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Gravitation flash cards

Master Gravitation through 94 JEE Advanced-level recall cards, systematically structured one idea at a time. Revise concept-wise, identify the areas where you need improvement, and focus your preparation with greater precision.

Gravitation, question and answer

17 of this chapter's 94 cards, laid out open so you can read straight through. The remaining 77 are in the interactive deck, where the answer stays hidden until you commit to one.

  1. 1.State Newton's law of universal gravitation.

    Every particle attracts every other particle with a force along the line joining them: F=Gm1m2r2F = \dfrac{Gm_1m_2}{r^2}, directed along the line of centres. It is always attractive and acts as an action–reaction pair.

    Hint: Force \propto product of masses, 1/r2\propto 1/r^2.

  2. 2.What is the value and SI unit of the universal gravitational constant GG?

    G=6.67×1011 N m2kg2G = 6.67\times10^{-11}\ \text{N m}^2\text{kg}^{-2}. It is a universal constant, independent of the medium and the nature of the masses.

    Hint: Same everywhere; dimension [M1L3T2][M^{-1}L^3T^{-2}].

  3. 3.Write the gravitational force in vector form between two masses.

    F21=Gm1m2r2r^21\vec{F}_{21} = -\dfrac{Gm_1m_2}{r^2}\,\hat{r}_{21}, where r^21\hat{r}_{21} points from 1 to 2. The minus sign shows the force is attractive (opposite to the position vector from the attracting mass).

    Hint: Minus sign = attraction.

  4. 4.Is the gravitational force a central force and is it conservative?

    Yes to both. It acts along the line joining the particles (central) and the work done is path-independent, depending only on endpoints (conservative), so a potential energy can be defined.

    Hint: Path-independent work \Rightarrow PE exists.

  5. 5.State the principle of superposition for gravitation.

    The net gravitational force on a particle is the vector sum of the forces due to all other particles taken one at a time: Fnet=iFi\vec{F}_{net} = \sum_i \vec{F}_i. Each pair interaction is unaffected by the presence of others.

    Hint: Vector-add pairwise forces.

  6. 6.How does a uniform spherical shell attract a mass outside and inside it?

    For a point outside, the shell attracts as if its whole mass were concentrated at its centre. For a point inside, the net gravitational force is zero everywhere.

    Hint: Outside: point mass at centre. Inside: zero.

  7. 7.What is acceleration due to gravity gg and its relation to GG, MM, RR?

    gg is the acceleration of a freely falling body near Earth's surface: g=GMR2g = \dfrac{GM}{R^2}, where MM and RR are Earth's mass and radius. Standard g9.8 m s2g \approx 9.8\ \text{m s}^{-2}.

    Hint: g=GM/R2g = GM/R^2.

  8. 8.How is gg related to the mean density ρ\rho of Earth?

    With M=43πR3ρM = \frac{4}{3}\pi R^3\rho,   g=GMR2=43πGRρ\;g = \dfrac{GM}{R^2} = \dfrac{4}{3}\pi G R\rho. So gRρg \propto R\rho for a uniform-density sphere.

    Hint: Substitute M=43πR3ρM=\frac43\pi R^3\rho.

  9. 9.How does gg vary with altitude hh above Earth's surface?

    gh=GM(R+h)2=g(1+hR)2g_h = \dfrac{GM}{(R+h)^2} = g\left(1+\dfrac{h}{R}\right)^{-2}. For hRh\ll R:   ghg(12hR)\;g_h \approx g\left(1-\dfrac{2h}{R}\right). Gravity decreases with height.

    Hint: Fractional drop 2h/R\approx 2h/R for small hh.

  10. 10.How does gg vary with depth dd below Earth's surface (uniform density)?

    gd=g(1dR)g_d = g\left(1-\dfrac{d}{R}\right). Only the mass of the inner sphere of radius (Rd)(R-d) contributes; the outer shell exerts zero net force. At the centre g=0g=0.

    Hint: gd=g(1d/R)g_d = g(1-d/R); centre 0\Rightarrow 0.

  11. 11.For small changes, which decreases gg faster — going up by hh or down by the same dd?

    Going up: gg decreases by fraction 2h/R\approx 2h/R. Going down: it decreases by fraction d/Rd/R. So for equal small distances, altitude reduces gg about twice as fast as depth.

    Hint: Altitude: 2h/R2h/R; depth: d/Rd/R.

  12. 12.Why does gg vary with latitude due to Earth's rotation?

    Rotation supplies part of gravity as centripetal force: gλ=gω2Rcos2λg_\lambda = g - \omega^2 R\cos^2\lambda, where λ\lambda is latitude. Effective gg is largest at the poles and smallest at the equator.

    Hint: gλ=gω2Rcos2λg_\lambda = g-\omega^2R\cos^2\lambda.

  13. 13.By how much is effective gg reduced at the equator due to rotation?

    At equator λ=0\lambda=0: reduction =ω2R0.034 m s2=\omega^2 R \approx 0.034\ \text{m s}^{-2}. At the poles (λ=90\lambda=90^\circ) there is no reduction, so gpole>gequatorg_{pole} > g_{equator}.

    Hint: Max effect at equator, zero at poles.

  14. 14.Besides rotation, why is true gg smaller at the equator than at the poles?

    Earth is an oblate spheroid: equatorial radius is larger than polar radius. Since g1/R2g\propto 1/R^2, the larger equatorial RR gives a smaller gg, adding to the rotational effect.

    Hint: Equatorial bulge \Rightarrow larger RR.

  15. 15.Define gravitational field intensity Eg\vec{E}_g at a point.

    It is the gravitational force per unit test mass placed at that point: Eg=Fm\vec{E}_g = \dfrac{\vec{F}}{m}. For a point mass MM: Eg=GMr2E_g = \dfrac{GM}{r^2}, directed toward MM. Units: N kg1\text{N kg}^{-1}.

    Hint: Force per unit mass; =g=g near Earth.

  16. 16.Define gravitational potential VV at a point.

    It is the work done by an external agent per unit mass in bringing a small mass from infinity to that point (without acceleration): V=WmV = \dfrac{W}{m}. For a point mass: V=GMrV = -\dfrac{GM}{r}. Units: J kg1\text{J kg}^{-1}.

    Hint: V=GM/rV=-GM/r; always negative, zero at infinity.

  17. 17.What is the relation between gravitational field and potential?

    The field is the negative gradient of potential: Eg=dVdrE_g = -\dfrac{dV}{dr}. The field points in the direction of decreasing potential.

    Hint: E=dV/drE=-dV/dr.

Open the interactive deck for the other 77 cards, with self-grading so the ones you keep missing come back.

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