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Where Earth and Moon Pulls Cancel

Irodov 1.231DifficultyDifficulty 2 of 5UniquenessUniqueness 2 of 5

Problem Irodov 1.231

The Earth (mass M1M_1) and the Moon (mass M2M_2) are separated, center to center, by nRnR, where n=60n=60 and RR is the Earth’s own radius. The Earth’s mass is η=81\eta=81 times the Moon’s, M1=ηM2M_1=\eta M_2. Find the distance rr from the Moon’s center at which the resultant of the Earth’s and the Moon’s gravitational field strengths is zero.

The Earth (left, mass M_1) and the Moon (right, mass M_2), not to scale, their centers a distance nR apart.

The Earth (left, mass M1M_1) and the Moon (right, mass M2M_2), not to scale, their centers a distance nRnR apart.

Given
  • η=81\eta=81
  • n=60n=60
  • RR
Find
rr

Solution

Step 1Equal and opposite field strengths
The balance point P on the line of centers, a distance r from the Moon's center within the separation nR. The pull F_1 toward the Earth and the pull F_2 toward the Moon are drawn equal in length.

The balance point PP on the line of centers, a distance rr from the Moon’s center within the separation nRnR. The pull F1F_1 toward the Earth and the pull F2F_2 toward the Moon are drawn equal in length.

At the sought point PP, distance rr from the Moon’s center and nR−rnR-r from the Earth’s center, the two field strengths are equal in magnitude; writing each as γM/(distance)2\gamma M/(\text{distance})^2 and using M1=ηM2M_1=\eta M_2 eliminates both masses in favor of the ratio η\eta.

γM1(nR−r)2=γM2r2(nR−rr)2=M1M2\begin{align*}\frac{\gamma M_1}{(nR-r)^2} &= \frac{\gamma M_2}{r^2} \\ \left(\frac{nR-r}{r}\right)^2 &= \frac{M_1}{M_2}\end{align*}
(nR−rr)2=η\left(\frac{nR-r}{r}\right)^2=\eta
(1)
Step 2Solve for rr, then substitute the numbers

Taking the positive square root, since nR−rnR-r and rr are both lengths, turns the balance condition (1) into a linear equation for rr.

η=nR−rrrη=nR−rr(1+η)=nR\begin{align*}\sqrt\eta &= \frac{nR-r}{r} \\ r\sqrt\eta &= nR-r \\ r\left(1+\sqrt\eta\right) &= nR\end{align*}

With η=81\eta=81, η=9\sqrt\eta=9, so rr is one tenth of the full separation nRnR; substituting the Earth’s radius RR from the standard table gives the numeric distance.

r=6R=3.82×107 mr=6R=3.82\times10^7\ \text{m}
r=nR1+η≈3.8×104 kmr=\frac{nR}{1+\sqrt\eta}\approx3.8\times10^4\ \text{km}
(2)
Check

As a limiting case, equal masses (η=1\eta=1) give r=nR/2r=nR/2, the midpoint of the separation, exactly as symmetry demands. Dimensionally rr is nRnR divided by a pure number, so it is a length, as required.

Remark

Because the divisor is 1+η1+\sqrt\eta rather than 1+η1+\eta, the balance point sits far farther from the Moon than dividing by 1+η1+\eta would place it: that alternative divisor gives r=nR/82=4.66×106 mr=nR/82=4.66\times10^6\ \text{m}, eight times closer to the Moon than the true r=nR/10=3.82×107 mr=nR/10=3.82\times10^7\ \text{m}, so taking the square root of the mass ratio, rather than the ratio itself, pushes the null point much farther out toward the heavier body. As η→∞\eta\to\infty the divisor grows only as η\sqrt\eta, so r→0r\to0 and the point closes in on the lighter body’s own center rather than receding without bound, a general feature of this balance for any two-body mass ratio (for a real, finite-sized Moon the point instead reaches the surface once η\eta is large enough, and then ceases to exist, rather than migrating into the interior).