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Some Gravity Notes

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distler Administator 20 posts

As we said in class, the acceleration due to gravity, near the Earth’s surface, is

(1)gGM ER E 2g \equiv \frac{G M_E}{R_E^2}

The gravitational potential energy

(2)U grav(r)=GM Emr=GM EmR E+yU_{\text{grav}}(r) = - \frac{G M_E m}{r} = - \frac{G M_E m}{R_E + y}

where we’ve written r=R E+y and y is the height above the Earth’s surface. For yR E, we can approximate this by a power series in y.

If you know Taylor series, you can compute it directly. If not, consider writing

1R E+y=?1R E(1+a 1(yR E)+a 2(yR E) 2+a 3(yR E) 3+)\frac{1}{R_E + y} \overset{?}{=} \frac{1}{R_E} \left(1+ a_1{\left(\tfrac{y}{R_E}\right)}+ a_2 {\left(\tfrac{y}{R_E}\right)}^2 + a_3 {\left(\tfrac{y}{R_E}\right)}^3+\dots\right)

for some choice of constants, a 1,a 2,a 3,. If we multiply by (R E+y), we should get 1:

1 (R E+y)1R E(1+a 1(yR E)+a 2(yR E) 2+a 3(yR E) 3+) =1+(1+a 1)(yR E)+(a 1+a 2)(yR E) 2+(a 2+a 3)(yR E) 3+\begin{split} 1&\equiv (R_E +y) \frac{1}{R_E} \left(1+ a_1{\left(\tfrac{y}{R_E}\right)}+ a_2 {\left(\tfrac{y}{R_E}\right)}^2 + a_3 {\left(\tfrac{y}{R_E}\right)}^3+\dots\right) \\ & = 1 + (1+a_1) {\left(\tfrac{y}{R_E}\right)} + (a_1+a_2) {\left(\tfrac{y}{R_E}\right)}^2 + (a_2+a_3) {\left(\tfrac{y}{R_E}\right)}^3 +\dots \end{split}

So, to make the equation true, we must have

a 1=1,a 2=1,a 3=1,a_1 = -1,\quad a_2 = 1,\quad a_3 = -1,\dots

So (2) can be approximated

U grav(R E+y) =GM ER E(1(yR E)+(yR E) 2) =GM ER E+mgymgy 2R E+\begin{split} U_{\text{grav}}(R_E+y) &= -\frac{G M_E}{R_E}\left(1 -{\left(\tfrac{y}{R_E}\right)} + {\left(\tfrac{y}{R_E}\right)}^2 -\dots\right)\\ &= - \frac{G M_E}{R_E} + m g y - m g \tfrac{y^2}{R_E} + \dots \end{split}

The first term is an irrelevant constant. The second is the gravitational potential energy we wrote down before, and the third term is the first correction, due to the fact that the gravitational force, due to the Earth, falls off with distance (rather than being constant).

 
distler Administator 20 posts

In class, we considered only the case where one of the masses is much greater than the other, Mm, and so is more-or-less stationary. What happens when that isn’t the case?

Let’s consider the extreme opposite situtation, namely two equal masses, m, in a circular orbit about the midpoint between them.

Layer 1 midpoint R R R R

The distance between them is r=2R, so the force on the first one is

F 1=Gm 2(2R) 2F_1 = \frac{G m^2}{{(2R)}^2}

(and, similarly, for F 2). So, for a circular orbit, we have

v 2R=1mF 1=Gm4R 2\frac{v^2}{R} = \frac{1}{m}{F_1} = \frac{G m}{4 R^2}

or

v 2=Gm4Rv^2 = \frac{G m}{4 R}

To compute the period, T=2πRv, we get something that looks just like Kepler’s 3rd Law.

T 2=const.R 3=16π 2GmR 3T^2 = \text{const} .\, R^3 = \frac{16\pi^2}{G m} R^3

but the constant is 4 times as big as before.

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