
In many gravitational problems, objects are treated as point masses.
However, real objects such as:
have mass distributed throughout a volume.
An extended body is an object whose size cannot be neglected.
To calculate its gravitational attraction, we must consider how the mass is distributed.
Fortunately, several important simplifications exist for spherically symmetric bodies.
Newton’s Law of Gravitation for two point masses is:
FG=Gm1m2r2F_G = \frac{Gm_1m_2}{r^2}FG=r2Gm1m2
where:
For extended objects, this equation is not always directly applicable.
An extended body is an object whose mass is distributed over a region of space rather than concentrated at a single point.
Examples include:
To determine the gravitational force, contributions from every small piece of mass must be added together.
An extended body can be divided into many tiny mass elements:
dmdmdm
Each mass element exerts a small gravitational force:
dF=Gm dmr2dF = \frac{Gm\,dm}{r^2}dF=r2Gmdm
The total force is obtained by integration:
F=∫dFF = \int dFF=∫dF
This calculus approach is the foundation of gravitational field calculations.
Many astronomical objects are approximately spherical.
Examples:
For these objects, a remarkable theorem greatly simplifies calculations.
For a spherically symmetric body:
This result is known as the Shell Theorem.
It was first demonstrated by Isaac Newton.
For a spherical object of mass MMM:
FG=GMmr2F_G = \frac{GMm}{r^2}FG=r2GMm
where:
This equation is exactly the same as the point-mass equation.
Outside a spherical body:
Sphere⟹Point Mass at Center\text{Sphere} \quad\Longrightarrow\quad \text{Point Mass at Center}Sphere⟹Point Mass at Center
This simplification is used extensively in AP Physics C.
Because the sphere behaves like a point mass:
g=GMr2g = \frac{GM}{r^2}g=r2GM
where:
This equation applies to:
At Earth’s surface:
r=REr=R_Er=RE
Thus:
g=GMERE2g = \frac{GM_E}{R_E^2}g=RE2GME
Substituting Earth’s values gives:
g≈9.8 m/s2g \approx 9.8\,m/s^2g≈9.8m/s2
At altitude hhh:
r=RE+hr=R_E+hr=RE+h
Therefore:
g=GME(RE+h)2g = \frac{GM_E}{(R_E+h)^2}g=(RE+h)2GME
As altitude increases:
g↓g\downarrowg↓
Gravity becomes weaker.
The Shell Theorem provides another remarkable result.
For a hollow spherical shell:
FG=0F_G=0FG=0
Every gravitational contribution is exactly canceled by contributions from other parts of the shell.
An object placed anywhere inside a hollow spherical shell experiences no net gravitational force.
Inside a hollow shell:
g=0g=0g=0
This result is independent of:
As long as the shell is spherically symmetric.
A uniform solid sphere behaves differently.
Only the mass enclosed within radius rrr contributes to the gravitational force.
The mass outside radius rrr produces no net force.
For a sphere of radius RRR and total mass MMM:
Mr=Mr3R3M_r = M\frac{r^3}{R^3}Mr=MR3r3
where:
Substituting the enclosed mass into Newton’s Law gives:
g=GMrr2g = \frac{GM_r}{r^2}g=r2GMr
Using:
Mr=Mr3R3M_r = M\frac{r^3}{R^3}Mr=MR3r3
yields:
g=GMrR3g = \frac{GMr}{R^3}g=R3GMr
Inside a uniform sphere:
g∝rg\propto rg∝r
The gravitational field increases linearly with distance from the center.
At the center:
r=0r=0r=0
Therefore:
g=0g=0g=0
The gravitational field vanishes at the exact center of a uniform sphere.
g∝rg\propto rg∝r
A straight-line increase.
g∝1r2g\propto \frac1{r^2}g∝r21
An inverse-square decrease.
Treat Earth as a point mass when studying satellites.
Model stellar gravity using the Shell Theorem.
Apply:
FG=GMmr2F_G = \frac{GMm}{r^2}FG=r2GMm
using the planet’s center as the source.
The Shell Theorem is fundamental in studying stars and galaxies.
Earth’s mass:
ME=5.97×1024 kgM_E = 5.97\times10^{24}\,kgME=5.97×1024kg
A satellite is located at:
r=2REr = 2R_Er=2RE
Find the gravitational field strength.
Using:
g=GME(2RE)2g = \frac{GM_E}{(2R_E)^2}g=(2RE)2GME g=14(GMERE2)g = \frac14 \left( \frac{GM_E}{R_E^2} \right)g=41(RE2GME) g=14(9.8)g = \frac14(9.8)g=41(9.8) g=2.45 m/s2g = 2.45\,m/s^2g=2.45m/s2
The field strength is one-fourth of its surface value.
Using the surface radius when the object is above Earth.
Always measure distance from the center.
Assuming gravity is zero outside Earth.
Gravity extends infinitely far from Earth.
Assuming all of a sphere’s mass contributes inside the sphere.
Only the enclosed mass contributes.
Outside a spherical body:
FG=GMmr2F_G = \frac{GMm}{r^2}FG=r2GMm g=GMr2g = \frac{GM}{r^2}g=r2GM
Inside a hollow shell:
FG=0F_G=0FG=0 g=0g=0g=0
Inside a uniform solid sphere:
g=GMrR3g = \frac{GMr}{R^3}g=R3GMr
Key ideas:
The study of gravitational attraction due to extended bodies provides the foundation for understanding planetary structure, satellite motion, stellar physics, and many advanced topics in AP Physics C Mechanics.
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