Phy 211: General Physics I Chapter 4: Motion in 2 & 3 Dimensions Lecture Notes.

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Presentation transcript:

Phy 211: General Physics I Chapter 4: Motion in 2 & 3 Dimensions Lecture Notes

2-Dimensional Motion A motion that is not along a straight line is a two- or three-dimensional motion. The position, displacement, velocity and acceleration vectors are not necessarily along the same directions; the rules for vector addition and subtraction apply The instantaneous velocity vector ( ) is always tangent to the trajectory but the average velocity ( ) is always in the direction of The instantaneous acceleration vector ( ) is always tangent to the slope of the velocity at each instant in time but the average acceleration ( ) is always in the direction of r B (t 1 ) r A (t 0 ) v(t)

Example of 2-D Motion

Displacement, Velocity & Accelerations When considering motion problems in 2-D, the definitions for the motion vectors described in Chapter 2 still apply. However, it is useful to break problems into two 1-D problems, usually –Horizontal (x) –Vertical (y) Displacement: Velocity: Acceleration: Use basic trigonometry relations to obtain vertical & horizontal components for all vectors

When t o = 0 and a is constant: Remember: when t o ≠0, t replaces  t in the above equations In Vector Notation: Equations of Kinematics in 2-D Horizontal: 1.v x - v ox = a x t 2.x - x o = ½ (v ox + v x )t 3.x - x o = v ox t + ½ a x t 2 4.v x 2 - v ox 2 = 2a x  x Vertical: 1.v y - v oy = a y t 2.y - y o = ½ (v oy + v y )t 3.y - y o = v oy t + ½ a y t 2 4.v y 2 - v oy 2 = 2a y  y

Projectile Motion Notes Projectile Motion is the classic 2-D motion problem: 1.Vertical motion is treated the same as free-fall  a y = - g = m/s 2 {downward} 2.Horizontal motion is independent of vertical motion but connected by time but no acceleration vector in horizontal direction  a x = 0 m/s 2 3.As with Free Fall Motion, air resistance is neglected

Projectile Motion Notes (cont.)

Uniform Circular Motion 1.Object travels in a circular path 2.Radius of motion (r) is constant 3.Speed (v) is constant 4.Velocity changes as object continually changes direction 5.Since v is changing (v is not but direction is), the object must be accelerated: 6.The direction of the acceleration vector is always toward the center of the circular motion is referred to as the centripetal acceleration 7.The magnitude of centripetal acceleration: v r

Derivation of Centrifugal Acceleration Consider an object in uniform circular motion, where: r = constant {radius of travel} v = constant {speed of object} The magnitude of the centripetal acceleration ( ) can be obtained by applying the Pythagorean theorem: The components of the velocity vector continuous change as the objects travels around the circle and are related to the angle,  : x v r y  x y