|
Shoemaker-Levy Comet Fragment 9 impacting Jupiter July 22 1994 |
|
Jupiter, showing the impact marks from fragments of Comet Shoemaker-Levy 9 in July 1994 |
Because [gravity] will act to pull meteors, comets, and other space debris toward a planet, the effective cross-section for a planet to capture an object is larger than its geometrical cross-section. What is the size of this effective cross-section in terms of the physical qualities of the planet and the situation? What features of the impacting body is it independent of?
Solution
System:
Interactions:
Model:
Approach:
Diagrammatic Representation
The Force Diagram of the Meteor approaching the Planet
Force Diagram of Meteor and Planet |
The [single-axis torque] about the center of the planet is zero, because the force of [gravity] acts along the same direction as the radius r. About this point, therefore, [angular momentum] is conserved.
Sketch showing Torque |
Mathematical Representation
We begin by recognizing that both Energy and Angular Momentum (about the planet's center) are conserved. Some of the object's potential Energy_ is transformed into Kinetic Energy, but none is lost. And since there is no torque when the Angular Momentum is calculated about the center of the planet, the angular momentum must be conserved as well. (Both of these statements would not be true if some nonconservative, dissipative force was present, but we are assuming motion through empty space, and a fall onto a surface with no atmosphere.)We write the conditions for the initial state (when the mass is very far from the planet) with subscript i and for the final state (when the mass comes down and just grazes the planet tangentially) by the subscript f.
\begin
[ \vec
= \vec
X \vec
= rF = I_
\alpha ]\end
\begin
[ I_
= I_
+ I_
]\end
\begin
[ I = \frac
m r^2 ] \end
\begin
[ I_
= \frac
(m r^2 + M R^2 ) ]\end
\begin
[ \omega_
= \omega_
+ \alpha (t_
- t_
) ] \end
\begin
[ \theta_
= \theta_
+ \omega_
( t_
- t_
) + \frac
\alpha ( t_
- t_
)^2 ]\end
\begin
[ \omega_
= \alpha t_
]\end
\begin
[ \theta_
= \frac
\alpha {t_{\rm f}}^2 ]\end
where
\begin
[ \alpha = \frac
{I_{\rm total}} = \frac
]\end