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Exercises · 7.13

Q.How will you 'weigh the sun', that is estimate its mass? The mean orbital radius of the earth around the sun is 1.5×108 km1.5 \times 10^{8}\text{ km}.

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We use Kepler’s Third Law in Newton’s form: the orbital period and radius of Earth give the Sun’s mass directly. The result is M⊙≈2.0×1030 kgM_\odot \approx 2.0 \times 10^{30}\ \text{kg}.

The idea is beautifully simple. Earth orbits the Sun because of gravity. If we know how far away Earth is and how long it takes to go around once, Newton’s law of gravitation and circular motion let us solve for the Sun’s mass. No need to visit the Sun — just use the orbit.

Kepler’s Third Law originally said “the square of the period is proportional to the cube of the semi-major axis.” Newton later gave it physical meaning: the constant of proportionality involves the mass of the central body. For a planet orbiting a much heavier star, the law becomes:

T2=4π2GM⊙a3T^2 = \frac{4\pi^2}{GM_\odot} a^3

where TT is the orbital period, aa is the mean orbital radius (semi-major axis), GG is the gravitational constant, and M⊙M_\odot is the Sun’s mass. Rearranging gives M⊙=4π2a3GT2M_\odot = \frac{4\pi^2 a^3}{G T^2}.

Let’s plug in the numbers step by step.

  1. Get the data in consistent units. The mean orbital radius is given as a=1.5×108 kma = 1.5 \times 10^8\ \text{km}. Convert to metres:

a=1.5×108×103=1.5×1011 m.a = 1.5 \times 10^8 \times 10^3 = 1.5 \times 10^{11}\ \text{m}.

Earth’s orbital period is one year. In seconds:

T=1 year=365.25×24×3600≈3.156×107 s.T = 1\ \text{year} = 365.25 \times 24 \times 3600 \approx 3.156 \times 10^7\ \text{s}.

(We use 365.25 days to account for the leap-year cycle — it’s precise enough.)

  1. Recall the gravitational constant.

G=6.67×10−11 N⋅m2/kg2.G = 6.67 \times 10^{-11}\ \text{N·m}^2/\text{kg}^2.

  1. Compute a3a^3.

a3=(1.5×1011)3=3.375×1033 m3.a^3 = (1.5 \times 10^{11})^3 = 3.375 \times 10^{33}\ \text{m}^3.

  1. Compute T2T^2.

T2=(3.156×107)2≈9.96×1014 s2.T^2 = (3.156 \times 10^7)^2 \approx 9.96 \times 10^{14}\ \text{s}^2.

  1. Plug into the formula.

M⊙=4π2×3.375×10336.67×10−11×9.96×1014.M_\odot = \frac{4\pi^2 \times 3.375 \times 10^{33}}{6.67 \times 10^{-11} \times 9.96 \times 10^{14}}.

First, the numerator: 4π2≈39.484\pi^2 \approx 39.48, so

39.48×3.375×1033≈1.332×1035.39.48 \times 3.375 \times 10^{33} \approx 1.332 \times 10^{35}. …

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