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The scientists
on the far-away planet of Zakron 5 have discovered that their planet’s orbit
will decay, causing it to fall into and be incinerated by its sun. The data
shows that the inhabitants only have approximately 10 million years left. The
alarmed Zakronians look for a new planet, but there are none available that are
big enough to accommodate their vast population. In desperation, they turn to
you, a young Earth scientist. You tell them about a theoretical planet design
you have read about. It would involve building concentric circles of rock
around a star to form a CD shaped planet, perfect for habitation.

The Zakronians
are overjoyed by your suggestion and plan to begin construction right away.
They decide to use rock from a nearby asteroid belt with an average density of
5,000 kg/m3. However, they want to know how thick to build the disc
so that the acceleration due to gravity for the majority of the planet
(anywhere not too close to the inner or outer edge) will be 7 m/s2.
What is your answer?
According to Newton’s law of universal gravitation, the
force of gravity one mass exerts on another mass is:
F= (Gm1m2/D2)
Where G is the universal gravitational constant and D is the
distance between the centers of mass.
In this case:
Force on person (or Zakronian) = Gmpersonmrock/D2
Newton’s second law of motion, åF = ma, reduces the
above expression by canceling mperson when converting to
acceleration. Therefore:
Acceleration due to gravity = Gmrock/D2

In order to integrate the planet, it is easiest to think of
it as a series of concentric rings about the subject. When we integrate each
ring, the vectors pulling horizontally will cancel each other out, leaving our
vertical gravity vector. Since the planet is huge, these rings go on
effectively into infinity, but as the rings get farther and farther away, their
potency decreases very rapidly (for reasons to be seen later). Each of these
rings is made up of wedges that can be integrated easily using polar
coordinates.

The area from a function to the origin in polar coordinates:
The area of each wedge, dA, is equal to the linear measure
of the arc, Rdq,
times dR. Therefore:
dA = R dq dr
A = R dr dq
A = ½R2 dq
This is the fundamental integral for polar coordinates.
(Incidentally, by plugging r = R, 0 = a, 2p = b, this integral proves that the area of a circle with radius
r does indeed have an area of pr2)
All we need, however, is the volume of each ring, dV. That
is:
2pTRdR
The total acceleration vector for each ring is, as given
above, Gm/D2. Since the mass of each ring is just dVr (where r is the density,
5,000 kg/m3):
dP = 2pGTrRdR/D2
R
However, the actual
pull of gravity, dZ, is only the y-component of dP. Fortunately, a relationship
between dP, dZ, D, and T can be found with a little geometry:
.5T Z
D
From similar triangles, it can be said that:
(dP/dZ) = (2D/T)
dP = 2dZD/T
When we plug this back into our equation, it yields:
2dZD/T = 2pTqGRdR/D2
Or:
dZ = pqT2GRdR/D3
Since D, as observable from the side view, is just (R2
/ .25T2)½:
dZ = pqT2GRdR(R2 + .25T2)(-3/2)
We can now (finally!) do the integral. As noted above, the
planet is so huge compared to the subject standing on it that the upper limit
is infinity.
Z = pqGT2R(R2
+ .25T2)(-3/2) dR
If u is defined as (R2 + .25T2), we
can substitute:
Z = pqGT2 u(-3/2)
½ du
(This is because du = 2RdR and therefore ½du = RdR)
Z = ½pqGT2 [-2u-½]
When we substitute back:
Z = ½pqGT2 [-2(R2 + .25T2)-½]
Plugging infinity in for R (fortunately for us) returns 0.
Therefore:
Z = ½pqGT2 (-(-2(.25T2)-½))
Z = pqGT2 ((.25T2)-½)
Z = pqGT2 ((.25T2)-½)
Z = 2pqGT
ASTOUDING! A messy, complicated integral reduces to a
simple, linear relationship between the thickness of the planet and it
gravitation! Once the calculus is over with, answering the Zakronians proves
easier than first expected:
7 = 2p(5,000)(6.67259 e-11)T
T = 7/(2.096e-6)
T = 3,339,287
km
The fact that we were integrated out to infinity did not
matter because the gravitation pull of each ring got successive smaller and
smaller. The reason for this is twofold. First, the rings were getting farther
and farther away from the subject and gravity varies inversely as the square of
the distance. Secondly, since the rings were moving farther out horizontally,
the vertical component of each successive ring got small very quickly.
This problem has parallels to the "real" world. An
electron near a positively charged plate effectively "thinks" that
the plate goes on forever.