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Natural Science Forum / Physics / Relativity / December 2006



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Graviational potential inside the Earth

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karandash2000@yahoo.com - 27 Dec 2006 23:57 GMT
Wolfram used to have the general formula for the gravitational
potential inside the Erath at an arbitrary depth d from the surface.
(NOT the potential of the shell but of the filled sphere).
Anybody that has it at his fingertips?
Pmb - 28 Dec 2006 00:03 GMT
> Wolfram used to have the general formula for the gravitational
> potential inside the Erath at an arbitrary depth d from the surface.
> (NOT the potential of the shell but of the filled sphere).
> Anybody that has it at his fingertips?

Are you thinking of the Earh as being a solid sphere of uniform mass
density? If so then the relationship is linear and can easily be decuded by
Gauss' law.

Mass density = rho = M/V => M = rho*V

Integral g*dA = G*M = G*rho*V = G*rho*(4*pi*r^3/3)

g(4*pi*r^2) = G*rho*(4*pi*r^3/3)

g = (G*rho*/3)r

You'd better double check this in case I screwed up the units.

Best wishes

Pete
Pmb - 28 Dec 2006 00:06 GMT
>> Wolfram used to have the general formula for the gravitational
>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 18 lines]
>
> Pete

Oops! That was for acceleration, not potential. The force is given by

F = mg = m(G*rho*/3)r = -grad U

U = -m(G*rho*/3)

Hmmm. A constant potential? That doesn't seem quite right. What did I do
wrong folks?

Pete
Pmb - 28 Dec 2006 00:10 GMT
>>> Wolfram used to have the general formula for the gravitational
>>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 27 lines]
> Hmmm. A constant potential? That doesn't seem quite right. What did I do
> wrong folks?

Okay. I got it

U = -(1/2)m(G*rho*/3)r^2
karandash2000@yahoo.com - 28 Dec 2006 00:25 GMT
> >>> Wolfram used to have the general formula for the gravitational
> >>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 31 lines]
>
> U = -(1/2)m(G*rho*/3)r^2

Thank you, Pete, the units don't seem right (the presence of r^2)
Pmb - 28 Dec 2006 00:44 GMT
>> >>> Wolfram used to have the general formula for the gravitational
>> >>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 35 lines]
>
> Thank you, Pete, the units don't seem right (the presence of r^2)

You're right. I think that the constant of proportionality in Gausses law
that I used has to be wrong. To find that constant consider a point charge
at the origin and chose the Gaussian surface as a sphere centered at the
origin.

Pete
karandash2000@yahoo.com - 28 Dec 2006 00:50 GMT
> >> >>> Wolfram used to have the general formula for the gravitational
> >> >>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 42 lines]
>
> Pete

I found something close, done for shell:
http://hep.ph.liv.ac.uk/~green/mechanics/lectures/l15notes.pdf

The same formalism should apply to non-shell but the integral needs to
change from a surface (double) integral to a volume (triple) integral.
I did it years ago , I was just hoping that someone has the results at
his fingertips. Dang, Wolfram took his reference down, U don't know why.
karandash2000@yahoo.com - 28 Dec 2006 00:59 GMT
> >>> Wolfram used to have the general formula for the gravitational
> >>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 31 lines]
>
> U = -(1/2)m(G*rho*/3)r^2

I think I found the correct solution:
http://www.madsci.org/posts/archives/2002-01/1011285522.Ph.r.html
John C. Polasek - 28 Dec 2006 03:54 GMT
>> >>> Wolfram used to have the general formula for the gravitational
>> >>> potential inside the Erath at an arbitrary depth d from the surface.
[quoted text clipped - 34 lines]
>I think I found the correct solution:
>http://www.madsci.org/posts/archives/2002-01/1011285522.Ph.r.html
For a uniform density the solution is very simple inside the earth:
    g(r) = g0*r/R
where r is distance from center of the earth of radius R and g0 is
surface gravity. It linearly increases from the center.
The shell theorem shows that it.s only the mass beneath you that
counts. So g is proportional to r^3/r^2 = r
Mass = k* R^3, and the usual 1/r^2.
John Polasek
Tom Roberts - 29 Dec 2006 02:08 GMT
> For a uniform density the solution is very simple inside the earth:
>     g(r) = g0*r/R
> where r is distance from center of the earth of radius R and g0 is
> surface gravity. It linearly increases from the center.

This is quite clearly wrong. The potential at the center must be much
less than the potential at infinity, where it is zero, and less than at
the surface. But this is correct for the Newtonian gravitational force,
so you were presumably answering a different question.

Koobee Wublee wrote:
> **  U c^2 = 2 G M / R - G M r^2 / R^3   In matter
> **  U c^2 = G M / r                     Free space

This has the correct limiting behavior, at both r=0 and r=R, but is
wrong by numerical factors. The sign is also wrong -- gravitational
potential is NEGATIVE near a massive body, and zero at infinity. The c^2
is also omitted in conventional units (c never appears in Newtonian
mechanics).

The correct answer is:

   phi(r) = - (G M / R) (3/2 - (1/2) r^2 / R^2)    for r<=R
          =  - G M / r                             for r>=R

> Force = m c^2 del U

In conventional units there is no c^2, and there must be a minus sign
(objects get pushed from regions of higher potential energy to regions
with lower potential energy).

> At the center of earth, the gravitational potential is the highest.
> Notice I choose to define gravitational potential as positive.

You think that objects fall up???
Or perhaps energy is not conserved???

> Credit should go to Dr. Roberts.

I don't remember it.... And I doubt I would have made those elementary
errors. I certainly would not have made the sign errors, as the signs
are of fundamental importance.

Tom Roberts
karandash2000@yahoo.com - 29 Dec 2006 02:18 GMT
> > For a uniform density the solution is very simple inside the earth:
> >     g(r) = g0*r/R
[quoted text clipped - 40 lines]
>
> Tom Roberts

Thank you, Tom
Appreciate it.
Koobee Wublee - 29 Dec 2006 07:16 GMT
> The correct answer is:
>
>     phi(r) = - (G M / R) (3/2 - (1/2) r^2 / R^2)    for r<=R
>            =  - G M / r                             for r>=R

Thanks for the correction.

> > Force = m c^2 del U
>
> In conventional units there is no c^2,

There is no conventional agreement.  I have clearly implied the
following.

**  U = G M / r / c^2, for r >= R

> and there must be a minus sign
> (objects get pushed from regions of higher potential energy to regions
> with lower potential energy).

Since there are no such separate quantities as the kinetic energy and
the potential energy, I can choose to define them as positive or
negative.  As long as I am consistent and make it very clear to others
readers.  You need to read more carefully what I wrote.

> > At the center of earth, the gravitational potential is the highest.
> > Notice I choose to define gravitational potential as positive.
>
> You think that objects fall up???

No.  What gives you that idea?

> Or perhaps energy is not conserved???

Conservation of energy is a universal, fundamental phenomenon.  It even
applies to spacetime in general in which GR is just a special case of.
<shrug>
Koobee Wublee - 28 Dec 2006 05:13 GMT
> Are you thinking of the Earh as being a solid sphere of uniform mass
> density? If so then the relationship is linear and can easily be decuded by
[quoted text clipped - 9 lines]
>
> You'd better double check this in case I screwed up the units.

So, Gauss' law fails you, eh?  Welcome to the real world.  Try

**  U c^2 = 2 G M / R - G M r^2 / R^3     In matter
**  U c^2 = G M / r                                   Free space

Force = m c^2 delU

At the center of earth, the gravitational potential is the highest.
Notice I choose to define gravitational potential as positive.

Credit should go to Dr. Roberts.
John C. Polasek - 28 Dec 2006 16:54 GMT
>> Are you thinking of the Earh as being a solid sphere of uniform mass
>> density? If so then the relationship is linear and can easily be decuded by
[quoted text clipped - 21 lines]
>
>Credit should go to Dr. Roberts.

The problem is complicated by the fact that you must specify potential
DIFFERENCE. If m falls from infinity, then U is negative as the mass
absorbs energy on its way to the surface under inverse square force.
If computed from the center of the earth, U is positive: energy is put
into the mass to raise it, now with a force proportional to radius.
The negative U achieved at the surface is further increased on its
passage down a hole to the center.

del U is already force. U is already potential. What is the mc^2 for?

John Polasek
 
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