Forest UCM RBM: Difference between revisions
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:<math>\vec L_{\mbox{tot}} = \vec L_{\mbox{orb}} + \vec L_{\mbox{spin}}</math> | :<math>\vec L_{\mbox{tot}} = \vec L_{\mbox{orb}} + \vec L_{\mbox{spin}}</math> | ||
;Precession of the Earth | |||
http://courses.physics.northwestern.edu/Phyx125/Precession%20of%20the%20Earth.pdf | |||
[[Forest_Ugrad_ClassicalMechanics#Rigid_Body_Motion]] | [[Forest_Ugrad_ClassicalMechanics#Rigid_Body_Motion]] | ||
Revision as of 13:31, 25 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
- [math]\displaystyle{ \vec R }[/math] point to the center of mass of the object
- [math]\displaystyle{ \vec {r}_k }[/math] points to a mass element [math]\displaystyle{ m_k }[/math]
- [math]\displaystyle{ \vec{r}_k^{\;\;\prime} }[/math] points from the center of mass to the mass element [math]\displaystyle{ m_k }[/math]
the angular momentum of mass element [math]\displaystyle{ m_k }[/math] about the point O is given as
- [math]\displaystyle{ \ell_k = \vec {r}_k \times \vec {p}_k = \vec {r}_k \times m \vec {\dot r}_k }[/math]
The total angular momentum about the point O is given as
- [math]\displaystyle{ \vec L = \sum \ell_k = \sum \vec {r}_k \times m_k \vec {\dot r}_k }[/math]
This can be cast in term of the angular momentum about the center of mass and the angular momentum of the motion
- [math]\displaystyle{ \vec {r}_k = \vec R + \vec{r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ \vec L = \sum \vec {r}_k \times m_k \vec {\dot r}_k }[/math]
- [math]\displaystyle{ = \sum (\vec R + \vec{r}_k^{\;\; \prime}) \times m_k (\vec \dot R + \vec{\dot r}_k^{\;\; \prime}) }[/math]
- [math]\displaystyle{ = \sum \vec R \times m_k \vec \dot R + \sum \vec R \times m_k \vec{\dot r}_k^{\;\; \prime} + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec \dot R +\sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\dot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ \sum \vec R \times m_k \vec \dot R = \vec R \times \sum m_k \vec \dot R = \vec R \times M \vec \dot R = \vec R \times \vec P }[/math]
- [math]\displaystyle{ \vec P = }[/math] momentum of the center of Mass
- [math]\displaystyle{ \sum \vec R \times m_k \vec{\dot r}_k^{\;\; \prime} = \vec R \times \sum m_k \vec{\dot r}_k^{\;\; \prime} 0 }[/math]
- [math]\displaystyle{ \sum m_k \vec{\dot r}_k^{\;\; \prime} = \sum m_k \left ( \vec {r}_k - \vec R\right ) = \sum m_k \vec {r}_k - \sum m_k \vec R = \vec {v}_{cm} - \vec{v}_{cm} = 0 }[/math]
- The location of the center of mass is at [math]\displaystyle{ \vec{ r}_k^{\;\; \prime} = 0 }[/math] the derivative is also zero
- [math]\displaystyle{ \sum m_k \vec{\dot r}_k^{\;\; \prime} = \sum m_k \left ( \vec {r}_k - \vec R\right ) = \sum m_k \vec {r}_k - \sum m_k \vec R = \vec {v}_{cm} - \vec{v}_{cm} = 0 }[/math]
- [math]\displaystyle{ \sum \vec{r}_k^{\;\; \prime} \times m_k \vec \dot R = \sum m_k \vec{r}_k^{\;\; \prime} \times \vec \dot R =0 }[/math] : The location of the CM is at 0
- [math]\displaystyle{ \vec L = \vec R \times \vec P + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\dot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ = L_{\mbox{CM}} + L_{\mbox{about CM}} }[/math]
The total angular momentum is the sum of the angular momentum of the center of mass of a rigid body [math]\displaystyle{ L_{\mbox{CM}} }[/math] and the angular momentum of the rigid body about the center of mass [math]\displaystyle{ L_{\mbox{about CM}} }[/math]
Planet example
What is the total angular momentum of the earth orbiting the sun?
There are two components
- [math]\displaystyle{ \vec L_{\mbox{CM}} }[/math] = angular momentum of the earth orbiting about the sun
- [math]\displaystyle{ \vec L_{\mbox{about CM}} }[/math] = angular momentum of the earth orbiting about the earth's center of mass (Spin)
- [math]\displaystyle{ \vec L_{\mbox{tot}} = \vec L_{\mbox{CM}} + \vec L_{\mbox{about CM}} }[/math]
- [math]\displaystyle{ \vec L_{\mbox{CM}} }[/math] is conserved and defined as Orbital angular momentum
- [math]\displaystyle{ \vec \dot L_{\mbox{CM}} = \vec \dot R \times \vec P + \vec R \times \vec \dot P }[/math]
- [math]\displaystyle{ \vec \dot R \times \vec P = \vec V \times M \vec V = 0 }[/math]
- [math]\displaystyle{ \Rightarrow \vec \dot L_{\mbox{orb}} = \vec R \times \vec \dot P=\vec R \times \vec {F}_{ext} }[/math]
If there is only a central force
- [math]\displaystyle{ \vec {F}(\mbox{ext}) = G \frac{Mm}{R^3} \vec R }[/math]
Then
- [math]\displaystyle{ \vec R \times \vec {F}(\mbox{ext}) = \vec R \times G \frac{Mm}{R^3} \vec R= G \frac{Mm}{R^3} \vec R \times \vec R =0 }[/math]
Thus
- [math]\displaystyle{ \vec \dot L_{\mbox{CM}} = \vec R \times \vec {F}(\mbox{ext}) = 0 }[/math]
- [math]\displaystyle{ \vec L_{\mbox{CM}} \equiv \vec L_{\mbox{Orb}} }[/math] = constant = Orbital angular momentum
The above is a good approximation even though the Sun's gravitational Field is not perfectly uniform
- How about [math]\displaystyle{ \vec L_{\mbox{about CM}} }[/math]?
Since
- [math]\displaystyle{ \vec L_{\mbox{tot}} = \sum \vec {r}_k \times m_k \vec {\dot r}_k =\vec L_{\mbox{Orb}} + \vec L_{\mbox{about CM}} }[/math]
as seen earlier
- [math]\displaystyle{ \vec L = \sum \vec {r}_k \times m_k \vec {\dot r}_k }[/math]
- [math]\displaystyle{ = \sum (\vec R + \vec{r}_k^{\;\; \prime}) \times m_k (\vec \dot R + \vec{\dot r}_k^{\;\; \prime}) }[/math]
- [math]\displaystyle{ = \vec R \times \vec P + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\dot r}_k^{\;\; \prime} }[/math]
Then
- [math]\displaystyle{ \dot \vec L = \vec \dot R \times \vec P +\vec R \times \vec \dot P + \sum \vec{\dot r}_k^{\;\; \prime} \times m_k \vec{\dot r}_k^{\;\; \prime} + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ =\vec R \times \vec \dot P + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ =\vec R \times \vec {F}(\mbox{ext}) + \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ =\vec{\dot{ L}}_{\mbox{Orv}} + \vec{\dot {L}}_{\mbox{about CM}} }[/math]
- [math]\displaystyle{ \Rightarrow \vec{\dot {L}}_{\mbox{about CM}} = \sum \vec{r}_k^{\;\; \prime} \times m_k \vec{\ddot r}_k^{\;\; \prime} }[/math]
- [math]\displaystyle{ \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]
The total angular momentum is the sum of the orbital angular momentum and the spin
- [math]\displaystyle{ \vec L_{\mbox{tot}} = \vec L_{\mbox{orb}} + \vec L_{\mbox{spin}} }[/math]
- Precession of the Earth
http://courses.physics.northwestern.edu/Phyx125/Precession%20of%20the%20Earth.pdf