Before you can read $r_{SOI} \approx R(m/M)^{2/5}$, you must already be fluent in a dozen tiny ideas that the parent note quietly assumed. Here we earn each one — plain words first, a picture second, and a "why the topic needs it" third.
The picture: a big heavy ball and a small light ball. Gravity does not care about colour or shape — only this one number.
Why the topic needs it: the entire SOI formula is driven by the ratiom/M — "how the planet's stuff compares to the Sun's stuff." Everything else is geometry.
The picture: the Sun far away on the left, the planet on the right, and a tiny spacecraft buzzing right next to the planet. R is the long line; r is the short line.
Why the topic needs it: because r≪R, we are allowed to approximate — to treat the spacecraft as sitting at roughly the same distance from the Sun as the planet does. That approximation is what makes the maths solvable at all.
G ::: the same tiny constant everywhere in the universe, 6.674×10−11 in SI units. It just sets the strength scale.
M (top) ::: bigger puller ⟹ stronger pull. Doubling M doubles a.
d2 (bottom) ::: inverse-square. Go twice as far and the pull is not half but a quarter.
Why "per unit mass"? Because gravity accelerates every kilogram the same amount, we drop the spacecraft's own mass entirely and speak of accelerationa (units of m/s²), not force. This is why the parent note writes FA=Gm/r2 with no spacecraft mass in it — it is really an acceleration.
The parent note suddenly writes dRd(R21). Here is that symbol, from zero.
The one rule we need — the power rule — says: to differentiate Rn, bring the power down front and lower it by one:
dRdRn=nRn−1
Apply it to R21=R−2:
dRdR−2=−2R−3=−R32
The minus sign says "the pull weakens as you move outward." The size is R32 — and that factor 2 is exactly where the dropped (1/2)1/5 in the final formula comes from.
The picture: the Sun tugs the spacecraft's "near side" a hair harder than its "far side." Both the planet and the craft are falling toward the Sun together, so the common fall cancels out — only the leftover difference perturbs the planet-centred orbit.
Why the topic needs it: this is the crux the Tidal Forces page expands. The Sun's disturbing action in the planet-centred view is
PA≈dRd(R2GM)r=R32GMr,
a tidal term ∝r/R3 — not the full GM/R2 force. Miss this and you get the wrong exponent.
Read top to bottom: masses give the ratio; distances plus the inverse-square law give both the main force and (via the derivative) the tidal term; comparing the two ratios yields the boundary; the ratio m/M raised to 2/5 gives the radius.