Quick Recap — Gravitation Basics

  • Universal law: F=Gm1m2r2F = \dfrac{Gm_1 m_2}{r^2}, with G=6.67×1011G = 6.67\times10^{-11} N m2^2/kg2^2 — the force is always attractive.
  • Acceleration due to gravity: g=GMR29.8g = \dfrac{GM}{R^2} \approx 9.8 m/s2^2 at Earth's surface.
  • Escape velocity: ve=2gR=2GMR11.2v_e = \sqrt{2gR} = \sqrt{\dfrac{2GM}{R}} \approx 11.2 km/s for Earth.
  • Kepler's laws: orbits are ellipses; equal areas are swept in equal times (angular momentum); and T2r3T^2 \propto r^3.
  • Gravity is a conservative force; gg is greatest at the poles and zero at the Earth's centre.

Beyond-NCERT JEE Formulae

Consolidated, exam-ready results that go past the plain NCERT statements — each tagged with when to use it and the trap examiners like to set.

1. Variation of gg (three regimes)

  • Small height (hRh\ll R): gh=g(12hR)g_h=g\left(1-\dfrac{2h}{R}\right) — a linear approximation; use for mountain- or aircraft-scale heights.
  • Any height: gh=g(RR+h)2g_h=g\left(\dfrac{R}{R+h}\right)^2 — the exact inverse-square in distance from the centre; use when hh is comparable with RR.
  • Depth: gd=g(1dR)g_d=g\left(1-\dfrac{d}{R}\right) — falls linearly to zero at the centre of a uniform Earth.
  • Latitude: gλ=gω2Rcos2λg_\lambda=g-\omega^2R\cos^2\lambda — the spin cuts gg most at the equator (λ=0\lambda=0) and not at all at the poles.

[JEE Tip] Height weakens gg TWICE as fast as depth: compare the factor 2hR\dfrac{2h}{R} against dR\dfrac{d}{R}. So the depth matching a small height hh is d=2hd=2h.

2. Gravitational field EE and potential VV

Outside any spherical body, or for a point mass (rRr\ge R): E=GMr2,V=GMrE=\dfrac{GM}{r^2},\qquad V=-\dfrac{GM}{r}

  • Solid sphere, inside (r<Rr<R): field E=GMrR3E=\dfrac{GMr}{R^3} grows linearly, while V=GM(3R2r2)2R3V=-\dfrac{GM\left(3R^2-r^2\right)}{2R^3}; at the centre Vc=3GM2RV_c=-\dfrac{3GM}{2R}.
  • Thin shell, inside (r<Rr<R): field E=0E=0, yet the potential stays flat at V=GMRV=-\dfrac{GM}{R} (its surface value).
  • Ring, on the axis at distance xx: field E=GMx(R2+x2)3/2E=\dfrac{GMx}{\left(R^2+x^2\right)^{3/2}} points along the axis, with V=GMR2+x2V=-\dfrac{GM}{\sqrt{R^2+x^2}}.

[JEE Tip] Field is a VECTOR (resolve and add components); potential is a SCALAR (add signed values, ignore direction). Inside a shell E=0E=0 but V0V\ne0 — a null field never forces a null potential. The two are linked by E=dVdrE=-\dfrac{dV}{dr}.

3. Escape and orbital speed

  • Escape speed: ve=2gR=2GMRv_e=\sqrt{2gR}=\sqrt{\dfrac{2GM}{R}} — independent of the body's mass and of the launch angle, since energy is a scalar.
  • Orbital speed at radius rr: vo=GMrv_o=\sqrt{\dfrac{GM}{r}}; skimming the surface this is vo=gRv_o=\sqrt{gR}.
  • Master link: ve=2vov_e=\sqrt2\,v_o — escaping needs only about 41 percent more speed than circling.

[JEE Tip] When the mass is missing but the density ρ\rho is given, switch to ve=R8πGρ3v_e=R\sqrt{\dfrac{8\pi G\rho}{3}} and g=43πGρRg=\dfrac{4}{3}\pi G\rho R — both follow from M=43πR3ρM=\dfrac{4}{3}\pi R^3\rho.

4. Energy of a satellite (circular orbit, radius rr)

KE=GMm2r,PE=GMmr,E=GMm2rKE=\dfrac{GMm}{2r},\qquad PE=-\dfrac{GMm}{r},\qquad E=-\dfrac{GMm}{2r}

  • The signs lock into a fixed pattern: KE=EKE=-E together with PE=2E=2KEPE=2E=-2\,KE.
  • Binding energy — the least energy to send it from the orbit to rest at infinity — equals GMm2r\dfrac{GMm}{2r}; every BOUND orbit has E<0E<0.
  • To break free FROM the orbit, raise the speed by the factor 2\sqrt2, that is Δv=(21)vo\Delta v=\left(\sqrt2-1\right)v_o.

[JEE Tip] A satellite dragged by the thin upper atmosphere actually SPEEDS UP: as rr shrinks, KE=GMm2rKE=\dfrac{GMm}{2r} rises. The energy lost to friction is drawn out of the deeper potential well.

5. Kepler's third law and the geostationary orbit

  • T2=4π2GMr3T^2=\dfrac{4\pi^2}{GM}\,r^3, so T2r3T^2\propto r^3 for one central body; inverted, rT2/3r\propto T^{2/3}.
  • A grazing circular orbit depends on density alone: T=3πGρT=\sqrt{\dfrac{3\pi}{G\rho}} (about 84 min at Earth's density, whatever the planet's size).
  • Geostationary satellite: a period of 24 h fixes r4.2×104r\approx4.2\times10^4 km (roughly 36000 km of height); it must ride over the EQUATOR moving west to east.

[JEE Tip] For a two-body BINARY the law is set by the SUM of the masses: T=2πd3G(m1+m2)T=2\pi\sqrt{\dfrac{d^3}{G\left(m_1+m_2\right)}} — never by one star alone.

Solved Examples — Beyond-NCERT Formulae

Example 1 — Same offset, up versus down. A planet has surface gravity gg. Find the acceleration due to gravity at a height h=R2h=\dfrac{R}{2} and at a depth d=R2d=\dfrac{R}{2}, and say which is larger.

  • Height (exact law): gh=g(RR+h)2=g(R3R/2)2=g(23)2=4g90.444gg_h=g\left(\dfrac{R}{R+h}\right)^2=g\left(\dfrac{R}{3R/2}\right)^2=g\left(\dfrac{2}{3}\right)^2=\dfrac{4g}{9}\approx0.444g.
  • Depth (linear law): gd=g(1dR)=g(112)=g2=0.5gg_d=g\left(1-\dfrac{d}{R}\right)=g\left(1-\dfrac{1}{2}\right)=\dfrac{g}{2}=0.5g.

Answer: gh=4g90.44gg_h=\dfrac{4g}{9}\approx0.44g while gd=0.5gg_d=0.5g, so gravity survives BETTER going down. Beware — the small-height rule g(12hR)g\left(1-\dfrac{2h}{R}\right) does not apply here, because hh is not small compared with RR.

Example 2 — Orbital versus escape speed. A moon has g=8g=8 m/s2^2 at its surface and radius R=4000R=4000 km. Find the speed of a surface-skimming satellite and the escape speed.

  • Orbital: vo=gR=(8)(4×106)=3.2×107=5.66×103v_o=\sqrt{gR}=\sqrt{(8)\left(4\times10^{6}\right)}=\sqrt{3.2\times10^{7}}=5.66\times10^{3} m/s.
  • Escape: ve=2vo=2gR=6.4×107=8.0×103v_e=\sqrt{2}\,v_o=\sqrt{2gR}=\sqrt{6.4\times10^{7}}=8.0\times10^{3} m/s.

Answer: vo5.66v_o\approx5.66 km/s and ve8.0v_e\approx8.0 km/s, standing in the ratio 1:21:\sqrt2. Writing 2gR\sqrt{2gR} for the orbital speed is the classic slip — that expression is the escape speed, larger by 2\sqrt2.

Example 3 — Total energy and period of a satellite. A satellite of mass m=200m=200 kg orbits the Earth at radius r=3Rr=3R, with g=9.8g=9.8 m/s2^2 and R=6400R=6400 km. Find its total mechanical energy and its orbital period.

  • Work with GM=gR2=(9.8)(6.4×106)2=4.01×1014GM=gR^2=(9.8)\left(6.4\times10^{6}\right)^2=4.01\times10^{14} in SI units, and r=3R=1.92×107r=3R=1.92\times10^{7} m.
  • Energy: E=GMm2r=(4.01×1014)(200)2(1.92×107)=2.09×109E=-\dfrac{GMm}{2r}=-\dfrac{\left(4.01\times10^{14}\right)(200)}{2\left(1.92\times10^{7}\right)}=-2.09\times10^{9} J.
  • Period: T=2πr3GM=2π(1.92×107)34.01×1014=2π(4199)=2.64×104T=2\pi\sqrt{\dfrac{r^3}{GM}}=2\pi\sqrt{\dfrac{\left(1.92\times10^{7}\right)^3}{4.01\times10^{14}}}=2\pi(4199)=2.64\times10^{4} s.

Answer: E2.09×109E\approx-2.09\times10^{9} J, negative as any bound orbit must be, and T2.64×104T\approx2.64\times10^{4} s, about 7.3 h. Quoting the potential energy GMmr-\dfrac{GMm}{r} alone would double the magnitude of the energy.

Example 4 — Kepler ratio. Two satellites circle the same planet with orbital radii in the ratio 1:91:9. Find the ratio of their periods.

  • Kepler's third law gives Tr3/2T\propto r^{3/2}, so T2T1=(r2r1)3/2\dfrac{T_2}{T_1}=\left(\dfrac{r_2}{r_1}\right)^{3/2}.
  • Substituting the radius ratio: T2T1=93/2=(91/2)3=33=27\dfrac{T_2}{T_1}=9^{3/2}=\left(9^{1/2}\right)^3=3^3=27.

Answer: the periods are in the ratio 1:271:27. Taking TrT\propto r would wrongly give 1:91:9; the exponent is 32\dfrac{3}{2}, not 11.

Example 5 — Field and potential of a solid sphere. For a uniform solid sphere of mass MM and radius RR, find the field and the potential at an inside point r=R2r=\dfrac{R}{2} and at an outside point r=2Rr=2R.

  • Inside (r=R2r=\tfrac R2): field E=GMrR3=GM(R/2)R3=GM2R2E=\dfrac{GMr}{R^3}=\dfrac{GM\left(R/2\right)}{R^3}=\dfrac{GM}{2R^2}, and V=GM(3R2r2)2R3=GM(3R2R2/4)2R3=11GM8RV=-\dfrac{GM\left(3R^2-r^2\right)}{2R^3}=-\dfrac{GM\left(3R^2-R^2/4\right)}{2R^3}=-\dfrac{11GM}{8R}.
  • Outside (r=2Rr=2R): field E=GMr2=GM4R2E=\dfrac{GM}{r^2}=\dfrac{GM}{4R^2}, and V=GMr=GM2RV=-\dfrac{GM}{r}=-\dfrac{GM}{2R}.

Answer: inside, E=GM2R2E=\dfrac{GM}{2R^2} with V=11GM8RV=-\dfrac{11GM}{8R}; outside, E=GM4R2E=\dfrac{GM}{4R^2} with V=GM2RV=-\dfrac{GM}{2R}. Note the potential is deepest at the CENTRE, where it is 3GM2R-\dfrac{3GM}{2R}, not at the surface.

Example 6 — Radius of a geostationary orbit. A satellite is to hover above one point on the equator, so its period is T=24T=24 h. Taking g=9.8g=9.8 m/s2^2 and R=6400R=6400 km, find its orbital radius.

  • Rearrange Kepler's law for the radius: r3=GMT24π2r^3=\dfrac{GM\,T^2}{4\pi^2}, with GM=gR2=4.01×1014GM=gR^2=4.01\times10^{14} and T=86400T=86400 s.
  • Compute: r3=(4.01×1014)(86400)24π2=7.59×1022r^3=\dfrac{\left(4.01\times10^{14}\right)\left(86400\right)^2}{4\pi^2}=7.59\times10^{22}, so r=(7.59×1022)1/3=4.23×107r=\left(7.59\times10^{22}\right)^{1/3}=4.23\times10^{7} m.

Answer: r4.23×104r\approx4.23\times10^{4} km from the Earth's centre, a height of about 36000 km. The famous 36000 km figure is the ALTITUDE; the orbital radius, measured from the centre, is one Earth radius more.

Example 7 — Binding energy and boosting an orbit. A satellite of mass m=100m=100 kg orbits the Earth at radius 2R2R, with g=9.8g=9.8 m/s2^2 and R=6400R=6400 km. Find (a) its binding energy and (b) the extra energy needed to lift it to a circular orbit of radius 3R3R.

  • Binding energy at 2R2R: GMm2(2R)=gR2m4R=mgR4=(100)(9.8)(6.4×106)4=1.57×109\dfrac{GMm}{2(2R)}=\dfrac{gR^2m}{4R}=\dfrac{mgR}{4}=\dfrac{(100)(9.8)\left(6.4\times10^{6}\right)}{4}=1.57\times10^{9} J.
  • Raising 2R3R2R\to3R: ΔE=(GMm6R)(GMm4R)=GMm12R=mgR12=5.23×108\Delta E=\left(-\dfrac{GMm}{6R}\right)-\left(-\dfrac{GMm}{4R}\right)=\dfrac{GMm}{12R}=\dfrac{mgR}{12}=5.23\times10^{8} J.

Answer: the binding energy is 1.57×109\approx1.57\times10^{9} J and the transfer needs 5.23×108\approx5.23\times10^{8} J. Climbing to the higher orbit costs energy even though the orbital SPEED there is smaller — the potential well pays the kinetic loss back twice over.

Example 8 — Effective gravity at a latitude. The Earth (R=6400R=6400 km, day 24 h) turns once about its axis. By how much does this spin reduce the effective gg at latitude λ=45\lambda=45^\circ?

  • Angular speed: ω=2π86400=7.27×105\omega=\dfrac{2\pi}{86400}=7.27\times10^{-5} rad/s, giving the equatorial reduction ω2R=(7.27×105)2(6.4×106)=3.38×102\omega^2R=\left(7.27\times10^{-5}\right)^2\left(6.4\times10^{6}\right)=3.38\times10^{-2} m/s2^2.
  • At latitude 4545^\circ: reduction =ω2Rcos2λ=(3.38×102)(cos245)=(3.38×102)(0.5)=1.69×102=\omega^2R\cos^2\lambda=\left(3.38\times10^{-2}\right)\left(\cos^245^\circ\right)=\left(3.38\times10^{-2}\right)(0.5)=1.69\times10^{-2} m/s2^2.

Answer: the effective gg drops by about 1.7×1021.7\times10^{-2} m/s2^2 at 4545^\circ — exactly half the equatorial reduction, since cos245=12\cos^245^\circ=\tfrac12 — leaving gλ9.78g_\lambda\approx9.78 m/s2^2. The cosine enters SQUARED; using it only once overstates the effect.