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That apparently is what palladin was saying, and it is a false argument.Rap said:I think what palladin was saying was that for a person below ground, there is some mass above them which pulls them upward, less mass below them to pull them downward, therefore they will weigh less, and that is a true and valid argument, which does not deny Gauss' theorem.
A correct statement is that at some depth below the surface of a spherical mass distribution, the spherical shell of mass above that depth contributes absolutely nothing to the gravitational force. The mass overhead does not pull them upward. All that matters is the sphere of below than the depth in question. In other words, with r=R-d, where R is the radius of the Earth and d is the depth below the surface,
[tex]g(r) = \frac{GM(r)}{r^2}[/tex]With this, and with a model of density inside the Earth such as the Preliminary Reference Earth Model (http://geophysics.ou.edu/solid_earth/prem.html ), one can investigate the behavior of g inside the Earth. Note that for a spherical mass distribution the derivative of mass wrt radial distance is related to the local density via
[tex]\frac{dM(r)}{dr} = 4\pi r^2 \rho(r)[/tex]
I'll define the mean density at some radial distance r from the center as
[tex]\bar{\rho}(r) \equiv \frac{M(r)}{V(r)} = \frac{M(r)}{4/3\pi r^3}[/tex]
With this, differentiating gravitational force respect to radial distance r yields
[tex]\aligned
\frac{dg(r)}{dr} &=
\frac{G dM/dr}{r^2} - 2\frac{GM(r)}{r^3}\\[6pt]
&= \frac{G 4\pi r^2 \rho(r)}{r^2} - 2\frac 4 3 \pi G \bar{\rho}(r)\\[6pt]
&= 4\pi G\left(\rho(r) - \frac 2 3 \bar{\rho}(r)\right)
\endaligned[/tex]
In words, gravitational force increases with depth if 2/3 of the mean density of the stuff at greater depths exceeds the local density at the depth in question, decreases otherwise. There are two points inside the Earth where marked changes in density makes the difference [itex]2/3 \bar{\rho}-\rho[/itex] change from positive to negative with increasing depth. The core-mantle boundary (the D" zone) marks the transition from the rocky material of the mantle to the molten iron of the outer core. In the transition zone at the top of the inner mantle, the mantle rock changes crystalline structure and hence changes density. (The point in the lower mantle where this density difference changes from negative to positive is of no special interest.)
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