Physics by Lamhi: Not Your Boring Physics

CLASS 11 · CHAPTER 7 · MECHANICS

DETAILED NOTES

Gravitation

The complete chapter, section by section: Kepler's three laws, Newton's law of gravitation, how g changes with height and depth, gravitational potential energy and escape speed, and the mechanics of satellite orbits, explained in plain language with original worked examples; for the interactive satellite-orbit simulation, see the concept page.

7.1 Kepler's Laws of Planetary Motion

Decades before Newton, Johannes Kepler mined Tycho Brahe’s painstaking naked-eye observations of the planets and pulled three purely empirical patterns out of the data, no explanation for why they held, just a precise description of what happened. Newton’s law of gravitation, in the next section, is what finally explains all three.

First law (law of orbits): every planet moves in an ellipse, with the Sun at one focus, not the centre. A circle is only the special case of an ellipse with zero eccentricity, and most planetary orbits are close enough to circular that the distinction is easy to miss.

Second law (law of areas): the line joining a planet to the Sun sweeps out equal areas in equal times. Since the Sun-planet distance changes around the orbit, this forces the planet to move faster when it is close to the Sun (perihelion) and slower when it is far away (aphelion); it is really just a statement that the planet’s angular momentum about the Sun stays constant, because gravity always points straight at the Sun and exerts no torque about it.

Third law (law of periods): the square of a planet’s orbital period is proportional to the cube of its semi-major axis:

T2∝a3T^2 \propto a^3

with the same constant of proportionality for every planet going around the same Sun. This last law is the one Newton’s law of gravitation reproduces most directly, worked out in §7.2.1 below.

7.2 Newton's Universal Law of Gravitation

Newton’s single claim was that the force holding the Moon in its orbit and the force pulling an apple to the ground are the same force, just evaluated at different distances. Any two point masses m1m_1 and m2m_2, separated by a distance rr, attract each other along the line joining them with a force:

Universal law of gravitation
F=Gm1m2r2\textcolor{#e08a1e}{F} = \dfrac{Gm_1m_2}{r^2}

where G=6.674×10−11 N m2kg−2G = 6.674\times10^{-11}\ \text{N m}^2\text{kg}^{-2} is the universal gravitational constant, the same number everywhere in the universe, for any pair of masses whatsoever. It is also tiny, which is why gravity between two everyday objects (two students, say) is utterly unnoticeable, and why it took a dedicated, delicate torsion-balance experiment (Cavendish’s, a century after Newton) to actually measure it in the laboratory. Two more things worth holding onto: the force is always attractive, never repulsive, and it obeys an inverse-square law, so doubling the distance cuts the force to a quarter, not a half.

7.2.1 Reproducing Kepler's third law

For a planet of mass mm in a (nearly) circular orbit of radius rr around the Sun, mass MM, gravity alone has to supply the centripetal force:

GMmr2=mv2r=mr(2πrT)2=4π2mrT2\dfrac{GMm}{r^2} = \dfrac{mv^2}{r} = \dfrac{m}{r}\left(\dfrac{2\pi r}{T}\right)^2 = \dfrac{4\pi^2mr}{T^2}

Cancel mm and rearrange for the period:

T2=(4π2GM)r3T^2 = \left(\dfrac{4\pi^2}{GM}\right)r^3

which is Kepler’s third law, with the proportionality constant pinned down explicitly as 4π2/GM4\pi^2/GM, depending only on the central mass MM. That it works out this cleanly, from a force law Newton proposed for entirely separate reasons, is the strongest evidence that the law of gravitation is correct.

7.3 Acceleration Due to Gravity, and Its Variation with Height and Depth

7.3.1 g at the Earth's surface

A test mass mm resting at the Earth’s surface feels a gravitational pull equal to its weight, mgmg, and treating the Earth as a uniform sphere of mass MM and radius RR (concentrated, by the shell theorem, as if at its centre), Newton’s law gives that same force as GMm/R2GMm/R^2. Equating the two:

g at the surface
g=GMR2\textcolor{#e08a1e}{g} = \dfrac{GM}{R^2}

Notice gg drops out of mm entirely, which is exactly why all objects, heavy or light, fall at the same rate in a vacuum.

7.3.2 Variation with height

At a height hh above the surface, the distance from Earth’s centre becomes R+hR+h, so:

g(h)=GM(R+h)2=g(1+hR)2g(h) = \dfrac{GM}{(R+h)^2} = \dfrac{g}{\left(1+\frac{h}{R}\right)^2}

For h≪Rh \ll R, the binomial approximation (1+x)−2≈1−2x(1+x)^{-2}\approx 1-2x turns this into a much more usable linear form:

g(h)≈g(1−2hR)g(h) \approx g\left(1-\dfrac{2h}{R}\right)

so gg falls off roughly twice as fast, per metre climbed, as it will per metre descended below the surface, which is the whole point of the next subsection.

7.3.3 Variation with depth

Go below the surface instead, to a depth dd, and a different rule applies. By the shell theorem, a uniform spherical shell of matter exerts zero gravitational force on anything strictly inside it, so only the mass enclosed within radius R−dR-d contributes at all; everything farther out simply cancels out. For a uniform-density Earth, that enclosed mass scales as the cube of the radius, M′=M(R−dR)3M' = M\left(\frac{R-d}{R}\right)^3, which gives:

g(d)=GM′(R−d)2=GMR3(R−d)g(d) = \dfrac{GM'}{(R-d)^2} = \dfrac{GM}{R^3}(R-d)
g(d)=g(1−dR)g(d) = g\left(1-\dfrac{d}{R}\right)

a straight line in dd, not a curve, reaching exactly zero at the centre (d=Rd=R), where every direction is equally “down” and the pulls from all sides cancel completely.

Worked example

Climbing up versus tunnelling down by the same distance

Take g=9.8 m/s2g=9.8\text{ m/s}^2 and R=6400 kmR=6400\text{ km}. Compare gg at a height of 64 km above the surface with gg at a depth of 64 km below it.

Height (using the approximate form, since h/R=0.01≪1h/R=0.01\ll1):

g(64 km)≈9.8(1−2×0.01)=9.604 m/s2g(64\text{ km}) \approx 9.8\left(1-2\times0.01\right) = \textcolor{#e08a1e}{9.604\text{ m/s}^2}

Depth, over the same 64 km:

g(64 km down)=9.8(1−0.01)=9.702 m/s2g(64\text{ km down}) = 9.8\left(1-0.01\right) = \textcolor{#e08a1e}{9.702\text{ m/s}^2}

The height formula’s factor of 2 is doing real work here: climbing 64 km costs almost twice as much of gg as descending the same 64 km, exactly as §7.3.2 predicted.

7.4 Gravitational Potential Energy and Escape Speed

7.4.1 Gravitational potential energy

Because gravity is attractive, pulling a mass mm away from MM takes positive work done against the force. Moving it from infinity, where it is conventional to set the potential energy to zero, in to a distance rr therefore requires negative net work (gravity itself is doing positive work, pulling it in), so:

U(r)−U(∞)=−∫∞rGMmr′2 dr′=−GMm[−1r′]∞r=−GMmrU(r) - U(\infty) = -\int_{\infty}^{r} \dfrac{GMm}{r'^2}\,dr' = -GMm\left[-\dfrac{1}{r'}\right]_{\infty}^{r} = -\dfrac{GMm}{r}
Gravitational P.E.
U(r)=−GMmr\textcolor{#e08a1e}{U(r)} = -\dfrac{GMm}{r}

The minus sign is not a convention to memorise, it is a genuine physical fact: any bound system, where the mass cannot escape to infinity on its own, must have negative total energy, with zero as the energy of a mass placed infinitely far away and released from rest.

7.4.2 Escape speed

“Escaping” means reaching infinity with (at worst) zero speed left over, i.e. arriving with exactly zero total mechanical energy. Launched from the surface with speed vev_e, that condition reads:

12mve2−GMmR=0\dfrac{1}{2}mv_e^2 - \dfrac{GMm}{R} = 0
Escape speed
ve=2GMR\textcolor{#e08a1e}{v_e} = \sqrt{\dfrac{2GM}{R}}

Note what vev_e does not depend on: the launched mass mm cancels out completely, and the direction of the launch does not appear anywhere either (ignoring atmospheric drag and the ground itself getting in the way), only the launch speed matters.

Worked example

Earth's escape speed, and why it's exactly √2 times the orbital speed

Take M=6.0×1024 kgM=6.0\times10^{24}\text{ kg} and R=6.4×106 mR=6.4\times10^6\text{ m}. The orbital speed just grazing the surface (§7.5.1 derives this generally) is:

vorbital=GMR=6.674×10−11×6.0×10246.4×106≈7.91 km/sv_{\text{orbital}} = \sqrt{\dfrac{GM}{R}} = \sqrt{\dfrac{6.674\times10^{-11}\times6.0\times10^{24}}{6.4\times10^6}} \approx \textcolor{#e08a1e}{7.91\text{ km/s}}

and the escape speed from the same surface:

ve=2GMR=2×vorbital≈11.19 km/sv_e = \sqrt{\dfrac{2GM}{R}} = \sqrt{2}\times v_{\text{orbital}} \approx \textcolor{#e08a1e}{11.19\text{ km/s}}

The ratio is exactly 2\sqrt{2}, always, for any planet or any launch radius, since both formulas share the same GM/R\sqrt{GM/R} underneath. This is precisely the dividing line the orbit simulation on the concept page is built around: drag the launch-speed slider past 1.41× circular speed and the orbit stops being an ellipse and becomes a one-way trip.

7.5 Orbital Velocity, Satellites, and Energy of an Orbiting Satellite

7.5.1 Orbital velocity and period

A satellite of mass mm coasting in a circular orbit of radius rr needs gravity to supply exactly the centripetal force, with nothing else pushing or pulling it:

GMmr2=mv2r\dfrac{GMm}{r^2} = \dfrac{mv^2}{r}
Orbital velocity
vorbital=GMr\textcolor{#e08a1e}{v_{\text{orbital}}} = \sqrt{\dfrac{GM}{r}}

Larger orbits therefore mean slower satellites, the opposite of what intuition about “falling faster from higher up” might suggest; a satellite further out has farther to fall but a gentler pull doing the falling. The orbital period follows directly, T=2πr/vorbitalT = 2\pi r / v_{\text{orbital}}, which rearranges into the same T2∝r3T^2\propto r^3 law derived in §7.2.1.

7.5.2 Energy of an orbiting satellite

The kinetic energy follows straight from vorbital2=GM/rv_{\text{orbital}}^2=GM/r:

K=12mvorbital2=GMm2rK = \dfrac{1}{2}mv_{\text{orbital}}^2 = \dfrac{GMm}{2r}

and adding the potential energy from §7.4.1, U=−GMm/rU=-GMm/r, gives the total mechanical energy of the orbit:

Total orbital energy
E=K+U=GMm2r−GMmr=−GMm2r\textcolor{#e08a1e}{E} = K+U = \dfrac{GMm}{2r}-\dfrac{GMm}{r} = -\dfrac{GMm}{2r}

Compare the three quantities and a pattern worth memorising falls out: E=−KE=-K, and also E=U/2E=U/2. A bound orbit’s total energy is always negative (confirming it is bound), equals minus its kinetic energy, and equals exactly half of its potential energy, for every circular orbit, regardless of rr, mm, or MM.

Worked example

Energy budget of a low-orbit satellite

A 1000 kg satellite orbits at 300 km altitude above Earth’s surface (R=6.4×106 mR=6.4\times10^6\text{ m}, so r=6.7×106 mr=6.7\times10^6\text{ m}, M=6.0×1024 kgM=6.0\times10^{24}\text{ kg}). Find its kinetic, potential, and total energy.

K=GMm2r=6.674×10−11×6.0×1024×10002×6.7×106≈2.99×1010 JK = \dfrac{GMm}{2r} = \dfrac{6.674\times10^{-11}\times6.0\times10^{24}\times1000}{2\times6.7\times10^6} \approx \textcolor{#e08a1e}{2.99\times10^{10}\text{ J}}U=−GMmr≈−5.98×1010 J,E=K+U≈−2.99×1010 JU = -\dfrac{GMm}{r} \approx \textcolor{#e08a1e}{-5.98\times10^{10}\text{ J}}, \qquad E = K+U \approx \textcolor{#e08a1e}{-2.99\times10^{10}\text{ J}}

Exactly as §7.5.2 promised, E=−KE=-K and E=U/2E=U/2 to within rounding. The orbital speed here works out to about 7.73 km/s and the period to roughly 91 minutes, both close to the International Space Station’s real numbers.

7.6 Geostationary and Polar Satellites, and Weightlessness

7.6.1 Geostationary satellites

A satellite is geostationary when it appears fixed over one spot on the ground, which requires three conditions together: its orbit must lie in the equatorial plane, it must orbit west to east (the same way Earth spins), and its period must equal Earth’s rotation period, about 24 hours. Only one radius satisfies T2=(4π2/GM)r3T^2=(4\pi^2/GM)r^3 for that particular TT, so there is exactly one geostationary orbit, not a family of them. These satellites are what television and communication relays depend on, since a ground dish can point at one fixed spot in the sky permanently.

7.6.2 Polar satellites

A polar satellite instead flies a low orbit (a few hundred to around a thousand kilometres up) passing near both poles on every revolution. Because this orbit is low, its period is only on the order of 100 minutes, far shorter than a day, so as Earth rotates underneath it, each successive pass sweeps over a new strip of the surface. Over enough orbits it images the entire planet, which is exactly why remote-sensing, weather, and mapping satellites use this kind of orbit rather than a geostationary one.

7.6.3 Weightlessness in orbit

It is tempting to say astronauts float because “there is no gravity up there,” but at ISS altitude Earth’s gravity is still roughly 90% as strong as at the surface, more than enough to bend the station’s path into a circle. What actually vanishes is the normal force: the astronaut, the station, and everything loose inside it are all in free fall together, accelerating toward Earth at exactly the same rate, so nothing presses against anything else, and a scale under the astronaut’s feet would read zero. It is the identical situation as a lift in free fall in §4.13 of the previous chapter, just falling around the Earth rather than straight down into it.

Worked example

How far out is geostationary orbit?

Using M=6.0×1024 kgM=6.0\times10^{24}\text{ kg} and T=24 h=86400 sT=24\text{ h}=86400\text{ s}, solve T2=(4π2/GM)r3T^2=(4\pi^2/GM)r^3 for rr:

r=(GMT24π2)1/3=(6.674×10−11×6.0×1024×(86400)24π2)1/3≈4.23×107 mr = \left(\dfrac{GMT^2}{4\pi^2}\right)^{1/3} = \left(\dfrac{6.674\times10^{-11}\times6.0\times10^{24}\times(86400)^2}{4\pi^2}\right)^{1/3} \approx \textcolor{#e08a1e}{4.23\times10^7\text{ m}}

That is the distance from Earth’s centre; subtract R=6.4×106 mR=6.4\times10^6\text{ m} to get the altitude above the surface:

h=r−R≈4.23×107−0.064×107≈3.59×104 kmh = r - R \approx 4.23\times10^7 - 0.064\times10^7 \approx \textcolor{#e08a1e}{3.59\times10^4\text{ km}}

about 35,900 km up, essentially the real figure (35,786 km) that every geostationary communications satellite actually sits at.

— From the NCERT exercises

Two of the chapter’s own exercise questions, with original worked solutions. (g=9.8 m/s2g=9.8\text{ m/s}^2, R=6.4×106 mR=6.4\times10^6\text{ m} where a numeric radius is needed.)

NCERT Exercise 7.12

A rocket is fired vertically with a speed of 5 km/s from the earth's surface. How far from the earth does the rocket go before returning to the earth?

Solution

Energy conservation between launch and the highest point (where the rocket is momentarily at rest, at distance R+hR+h from the centre):

12mv2−GMmR=−GMmR+h\dfrac{1}{2}mv^2 - \dfrac{GMm}{R} = -\dfrac{GMm}{R+h}

Writing GM=gR2GM=gR^2 so that only known quantities appear, and solving for R+hR+h:

1R+h=1R−v22gR2=16.4×106−(5000)22×9.8×(6.4×106)2\dfrac{1}{R+h} = \dfrac{1}{R} - \dfrac{v^2}{2gR^2} = \dfrac{1}{6.4\times10^6} - \dfrac{(5000)^2}{2\times9.8\times(6.4\times10^6)^2}R+h≈7.99×106 m  ⇒  h≈1.6×106 m (≈1600 km above the surface)R+h \approx 7.99\times10^6\text{ m} \;\Rightarrow\; h \approx \textcolor{#e08a1e}{1.6\times10^6\text{ m}\ (\approx1600\text{ km above the surface})}

Since the launch used up all but a sliver of the escape energy (5 km/s is well under the 11.2 km/s needed to escape outright), the rocket climbs a long way, over a thousand kilometres, but still falls back rather than leaving for good.

NCERT Exercise 7.15

A body weighs 63 N on the surface of the earth. What is the gravitational force on it due to the earth at a height equal to half the radius of the earth?

Solution

At height h=R/2h=R/2, the distance from the centre becomes R+h=3R/2R+h = 3R/2, so by the inverse-square law the weight scales by (R/(3R/2))2=(2/3)2=4/9(R/(3R/2))^2 = (2/3)^2 = 4/9, independent of RR itself:

W(h)=W0×49=63×49=28 NW(h) = W_0\times\dfrac{4}{9} = 63\times\dfrac{4}{9} = \textcolor{#e08a1e}{28\text{ N}}