In this section we shall do the usual example of free-fall motion but the distinction will be the use of spherical co-ordinates to ease the use of mental geometric gymnastics and also a classical introduction to Larmor precession will be introduced. Because the earth is for the most part a sphere, spherical co-ordinates should be used with only very minor modifications. Gravity points in the -\(\hat{r}\) direction the \(\hat{\theta}\) is going from north pole to south pole and \(\hat{\phi}\) is going along a latitude. Ultimately we want to describe the motion as a function of latitude so the simple transformation of \(\frac{\pi}{2}- \theta = \lambda\) will be introduced ; \(\lambda\) is the latitude defined as being zero at the equator and goes to \(45^{\circ}\) in either direction.
First a note on unit vectors:
The \(\hat{r}\) is the one commonly introduced in text books and is reproduced below along with \(\hat{\theta}\) and \(\hat{\phi}\)
\begin{equation}
\hat{r}= \cos \phi \sin \theta \hat{x}+ \sin\phi \sin \theta \hat{y} + \cos \theta \hat{z}\\
\hat{\theta}= \cos \phi \cos \theta \hat{x}+ \sin\phi \cos \theta \hat{y} - \sin \theta \hat{z}\\
\hat{\phi}= -\sin \theta \hat{x}+ \cos \theta \hat{y}
\end{equation}
From these three equations one can easily find the inverse transformations that give \(\hat{x}\), \(\hat{y}\) and \(\hat{z}\) in terms of the spherical unit vectors in this manner. To find what \(\hat{x}\) is simply collect the terms next to the \(\hat{x}\) in the above equations and group them together.
So \(\hat{x} = \cos \phi \sin \theta \hat{r} + \cos \phi \cos \theta \hat{\theta} -\sin \theta \hat{\phi}\). Same applies for the rest.
Also, if you know what the \(\hat{r }\) unit vector looks like in Cartesian unit vectors then \( \hat{\theta} \)is not very far away. First note that it is perpendicular to the \(\hat{r}\) unit vector and therefore while we had to project the \(\hat{r}\) onto the x-y axis by taking the \(\sin \theta \) in order to project the \(\hat{\theta}\) we use \(\cos \theta\). Since \(\hat{\theta}\) is going in the -\(\hat{z}\) direction we take the -\(\sin \theta\) .
So why is all this important? Well, our \(\Omega\) or angular velocity will be in the \(\hat{z}\) direction and we will need to put it into spherical unit vectors. But from the above discussion, rather than playing with right triangles and twisting and contorting your head in unseemly manners. Simply collect the \(\hat{z}\) in the \(\hat{r}\) and \(\hat{\theta}\) equations. So we have the following:
\begin{equation}
\mathbf{\Omega \hat{z}} = \Omega \cos \theta \hat{r} - \Omega \sin \theta \hat{\theta}
\end{equation}
Imagine if you were on a test, you just saved yourself five minutes of agony. Now since \(\hat{\theta}\) moves in the -\(\hat{z}\) we will need to re-write \(\mathbf{\Omega}\) in the following manner:
\begin{equation}
\mathbf{\Omega \hat{z}} = \Omega \cos \theta \hat{r} + \Omega \sin \theta \hat{\theta}
\end{equation}
Also because we will put the origin at the surface of the earth and not the center we shall use the effective gravitational acceleration that already includes the effects of the centrifugal force. Thus our expression for equation of motion will have no expression involving position and we will not have to bite our lips for this time-saving step.
Finally we come to the general equation of motion:
\begin{equation}
F_{rot} = mg_{eff}+ F_{cor}\\
F_{rot} = mg_{eff} + v_{rot} \times 2\Omega
\end{equation}
In the above expressions the subscript "rot" stands for rotational reference frame. Next we take the determinant to get the expression below:
\begin{equation}
v \times \mathbf{\Omega} = \hat{r} \left(v_{\phi}\Omega \sin \theta \right) + \hat{\theta}\left(v_{\phi}\Omega \cos \theta \right) + \hat{\phi}\left( v_{r}\Omega \sin \theta - v_{\theta}\Omega \cos \theta \right)
\end{equation}
We know have our equations of motion:
\begin{equation}
\ddot{r} = v_{\phi} \Omega \sin \theta - g_{eff} \\
\ddot{\theta} = v_{\phi}\Omega \cos \theta \\
\ddot{\phi} = \left( v_{r} \Omega \sin \theta - v_{\phi} \Omega \cos \theta \right)
\end{equation}
The procedure of getting the solution is by using a bit of perturbation theory. First solve the equations by assuming \(\Omega\) is zero to get the following equations:
\begin{equation}
\theta = 0\\
\phi = 0 \\
r = h - \frac{g t^2}{2}\\
v_{\theta} = 0\\
v_{\phi} = 0\\
v_{r} = -gt
\end{equation}
Next assume that the angular velocity is non-zero but very small so that our zero order approximation are fairly accurate enough and plug the results in the equations of motions. The only equation that survives is \(\ddot{\phi} = -gt \Omega \sin \theta\). This gives the deviation in the \hat{\phi} direction. To get how this deviation varies according to latitudes simply put in the transformation mentioned at the beginning of this section.
The next example introduces the phenomenon of Larmor precession. Imagine a negative electric charge q is moving in an elliptical orbit about a positive charge q. What are the equations of motion in the rotating reference frame?
\begin{equation}
F_{rot} = 2m\left(v_{rot} \times \Omega \right) + q\left(v_{rot} + \Omega \times r \right) \times \vec{B} + \left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r} \\
F_{rot} = 2m\left(v_{rot} \times \Omega \right) + qv_{rot} \times \vec{B} + q\left(\Omega \times r \right) \times \vec{B}+ \left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r}\\
F_{rot} = v_{rot} \times \left(2m \Omega - q\vec{B}\right) - q\left(\Omega \times r \right) \times \vec{B}+\left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r}
\end{equation}
Now in order not to have linear velocity in the rotating reference frame the first term in the last equation has to disappear and therefore \Omega has to be \(\frac{qB}{2m}\). This is the Larmor frequency at which the precession occurs. The particle has no translational velocity. We are then left with the following expression:
\begin{equation}
F_{rot} = -\frac{q^2}{2m}\left(\vec{B} \times r \right) \times \vec{B} + \frac{q^2}{2m}\left(\vec{B}\times r \right) \times \vec{B} - \frac{q^2}{4\pi \epsilon r^2} \hat{r}
\end{equation}
First a note on unit vectors:
The \(\hat{r}\) is the one commonly introduced in text books and is reproduced below along with \(\hat{\theta}\) and \(\hat{\phi}\)
\begin{equation}
\hat{r}= \cos \phi \sin \theta \hat{x}+ \sin\phi \sin \theta \hat{y} + \cos \theta \hat{z}\\
\hat{\theta}= \cos \phi \cos \theta \hat{x}+ \sin\phi \cos \theta \hat{y} - \sin \theta \hat{z}\\
\hat{\phi}= -\sin \theta \hat{x}+ \cos \theta \hat{y}
\end{equation}
From these three equations one can easily find the inverse transformations that give \(\hat{x}\), \(\hat{y}\) and \(\hat{z}\) in terms of the spherical unit vectors in this manner. To find what \(\hat{x}\) is simply collect the terms next to the \(\hat{x}\) in the above equations and group them together.
So \(\hat{x} = \cos \phi \sin \theta \hat{r} + \cos \phi \cos \theta \hat{\theta} -\sin \theta \hat{\phi}\). Same applies for the rest.
Also, if you know what the \(\hat{r }\) unit vector looks like in Cartesian unit vectors then \( \hat{\theta} \)is not very far away. First note that it is perpendicular to the \(\hat{r}\) unit vector and therefore while we had to project the \(\hat{r}\) onto the x-y axis by taking the \(\sin \theta \) in order to project the \(\hat{\theta}\) we use \(\cos \theta\). Since \(\hat{\theta}\) is going in the -\(\hat{z}\) direction we take the -\(\sin \theta\) .
So why is all this important? Well, our \(\Omega\) or angular velocity will be in the \(\hat{z}\) direction and we will need to put it into spherical unit vectors. But from the above discussion, rather than playing with right triangles and twisting and contorting your head in unseemly manners. Simply collect the \(\hat{z}\) in the \(\hat{r}\) and \(\hat{\theta}\) equations. So we have the following:
\begin{equation}
\mathbf{\Omega \hat{z}} = \Omega \cos \theta \hat{r} - \Omega \sin \theta \hat{\theta}
\end{equation}
Imagine if you were on a test, you just saved yourself five minutes of agony. Now since \(\hat{\theta}\) moves in the -\(\hat{z}\) we will need to re-write \(\mathbf{\Omega}\) in the following manner:
\begin{equation}
\mathbf{\Omega \hat{z}} = \Omega \cos \theta \hat{r} + \Omega \sin \theta \hat{\theta}
\end{equation}
Also because we will put the origin at the surface of the earth and not the center we shall use the effective gravitational acceleration that already includes the effects of the centrifugal force. Thus our expression for equation of motion will have no expression involving position and we will not have to bite our lips for this time-saving step.
Finally we come to the general equation of motion:
\begin{equation}
F_{rot} = mg_{eff}+ F_{cor}\\
F_{rot} = mg_{eff} + v_{rot} \times 2\Omega
\end{equation}
In the above expressions the subscript "rot" stands for rotational reference frame. Next we take the determinant to get the expression below:
\begin{equation}
v \times \mathbf{\Omega} = \hat{r} \left(v_{\phi}\Omega \sin \theta \right) + \hat{\theta}\left(v_{\phi}\Omega \cos \theta \right) + \hat{\phi}\left( v_{r}\Omega \sin \theta - v_{\theta}\Omega \cos \theta \right)
\end{equation}
We know have our equations of motion:
\begin{equation}
\ddot{r} = v_{\phi} \Omega \sin \theta - g_{eff} \\
\ddot{\theta} = v_{\phi}\Omega \cos \theta \\
\ddot{\phi} = \left( v_{r} \Omega \sin \theta - v_{\phi} \Omega \cos \theta \right)
\end{equation}
The procedure of getting the solution is by using a bit of perturbation theory. First solve the equations by assuming \(\Omega\) is zero to get the following equations:
\begin{equation}
\theta = 0\\
\phi = 0 \\
r = h - \frac{g t^2}{2}\\
v_{\theta} = 0\\
v_{\phi} = 0\\
v_{r} = -gt
\end{equation}
Next assume that the angular velocity is non-zero but very small so that our zero order approximation are fairly accurate enough and plug the results in the equations of motions. The only equation that survives is \(\ddot{\phi} = -gt \Omega \sin \theta\). This gives the deviation in the \hat{\phi} direction. To get how this deviation varies according to latitudes simply put in the transformation mentioned at the beginning of this section.
The next example introduces the phenomenon of Larmor precession. Imagine a negative electric charge q is moving in an elliptical orbit about a positive charge q. What are the equations of motion in the rotating reference frame?
\begin{equation}
F_{rot} = 2m\left(v_{rot} \times \Omega \right) + q\left(v_{rot} + \Omega \times r \right) \times \vec{B} + \left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r} \\
F_{rot} = 2m\left(v_{rot} \times \Omega \right) + qv_{rot} \times \vec{B} + q\left(\Omega \times r \right) \times \vec{B}+ \left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r}\\
F_{rot} = v_{rot} \times \left(2m \Omega - q\vec{B}\right) - q\left(\Omega \times r \right) \times \vec{B}+\left(\Omega \times r \right) \times \Omega + \frac{q^2}{4\pi \epsilon r^2} \hat{r}
\end{equation}
Now in order not to have linear velocity in the rotating reference frame the first term in the last equation has to disappear and therefore \Omega has to be \(\frac{qB}{2m}\). This is the Larmor frequency at which the precession occurs. The particle has no translational velocity. We are then left with the following expression:
\begin{equation}
F_{rot} = -\frac{q^2}{2m}\left(\vec{B} \times r \right) \times \vec{B} + \frac{q^2}{2m}\left(\vec{B}\times r \right) \times \vec{B} - \frac{q^2}{4\pi \epsilon r^2} \hat{r}
\end{equation}