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Circular Motion

Circular Motion. Definitions. Circular motion: when an object moves in a two-dimensional circular path Spin: object rotates about an axis that pass through the object itself. Definitions. Orbital motion: object circles an axis that does not pass through the object itself.

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Circular Motion

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  1. Circular Motion

  2. Definitions • Circular motion: when an object moves in a two-dimensional circular path • Spin: object rotates about an axis that pass through the object itself

  3. Definitions • Orbital motion: object circles an axis that does not pass through the object itself

  4. Circle Terminology • Radius • Diameter • Chord • Tangent • Arc

  5. Establishing Position • The simplest coordinate system to use for circular motion puts the tails of position vectors at the center of the circular motion.

  6. Polar Coordinates (r, θ) • magnitude of r = radius of circular path • θ = angle of rotation • θ is measured in radians

  7. Radian Measure • Definition of a radian: One radian is equal to the central angle of a circle that subtends an arc of the circle’s circumference whose length is equal to the length of the radius of the circle.

  8. Radian Measure • There are exactly 2π radians in one complete circle. • Unit analysis: • 180° = π radians

  9. Establishing Position • In circular motion, change of position is measured in angular units. • θ can have a positive or negative value.

  10. Δθ ω = Δt Speed and Velocity • ω represents the time-rate of change of angular position; this is also called the angular speed. • By definition:

  11. Δθ ω = Δt Speed and Velocity • ω is a scalar quantity. • It is commonly expressed as number of rotations or revolutions per unit of time. • Ex. “rpm”

  12. Δθ ω = Δt Speed and Velocity • If angular speed is constant, then the rotating object experiences uniform circular motion.

  13. rad or s-1 s Speed and Velocity • In the SI, the units are radians per second. • Written as:

  14. Speed and Velocity • The velocity vector of a particle in circular motion is tangent to the circular path. • This velocity is called tangential velocity.

  15. Speed and Velocity • The magnitude of the tangential velocity is called the tangential speed, vt. vt = |vt|

  16. l vt = Δt Speed and Velocity • Another formula for tangential speed is: • arclengthl = r × Δθ

  17. rΔθ vt = Δt Speed and Velocity • average tangential speed:

  18. Δv a = Δt vt2 a = r Acceleration • Linear motion: • Circular motion:

  19. Acceleration • The instantaneous acceleration vector always points toward the center of the circular path. • This is called centripetal acceleration.

  20. vt2 ac = m/s² r Acceleration • The magnitude of centripetal acceleration is: • For all circular motion at constant radius and speed

  21. Acceleration • Another formula for centripetal acceleration: ac = -rω2

  22. Angular Velocity • Uniform angular velocity (ω) implies that the rate and direction of angular speed are constant.

  23. Angular Velocity • Right-hand rule of circular motion:

  24. Angular Velocity • Nonuniform circular motion is common in the real world. • Its properties are similar to uniform circular motion, but the mathematics are more challenging.

  25. ω2 – ω1 Δω α = = Δt Δt Angular Acceleration • change in angular velocity • notation: α • average angular acceleration:

  26. ω2 – ω1 Δω α = = Δt Δt Angular Acceleration • units are rad/s², or s-2 • direction is parallel to the rotational axis

  27. Tangential Acceleration • defined as the time-rate of change of the magnitude of tangential velocity

  28. Δvt at = =αr Δt Tangential Acceleration • average tangential acceleration:

  29. Tangential Acceleration • instantaneous tangential acceleration: at =αr Don’t be too concerned about the calculus involved here...

  30. Tangential Acceleration • Instantaneous tangential acceleration is tangent to the circular path at the object’s position.

  31. Tangential Acceleration • If tangential speed is increasing, then tangential acceleration is in the same direction as rotation.

  32. Tangential Acceleration • If tangential speed is decreasing, then tangential acceleration points in the opposite direction of rotation.

  33. Equations of Circular Motion • note the substitutions here:

  34. Dynamics of Circular Motion

  35. Centripetal Force • in circular motion, the unbalanced force sum that produces centripetal acceleration • abbreviated Fc

  36. mvt² Fc = r Centripetal Force • to calculate the magnitude of Fc:

  37. Centripetal Force • Centipetal force can be exerted through: • tension • gravity

  38. Torque • the product of a force and the force’s position vector • abbreviated: τ • magnitude calculated by the formula τ = rF sin θ

  39. Torque τ = rF sin θ • r = magnitude of position vector from center to where force is applied • F = magnitude of applied force

  40. Torque τ = rF sin θ • θ = smallest angle between vectors r and F when they are positioned tail-to-tail • r sin θ is called the moment arm (l) of a torque

  41. Torque • Maximum torque is obtained when the force is perpendicular to the position vector. • Angular acceleration is produced by unbalanced torques.

  42. Torque • Zero net torques is called rotational equilibrium. • Στ= 0 N·m

  43. F1 l2 = F2 l1 Torque • Law of Moments: l1F1 = l2F2 • Rearranged:

  44. Universal Gravitation

  45. The Ideas • Geocentric: The earth is the center of the universe • Heliocentric: The sun is the center of the universe • Some observations did not conform to the geocentric view.

  46. The Ideas • Ptolemy developed a theory that involved epicycles in deferent orbits. • For centuries, the geocentric view prevailed.

  47. The Ideas • Copernicus concluded the geocentric theory was faulty. • His heliocentric theory was simpler.

  48. The Ideas • Tycho Brahe disagreed with both Ptolemy and Copernicus. • He hired Johannes Kepler to interpret his observations.

  49. Kepler’s Laws • Kepler’s 1st Law states that each planet’s orbit is an ellipse with the sun at one focus.

  50. Kepler’s Laws • Kepler’s 2nd Law states that the position vector of a planet travels through equal areas in equal times if the vector is drawn from the sun.

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