In physics, acceleration is a measure of how fast and in what direction an object's speed and direction of motion are changing. It is defined as the rate of change of the velocity. Like velocity, acceleration has a magnitude and a direction, making it a vector quantity. The SI unit for acceleration is metre per second squared (m⋅s−2, m/s2). The tangential acceleration of an object is the component of the acceleration which is in the same direction as the motion (or tangential velocity) of the object. When the velocity of the object does not change direction, this is called linear acceleration. Deceleration or retardation, on the other hand, is the component of the acceleration in the opposite (or antiparallel) direction to the tangential velocity. Radial acceleration or normal acceleration (or centripetal acceleration during circular motions) is the component of the acceleration that changes the direction of the object's velocity. In Newtonian mechanics, the acceleration of a mass arises from forces acting on it, with its net acceleration being a result of the net force acting on it. By Newton's second law, the magnitude of the net acceleration will be proportional to the magnitude of the net force acting on the object and inversely proportional to the mass of the object, while the direction of the net acceleration will be the same as the direction of the net force.
Definition and properties
Average acceleration
An object's average acceleration a ¯ {\displaystyle {\bar {\mathbf {a} }}} over a period of time is its change in velocity, Δ v {\displaystyle \Delta \mathbf {v} } , divided by the duration of the period, Δ t {\displaystyle \Delta t} . Mathematically,
a ¯ = Δ v Δ t . {\displaystyle {\bar {\mathbf {a} }}={\frac {\Delta \mathbf {v} }{\Delta t}}.} The average acceleration is the simplest way to measure acceleration, requiring only knowledge of the change in velocity and the change in time. In a strict sense, the average acceleration is the only true acceleration one is able to directly measure without appealing to an empirical law, meaning that it is the most fundamental form of acceleration measurement. The average acceleration is most often used to approximate the kinematics of an object by assuming that the velocity changes linearly with time. Over short time intervals, we can often assume that the acceleration is uniform, meaning acceleration a {\displaystyle \mathbf {a} } of the object will be exactly equal to the average acceleration a ¯ {\displaystyle {\bar {\mathbf {a} }}} (see subsection Uniform acceleration for details.) By Newton's second law of motion, the average acceleration is related to the average force f ¯ {\displaystyle {\bar {\mathbf {f} }}} on a particle of mass m {\displaystyle m} by,
f ¯ = m a ¯ . {\displaystyle {\bar {\mathbf {f} }}=m{\bar {\mathbf {a} }}.} This means that a measurement of the average acceleration is also a measurement of the average force (also known as impulse J = f ¯ {\displaystyle \mathbf {J} ={\bar {\mathbf {f} }}} .)
Instantaneous acceleration
Instantaneous acceleration 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:
a = lim Δ t → 0 Δ v Δ t = d v d t = v ˙ . {\displaystyle \mathbf {a} =\lim _{{\Delta t}\to 0}{\frac {\Delta \mathbf {v} }{\Delta t}}={\frac {d\mathbf {v} }{dt}}={\dot {\mathbf {v} }}.}
As acceleration is defined as the derivative of velocity, v, with respect to time t and velocity is defined as the derivative of position, x, with respect to time, acceleration can be thought of as the second derivative of x with respect to t:
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