}(t) = {v_0}^2 + 2mathbf{a cdot}[mathbf{s}(t)-mathbf{s}_0]
where - t is the elapsed time,
- mathbf{s}_0 is the initial displacement from the origin,
- mathbf{s}(t) is the displacement from the origin at time t,
- mathbf{v}_0 is the initial velocity,
- mathbf{v}(t) is the velocity at time t, and
- mathbf{a} is the uniform rate of acceleration.
Circular motion
{{multiple image|align = vertical|width1 = 100|image1 = Position vector plane polar coords.svg|caption1 = Position vector r, always points radially from the origin.|width2 = 150|image2 = Velocity vector plane polar coords.svg|caption2 = Velocity vector v, always tangent to the path of motion.|width3 = 200|image3 = Acceleration vector plane polar coords.svg|caption3 = Acceleration vector a, not parallel to the radial motion but offset by the angular and Coriolis accelerations, nor tangent to the path but offset by the centripetal and radial accelerations.|footer = Kinematic vectors in plane polar coordinates. Notice the setup is not restricted to 2d space, but may represent the osculating plane plane in a point of an arbitrary curve in any higher dimension.}}In uniform circular motion, that is moving with constant speed along a circular path, a particle experiences an acceleration resulting from the change of the direction of the velocity vector, while its magnitude remains constant. The derivative of the location of a point on a curve with respect to time, i.e. its velocity, turns out to be always exactly tangential to the curve, respectively orthogonal to the radius in this point. Since in uniform motion the velocity in the tangential direction does not change, the acceleration must be in radial direction, pointing to the center of the circle. This acceleration constantly changes the direction of the velocity to be tangent in the neighboring point, thereby rotating the velocity vector along the circle.â€¢ For a given speed v, the magnitude of this geometrically caused acceleration (centripetal acceleration) is inversely proportional to the radius r of the circle, and increases as the square of this speed:
a_c = frac {v^2} {r};.
â€¢ Note that, for a given angular velocity omega, the centripetal acceleration is directly proportional to radius r. This is due to the dependence of velocity v on the radius r.
v = omega r.
Expressing centripetal acceleration vector in polar components, where mathbf{r} is a vector from the centre of the circle to the particle with magnitude equal to this distance, and considering the orientation of the acceleration towards the center, yields
mathbf {a_c}= -frac{v^2}{|mathbf {r}|}cdot frac{mathbf {r}}{|mathbf {r}|};.
As usual in rotations, the speed v of a particle may be expressed as an angular speed with respect to a point at the distance r as
omega = frac {v}{r}.
Thus mathbf {a_c}= -omega^2 mathbf {r};. This acceleration and the mass of the particle determine the necessary centripetal force, directed toward the centre of the circle, as the net force acting on this particle to keep it in this uniform circular motion. The so-called 'centrifugal force', appearing to act outward on the body, is a so-called pseudo force experienced in the frame of reference of the body in circular motion, due to the body's linear momentum, a vector tangent to the circle of motion.In a nonuniform circular motion, i.e., the speed along the curved path is changing, the acceleration has a non-zero component tangential to the curve, and is not confined to the principal normal, which directs to the center of the osculating circle, that determines the radius r for the centripetal acceleration. The tangential component is given by the angular acceleration alpha, i.e., the rate of change alpha = dotomega of the angular speed omega times the radius r. That is,
a_c = r alpha.
The sign of the tangential component of the acceleration is determined by the sign of the angular acceleration (alpha), and the tangent is of course always directed at right angles to the radius vector.Relation to relativity
Special relativity
The special theory of relativity describes the behavior of objects traveling relative to other objects at speeds approaching that of light in a vacuum. Newtonian mechanics is exactly revealed to be an approximation to reality, valid to great accuracy at lower speeds. As the relevant speeds increase toward the speed of light, acceleration no longer follows classical equations.As speeds approach that of light, the acceleration produced by a given force decreases, becoming infinitesimally small as light speed is approached; an object with mass can approach this speed asymptotically, but never reach it.General relativity
Unless the state of motion of an object is known, it is impossible to distinguish whether an observed force is due to gravity or to accelerationâ€”gravity and inertial acceleration have identical effects. Albert Einstein called this the equivalence principle, and said that only observers who feel no force at allâ€”including the force of gravityâ€”are justified in concluding that they are not accelerating.Brian Greene, (The Fabric of the Cosmos: Space, Time, and the Texture of Reality), page 67. Vintage {{ISBN|0-375-72720-5}}Conversions
{{Acceleration conversions}}See also
{{div col |colwidth=22em}}- Inertia
- Jerk (physics)
- Four-vector: making the connection between space and time explicit
- Gravitational acceleration
- Acceleration (differential geometry)
- Orders of magnitude (acceleration)
- Shock (mechanics)
- Shock and vibration data loggermeasuring 3-axis acceleration
- Space travel using constant acceleration
- Specific force
References
{{reflist}}External links
- Acceleration Calculator Simple acceleration unit converter
- weblink" title="web.archive.org/web/20101108131449weblink">Measurespeed.com - Acceleration Calculator Based on starting & ending speed and time elapsed.
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