College Physics
College Physics
11th Edition
ISBN: 9781305952300
Author: Raymond A. Serway, Chris Vuille
Publisher: Cengage Learning
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2. We can use a simple model which uses our
understanding of uniform circular motion to
estimate the largest possible rotational speed of a
planet around its own axis. For a planet of mass M
and radius R our model assumes that the planet
"falls apart" when the loose rocks on the surface at
the equator are no longer sitting on the surface
because they leave the surface. A loose rock of mass
m is shown on the equator in the drawing.
M
m
R
С.
Now return to the 'slowly' rotating planet (where
the loose rocks are not flying off the surface) and consider a
loose rock that is not on the equator, but at some higher
latitude, 0 (as shown). Do you need forces besides gravity and
the normal force to make this situation possible? Justify your
answer (you just need to justify whether you need another
force but not what that other force might be if it is needed).
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Transcribed Image Text:2. We can use a simple model which uses our understanding of uniform circular motion to estimate the largest possible rotational speed of a planet around its own axis. For a planet of mass M and radius R our model assumes that the planet "falls apart" when the loose rocks on the surface at the equator are no longer sitting on the surface because they leave the surface. A loose rock of mass m is shown on the equator in the drawing. M m R С. Now return to the 'slowly' rotating planet (where the loose rocks are not flying off the surface) and consider a loose rock that is not on the equator, but at some higher latitude, 0 (as shown). Do you need forces besides gravity and the normal force to make this situation possible? Justify your answer (you just need to justify whether you need another force but not what that other force might be if it is needed).
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