Difference between revisions of "Forest UCM RBM"
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::<math>\Rightarrow \vec{\dot {L}}_{\mbox{about CM}} = \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} </math> | ::<math>\Rightarrow \vec{\dot {L}}_{\mbox{about CM}} = \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} </math> | ||
− | :<math> \vec{\dot {L}}_{\mbox{spin}}\equiv\vec{\dot {L}}_{\mbox{about CM}} = \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} \equiv \ | + | :<math> \vec{\dot {L}}_{\mbox{spin}}\equiv\vec{\dot {L}}_{\mbox{about CM}} = \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} \equiv \tau(\mbox{ext about CM}) </math> |
Revision as of 13:40, 24 November 2014
Rigid Body Motion
Rigid Body
- Rigidy Body
- A Rigid Body is a system involving a large number of point masses, called particles, whose distances between pairs of point particles remains constant even when the body is in motion or being acted upon by external force.
- Forces of Constraint
- The internal forces that maintain the constant distances between the different pairs of point masses.
Total Angular Momentum of a Rigid Body
Consider a rigid body that rotates about a fixed z-axis with the origin at point O.
INSERT PICTURE HERE
let
- point to the center of mass of the object
- points to a mass element
- points from the center of mass to the mass element
the angular momentum of mass element
about the point O is given asThe total angular momentum about the point O is given as
This can be cast in term of the angular momentum about the center of mass and the angular momentum of the motion
- momentum of the center of Mass
- The location of the center of mass is at the derivative is also zero
- : The location of the CM is at 0
The total angular momentum is the sum of the angular momentum of the center of mass of a rigid body
and the angular momentum of the rigid body about the center of massPlanet example
What is the total angular momentum of the earth orbiting the sun?
There are two components
- = angular momentum of the earth orbiting about the sun
- = angular momentum of the earth orbiting about the earth's center of mass (Spin)
- is conserved and defined as Orbital angular momentum
If there is only a central force
Then
Thus
- = constant = Orbital angular momentum
The above is a good approximation even though the Sun's gravitational Field is not perfectly uniform
- How about ?
Since
as seen earlier
Then