| Centripetal Force |
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its own right. Any physical force ( Gravity , Electrostatics , Friction , etc.) can be used to supply the centripetal force. The term ''centripetal force'' comes from the Latin words ''centrum'' ("center") and ''petere'' ("tend towards"). BASIC IDEA Objects moving in a straight line with constant speed have constant Velocity and require no force to do so, since they experience no acceleration. However, an object moving in a circle at constant speed has a changing direction of motion. Since velocity is a vector of speed and direction, a changing direction implies a changing velocity. The rate of this change in velocity is the centripetal acceleration. Differentiating the velocity vector gives . The centripetal acceleration varies with the radius of the circle and speed , becoming larger for higher speed and smaller radius. More precisely, the centripetal acceleration is given by : The direction of this acceleration is towards the center of the circle. By Newton's Second Law Of Motion , a force must be applied to a mass to produce this acceleration. The amount of force needed to move at speed on a circle of radius is exactly : ''(where m is mass, v is velocity, r is radius of the circle, and the minus sign denotes that the vector points to the center of the circle and ω = v / r is the Angular Velocity )''. If the applied force is less or more than , the object will move on a larger or smaller circle. In vector notation we can write: :, where is the angular velocity vector of the rotation and is a vector from an arbitrary point on the rotation axis to the body (with mass ). An object that moves in a Circular Path undergoes a continuous Acceleration towards the center of the circle. The Net Force that causes this acceleration is called a centripetal force (from Latin ''centrum'' "center" and ''petere'' "tend towards"). This term refers to the ''effect'' of the force (namely, to maintain the circular motion of the object); the ''origin'' of the centripetal force can be anything that causes a Force to exist. An object can travel in a circle with a constant Speed only if the Net Force acting on it is a centripetal force. (And if the object is traveling in a circle with a varying Speed , the component of the Net Force along the Radius is the centripetal force.) EXAMPLES For an orbiting Satellite , the centripetal force is supplied by the gravitational attraction between the satellite and its primary, and acts toward the center of mass which lies in the satellite's primary. For an object at the end of a rope rotating about a Vertical Axis , the centripetal force is the Horizontal component of the tension of the rope which acts towards the Axis Of Rotation . For a spinning object, internal Tensile Stress gives the centripetal force that holds the object together in one piece. COMMON MISUNDERSTANDINGS Centripetal force should not be mixed up with Centrifugal Force . In an Inertial Reference Frame (not rotating or accelerating), the centripetal force accelerates a particle in such a way that it moves along a circular path. In a corotating Reference Frame , a particle in circular motion appears to have zero velocity, if the rotation is not accounted for. The centripetal force is exactly cancelled by a centrifugal force that in this approach appears as a Fictitious Force . Centripetal forces are according to Newtonian mechanics true forces, while centrifugal forces only appear relative to rotating frames. Centripetal force should not be confused with Central Force , either. DERIVATION Simply use a Polar Coordinate System , assume a constant radius, and differentiate twice. Let r(t) be a vector that describes the position of a Point Mass as a function of time. Since we are assuming uniform Circular Motion , let r(t) = R·'''u'''r, where R is a constant (the radius of the circle) and '''u'''r is the Unit Vector pointing from the origin to the point mass. In terms of Cartesian unit vectors: : ''Note: unlike in Cartesian Coordinates where the unit vectors are constants, in Polar Coordinates the direction of the unit vectors depend on the angle between the x_axis and the point being described; the angle θ.'' So we differentiate to find velocity: : : : where ω is the angular velocity (just a short way of writing dθ/dt), uθ is the unit vector that is perpendicular to ur that points in the direction of increasing θ. In cartesian terms: uθ = -sin(θ) ux + cos(θ) uy This result for the velocity is good because it matches our expectation that the velocity should be directed around the circle, and that the magnitude of the velocity should be ωR. Differentiating again, we find that the acceleration, a is: : Thus, the radial component of the acceleration is: : GEOMETRIC DERIVATION (NO CALCULUS!) The circle on the left in Figure 1 shows an object moving on a circle at constant speed at four different times in its orbit. Its position is given by and its velocity is . The velocity vector is always perpendicular to the position vector; thus, since moves in a circle, so does . The circular motion of the velocity is shown in the circle on the right of Figure 1, along with its accelaration . Just as velocity is the rate of change of position, acceleration is the rate of change of velocity. The position and velocity vectors move in tandem, so they go around their circles in the same time . That time equals the distance traveled divided by the velocity : and, by analogy, : Setting these two equations equal and solving for , we get : Comparing the two circles in Figure 1 also shows that the acceleration points towards the center of the circle. SEE ALSO REFERENCES |
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