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NCERT Exemplar · Q3

Q.Different points in earth are at slightly different distances from the sun and hence experience different forces due to gravitation. For a rigid body, we know that if various forces act at various points in it, the resultant motion is as if a net force acts on the c.m. (centre of mass) causing translation and a net torque at the c.m. causing rotation around an axis through the c.m. For the earth-sun system (approximating the earth as a uniform density sphere)

(a) the torque is zero.
(b) the torque causes the earth to spin.
(c) the rigid body result is not applicable since the earth is not even approximately a rigid body.
(d) the torque causes the earth to move around the sun.
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The gravitational force from the Sun varies across Earth's diameter, but because Earth is spherically symmetric the net torque about Earth's center of mass is zero; the tidal force gradient does not produce rotation of Earth around its own axis or orbital motion—those have independent causes.

Why the torque vanishes: the Equivalence Principle and spherical symmetry

The Sun pulls harder on the near side of Earth than the far side because gravity weakens with distance. You might think this differential force—called a tidal force—would twist Earth, producing a torque about its center of mass. But torque depends not just on force magnitude but on where the force acts and in what direction.

For a spherically symmetric body like Earth (approximated as uniform density), every mass element on the near hemisphere has a partner on the far hemisphere arranged symmetrically about the center. The Sun's force on the near side is stronger and points slightly inward; the force on the far side is weaker and points slightly outward. When you sum the torques from all these pairs about Earth's center of mass, the angular contributions cancel exactly. The net effect is a stretching along the Earth–Sun line (the tidal bulge) but no net torque about the center.

This is a beautiful consequence of spherical symmetry: the gradient of a central force field (the Sun's gravity) produces no torque on a spherically symmetric mass distribution about its own center.


Step-by-step reasoning

  1. Set up the problem. Earth is a sphere of radius RR centered at position rCM\mathbf{r}_{\text{CM}} relative to the Sun. A small mass element dmdm at position r\mathbf{r} experiences gravitational force

dF=−GM⊙ dm∣r−r⊙∣3(r−r⊙),d\mathbf{F} = -\frac{GM_{\odot} \, dm}{|\mathbf{r} - \mathbf{r}_{\odot}|^3} (\mathbf{r} - \mathbf{r}_{\odot}),

where r⊙\mathbf{r}_{\odot} is the Sun's position. The distance ∣r−r⊙∣|\mathbf{r} - \mathbf{r}_{\odot}| varies across Earth's diameter by roughly 2R≈1.3×104 km2R \approx 1.3 \times 10^4 \, \text{km}, a tiny fraction of the Earth–Sun distance d≈1.5×108 kmd \approx 1.5 \times 10^8 \, \text{km}.

  1. Expand the force in a Taylor series. Because R≪dR \ll d, write r=rCM+δ\mathbf{r} = \mathbf{r}_{\text{CM}} + \boldsymbol{\delta} where ∣δ∣≤R|\boldsymbol{\delta}| \leq R. Expanding the gravitational force to first order in δ/d\boldsymbol{\delta}/d gives

dF≈−GM⊙ dmd2d^+(tidal terms),d\mathbf{F} \approx -\frac{GM_{\odot} \, dm}{d^2} \hat{\mathbf{d}} + \text{(tidal terms)},

where d^\hat{\mathbf{d}} points from Earth's center toward the Sun. The leading term is the same for every dmdm; integrating over Earth's mass MM yields the familiar orbital force Fnet=−GM⊙M/d2 d^\mathbf{F}_{\text{net}} = -GM_{\odot}M/d^2 \, \hat{\mathbf{d}} acting at the center of mass.

  1. Compute the torque about the center of mass. The torque on element dmdm is

dτ=δ×dF.d\boldsymbol{\tau} = \boldsymbol{\delta} \times d\mathbf{F}.

The uniform part of dFd\mathbf{F} (the orbital force) contributes

∫δ×(−GM⊙ dmd2d^)=−GM⊙d2d^×∫δ dm=0,\int \boldsymbol{\delta} \times \left(-\frac{GM_{\odot} \, dm}{d^2} \hat{\mathbf{d}}\right) = -\frac{GM_{\odot}}{d^2} \hat{\mathbf{d}} \times \int \boldsymbol{\delta} \, dm = \mathbf{0},

because ∫δ dm=0\int \boldsymbol{\delta} \, dm = \mathbf{0} by definition of the center of mass.

  1. What about the tidal (gradient) terms? The next-order terms in the expansion are proportional to δ\boldsymbol{\delta} and produce the tidal force. For a spherically symmetric mass distribution, the integral

∫δ×(tidal force on dm)\int \boldsymbol{\delta} \times (\text{tidal force on } dm)

also vanishes. Physically, for every element at +δ+\boldsymbol{\delta} there is a symmetric partner at −δ-\boldsymbol{\delta} (or more generally, the angular average over the sphere is zero), so the torques cancel in pairs.

  1. Interpret the options.
    • (A) The torque is zero. ✓ This is correct.
    • (B) The torque causes Earth to spin. ✗ Earth's rotation (its day) is a relic of the angular momentum from the solar nebula; the Sun's tidal torque on a perfectly spherical Earth is zero. (Real tidal torques arise from Earth's equatorial bulge and the Moon, gradually slowing Earth's spin.)
    • (C) Rigid-body result not applicable. ✗ Earth is elastic and deforms under tidal stress, but the center-of-mass theorem and torque calculation for external forces apply perfectly well to any body, rigid or deformable.
    • (D) The torque causes Earth to move around the Sun. ✗ Orbital motion is caused by the net force (which acts at the c.m. and produces centripetal acceleration), not by torque. Torque would cause rotation about the c.m., not translation.
Tip

Tidal forces stretch a body along the line joining the two masses (creating ocean tides) but produce no net torque on a sphere. Torques appear only when the body is asymmetric (e.g., the Moon's torque on Earth's equatorial bulge causes precession).

Watch out

Do not confuse the force gradient (which is nonzero and causes tides) with torque (which is zero for a symmetric body). Also, orbital motion is due to the net force, not torque—torque rotates a body about its own axis, force translates the center of mass.

✓Final answer

The correct option is (A): the torque is zero.

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