Natko said:
Thanks for the quick reply!
Can you explain this in more understandable terms as I am only in Grade 9 please, especially what you mean by "gradient," "field," and the "1/r3 factor".
The Earth as a whole is accelerating toward the moon. This acceleration is given by
a_{\text{earth}} = \frac{GM_{\text{moon}}}{R^2}
where
G is the universal gravitational constant,
Mmoon, and
R is the distance between the center of the moon and the center of the earth. Now imagine a drop of water on the surface of the Earth directly on the line from the Earth to the moon. This drop of water is a bit closer to the moon than is the center of the earth. Denoting the radius of the Earth with a lower case
r, the distance between the drop and the moon is
R-r. This shorter distance means the drop experiences a slightly greater acceleration than does the Earth as a whole:
a_{\text{drop}} = \frac{GM_{\text{moon}}}{(R-r)^2}
Factoring
R out of
R-r yields R-r=R(1-r/R). Thus another way to write the acceleration of the drop is
a_{\text{drop}} = \frac{GM_{\text{moon}}}{R^2}\frac1{(1-r/R)^2}
The acceleration of the drop relative to the Earth as a whole is simply the difference between these:
\begin{aligned}<br />
a_{\text{rel}}<br />
&= \frac{GM_{\text{moon}}}{(R-r)^2} - \frac{GM_{\text{moon}}}{R^2} \\<br />
&= \frac{GM_{\text{moon}}}{R^2}\frac1{(1-r/R)^2}<br />
- \frac{GM_{\text{moon}}}{R^2} \\<br />
&= \frac{GM_{\text{moon}}}{R^2}\left(\frac1{(1-r/R)^2}-1\right)<br />
\end{aligned}
The first term in parentheses can be rewritten as
\frac1{(1-r/R)^2} =<br />
1+2\frac r R + 3\left(\frac r R\right)^2 + 4\left(\frac r R\right)^3 + \cdots
With this, the acceleration of the drop relative to the Earth becomes
\begin{aligned}<br />
a_{\text{rel}}<br />
&= \frac{GM_{\text{moon}}}{R^2}\left(\frac1{(1-r/R)^2}-1\right) \\<br />
&= \frac{GM_{\text{moon}}}{R^2}<br />
\left(2\frac r R + 3\left(\frac r R\right)^2 + 4\left(\frac r R\right)^3 + \cdots\right)<br />
\end{aligned}
Because the distance to the moon or the sun is much greater than the radius of the earth, the first term is going to be the dominant one. Thus
<br />
a_{\text{rel}} \approx \frac{GM_{\text{moon}}}{R^2} 2\frac r R<br />
= \frac{2GM_{\text{moon}}r}{R^3}<br />
So, 1/R
3. Substitute the moon for the sun and the same kind of inverse cube relation will hold.