Chapter 6: Uniform Circular Motion and Gravitation
Rotation Angle and Angular Velocity
Rotation Angle (): The angle of rotation defined by the ratio of arc length () to the radius of curvature ():

Angular Velocity:
Tangential Velocity (): The linear speed tangent to the circular path relates to angular velocity () and radius () by:
, ( radians)
= period = time for one revolution to pass
Centripetal Acceleration and Centripetal Force
Centripetal Acceleration (): Radial acceleration pointing directly toward the center of curvature caused by a change in velocity direction:
Uniform Circular Motion = an object moves in a circle at a constant speed
Centripetal Force ( ): Any net force perpendicular to velocity that directs an object toward the center of curvature:
Unbanked turn with friction:
Steps to derive
1) Frictional force = and Centripetal Force are set equal in order to maintain circular motion
2) Use N = w = mg
3) Cancel m from both sides, simplify , so
Banked turn with no friction
Steps to derive
1) set Fnet(y) = 0, so - w = 0
2) Using trig angle (adjacent), = Ncos Ncos - w = 0
3) Ncos = w Ncos = mg
4) set Fnet(x) = m, since Fnet only force nin x direction is normal force = m
5) Use =
6) Using trig angle (opposite), = Nsin Nsin =
7) plug in and simplify to , so
Unbanked (Level) Curves: Static friction () between the tires and the roadway supplies the necessary centripetal force:
Banked Curves: The normal force () is tilted at an angle () relative to the vertical to provide centripetal force without relying on friction:
X direction:
Y direction:

Newton’s Universal Law of Gravitation
Universal Gravitation Law: Every mass attracts every other mass along a line intersecting their centers of mass ( ):
G = gravitational constant,
m1,m2 = two masses
r = radius
R is distance between their centers of mass
Surface Gravity: For objects near Earth's surface, the distance separating their centers of mass is approximated by Earth's radius ().
Earth-Moon System: Earth and the Moon revolve around their common center of mass once per month, producing detectable orbital "wiggles" in Earth's elliptical path around the Sun.
Tidal Dynamics: The gravitational differential exerted across Earth creates two high and two low ocean tides per day as Earth rotates under the tidal bulge
For the planet that feels the acceleration:
relative gravity =