← All parts of this equation

Equation 4 · Part 3 · How We Know What Is Inside a Planet

Symbol R^2

C/MR2=0.353±0.017C/MR^{2} = 0.353 \pm 0.017
R2R^{2}

What this part means

The square of R: multiply R by itself.

Its job in the formula

R2R^2 is part of the quantity the equation computes from the expression on the right.

The passage around this formula

What a moment-of-inertia factor rules out is more reliable than what it establishes. It is a single number, so it cannot distinguish a small dense core under a light mantle from a larger, less dense core under a heavier one; infinitely many radial density profiles share the same I∗I^{*} . But it will refuse an entire class of models outright. For Mercury, MESSENGER radio tracking combined with spin measurements gave C/MR2R^{2} = 0.353 ±\pm 0.017 together with a ratio of mantle-plus-crust moment to total moment of 0.452 ±\pm 0.035 , a combination consistent with a solid silicate outer shell over an iron-sulfide layer, a liquid iron-rich outer core and possibly a solid inner core [ 7 ] . Seven years…

Read this part in the article →

Learn the underlying idea

An exponent tells how a base is used in multiplication. In x³, x is the base and 3 is the exponent: x³ = x × x × x.

Open the illustrated exponents: repeated multiplication and powers guide →

See this notation across published equations →

Sources cited in the surrounding passage

These citations provide research context; check each source for the exact claim it supports.