Chapter 1 — Gravitation
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Can You Recall?
- What are the effects of a force acting on an object?
- What types of forces are you familiar with?
- What do you know about the gravitational force?
Gravitation is a universal force: it acts between any two masses anywhere in the universe.
1) Gravitation — The Idea
Newton’s Insight
Observing a falling apple, Newton reasoned that the Earth attracts the apple towards its centre. The vertical direction at any place is along the line joining that point to Earth’s centre. He extended this idea to the Moon, planets and the Sun: the same attractive force could be guiding celestial motions.
Force & Motion
A force changes the speed and/or the direction of motion. (Recall Newton’s laws.) Celestial motion involves continuous change of direction, hence a continuous force.
2) Circular Motion & Centripetal Force
Definition The centripetal force is the inward force required to keep an object moving in a circular path of radius \(r\) with speed \(v\).
For the Moon orbiting Earth (and planets around the Sun), this needed centripetal force is provided by gravity.
3) Kepler’s Laws of Planetary Motion
First Law (Law of Orbits)
Planets move in elliptical orbits with the Sun at one focus.
Ellipse: sum of distances from any point on the curve to the two foci is constant.
Second Law (Law of Areas)
The line joining a planet and the Sun sweeps equal areas in equal times. Planets move faster near perihelion and slower near aphelion.
Third Law (Harmonic Law)
The square of the orbital period is proportional to the cube of the semi-major axis (mean distance \(r\)).
4) Newton’s Universal Law of Gravitation
Statement Every pair of masses \(m_1\) and \(m_2\), separated by distance \(d\), attract each other with a force
- \(F\) is along the line joining their centres (or centres of mass).
- \(G\) is the universal gravitational constant. In SI, \([G] = \mathrm{N\,m^2\,kg^{-2}}\).
- For spherical bodies, take \(d\) as distance between centres.
Application: Ocean Tides
High and low tides occur mainly due to the Moon’s gravity pulling Earth’s oceans. Places roughly 90° away experience low tide at the same time.
5) Acceleration due to Gravity (g)
Earth’s gravitational force on a mass \(m\) at distance \(r\) from Earth’s centre (mass \(M\)):
On Earth’s surface (\(r=R\)):
Variation of g
- With latitude (on surface): Earth is oblate; \(R\) is slightly smaller at poles → \(g\) higher at poles (~9.832 m/s²) and lower at equator (~9.780 m/s²).
- With height: \(g(h)=\dfrac{GM}{(R+h)^2}\) — decreases with \(h\); small change for \(h\ll R\).
- With depth: \(g\) decreases as we go inside Earth (effective mass contributing reduces).
- Other worlds: \(g\) depends on \(M\) and \(R\). On Moon, \(g\approx \tfrac{1}{6}g_{\oplus}\).
6) Mass and Weight
Mass
- Amount of matter (inertia measure). Scalar; SI unit: kg.
- Independent of location (same on Earth, Moon, etc.).
Weight
The gravitational force on a body: \(W=mg\). Vector (towards Earth’s centre). Varies with \(g\).
In everyday speech we often say “weight in kg”, but scientifically that’s mass.
7) Free Fall
When only gravity acts, an object is in free fall. Taking upward as positive, for objects dropped from rest:
8) Gravitational Potential Energy (Concept)
Near Earth for small heights \(h\) (\(h\ll R\)), we often use \(U\approx mgh\) with \(U=0\) on ground by choice. For large distances, it’s convenient to take \(U=0\) at infinity; then the gravitational potential energy of mass \(m\) at distance \(r=R+h\) from Earth’s centre is
9) Escape Velocity
Definition The minimum speed required at the surface so that a body can escape Earth’s gravity and reach infinity with zero residual speed.
For Earth, \(v_{\text{esc}}\approx 11.2\,\mathrm{km\,s^{-1}}\) (air resistance neglected).
10) Weightlessness in Space
Astronauts feel “weightless” in orbit not because \(g=0\) (it isn’t), but because spacecraft and everything inside are in continuous free fall around Earth (same acceleration), producing apparent weightlessness.
Worked Examples
Example A — Tiny attraction between two people
Given: \(m_1=75\,\text{kg},\; m_2=80\,\text{kg},\; d=1\,\text{m},\; G=6.67\times10^{-11}\,\mathrm{N\,m^2\,kg^{-2}}\)
Extremely small—overpowered by friction and other forces in daily life.
Example B — Earth’s pull on a person
Given: \(M=6\times10^{24}\,\text{kg},\; R=6.4\times10^6\,\text{m},\; m=75\,\text{kg}\)
Corresponding acceleration \(a=F/m\approx 9.77\,\mathrm{m\,s^{-2}}\); velocity after 1 s from rest: \(v\approx 9.77\,\mathrm{m\,s^{-1}}\).
Example C — Free fall from 125 m
Given: \(u=0,\; s=125\,\text{m},\; g=10\,\mathrm{m\,s^{-2}}\)
At half the time (2.5 s): \(s=\tfrac{1}{2}g t^2=31.25\,\text{m}\Rightarrow\) height above ground \(=125-31.25=93.75\,\text{m}.\)
Example D — Ball thrown upwards to 4.05 m
Given: Max height \(s=4.05\,\text{m},\; g=10\,\mathrm{m\,s^{-2}}\)
Example E — Weight on the Moon
If weight on Earth is 750 N (mass \(m\)), then using \(g_{\text{Moon}}\approx \tfrac{1}{6}g_{\oplus}\):
Typical Values of g with Height
| Place / Height (km) | Approx. \(g\) (m/s²) | Remark |
|---|---|---|
| Surface (avg), 0 | 9.8 | Reference value |
| Mount Everest, 8.8 | ≈ 9.8 | Very small change |
| Max man-made balloon, 36.6 | ≈ 9.77 | Small decrease |
| Low-Earth Orbit sat., 400 | ≈ 8.7 | Significant drop |
| Geostationary sat., 35,700 | ≈ 0.225 | Very weak pull |
Use Your Brain Power
- Is there a gravitational force between you and your friend? If yes, why don’t you move noticeably?
- If Earth’s mass doubled and radius halved, what happens to \(g\)? (Hint: \(g\propto M/R^2\)).
- What would happen if there were no gravity?
- Why do satellites not fall to Earth though gravity pulls them inward?
Great Scientist: Sir Isaac Newton (1642–1727)
Authored Principia; formulated the laws of motion, universal gravitation, and developed calculus. Built the first reflecting telescope.
Great Scientist: Johannes Kepler (1571–1630)
Using Tycho Brahe’s observations, Kepler discovered the three laws of planetary motion—later derived by Newton from his gravitational theory.
Quick Formula Sheet
- Universal gravitation: \(F=G\dfrac{m_1m_2}{d^2}\)
- Centripetal force: \(F_c=\dfrac{mv^2}{r}\)
- \(g\) at distance \(r\): \(g=\dfrac{GM}{r^2}\), at surface: \(g=\dfrac{GM}{R^2}\)
- Weight: \(W=mg\)
- Free fall (from rest): \(v=gt,\ s=\tfrac{1}{2}gt^2,\ v^2=2gs\)
- Projectile straight up: use \(a=-g\)
- Potential energy (far-field): \(U=-\dfrac{GMm}{r}\)
- Escape velocity: \(v_{\text{esc}}=\sqrt{\dfrac{2GM}{R}}\)
Chapter Wrap-Up
Gravitation is a universal attraction explained quantitatively by Newton’s inverse-square law and supported by Kepler’s observational laws. Near Earth, it gives rise to the acceleration \(g\), governs free-fall and weight, and explains orbital motion, tides, and escape velocity. In orbit, apparent weightlessness is a consequence of continuous free fall.
Chapter 1 — Gravitation: Exercise Solutions
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Q1) Rewrite the table by putting connected items in a single row
| I (Concept) | II (Unit) | III (Key Property) |
|---|---|---|
| Mass | kg | Measure of inertia |
| Weight | N | Depends on height (varies with \(g\)) |
| Acceleration due to gravity | m/s² | Zero at the centre (of the Earth) |
| Gravitational constant | N·m²/kg² | Same in the entire universe |
Q2) Answer the following
a) Mass vs Weight; values on Mars?
- Mass (\(m\)): Amount of matter; scalar; SI unit kg; same everywhere; measure of inertia.
- Weight (\(W\)): Gravitational force on the body; vector; \(W=mg\); SI unit N; changes with local \(g\).
- On Mars: \(m\) remains the same; \(W\) decreases because \(g_{\text{Mars}} < g_{\oplus}\).
b) Definitions
- Free fall: Motion only under gravity (no other forces). From rest: \(\;v=gt,\; s=\tfrac{1}{2}gt^2,\; v^2=2gs\).
- Acceleration due to gravity (\(g\)): \(g=\dfrac{GM}{r^2}\) (towards Earth’s centre). Near surface \(g\approx 9.8\,\mathrm{m/s^2}\).
- Escape velocity (\(v_{\text{esc}}\)): Minimum speed at surface to reach infinity with zero speed: \(\;v_{\text{esc}}=\sqrt{\dfrac{2GM}{R}}\).
- Centripetal force: Inward force to keep circular motion: \(\;F_c=\dfrac{mv^2}{r}\).
c) Kepler’s Laws → Newton’s inverse-square
- Law of Orbits: Planetary orbits are ellipses with Sun at one focus.
- Law of Areas: Equal areas are swept in equal times (variable speed).
- Harmonic Law: \(T^2 \propto r^3\).
d) Equal times up and down
Upward motion with initial speed \(u\), acceleration \(-g\): at top \(v=0\).
Descending from rest at top: \(u=0\), distance \(h\), acceleration \(+g\).
Hence: time to go up equals time to come down.
e) If \(g\) suddenly doubles, why is pulling an object along the floor twice as difficult?
Normal reaction \(N=mg\). Limiting friction \(f=\mu N=\mu mg\). If \(g\to 2g\), then \(f\to 2\mu mg\): the resistive force doubles. Thus it becomes twice as difficult to pull the object.
Q3) Explain why the value of \(g\) is zero at the centre of the Earth.
Inside a spherically symmetric Earth of uniform density, only the mass at radius \(r\) contributes to gravity at that radius; outer shells cancel. The enclosed mass \(M(r)\propto r^3\), and \(g(r)=\dfrac{GM(r)}{r^2}\propto r\). Hence as \(r\to 0\) (centre), \(g\to 0\).
Q4) If a planet’s period is \(T\) at distance \(R\), show it becomes \(8T\) at distance \(2R\).
Note: If your textbook expects \(8T\) (not \(2\sqrt2\,T\)), that would be a misprint. By Kepler’s third law, the correct factor is \(2\sqrt{2}\approx 2.828\), not \(8\).
Q5) Numerical Problems (Solved with steps)
a) Drop from 5 m takes 5 s → find \(g\)
Ans: \(0.4~\mathrm{m/s^2}\) ✓
b) \(R_A=\tfrac12 R_B\). If \(g_B=\tfrac12 g_A\), find \(M_B\) in terms of \(M_A\).
Ans: \(2M_A\) ✓
c) On Earth: \(m=5\) kg, \(W=49\) N. On Moon (\(g_{\text{Moon}}=\tfrac16 g_{\oplus}\))?
Mass unchanged: \(5\) kg. Weight: \(W_{\text{Moon}}=mg_{\text{Moon}}=5\times \tfrac{9.8}{6}\approx 8.17\) N.
Ans: \(5\) kg and \(8.17\) N ✓
d) Thrown up to \(h=500\) m, \(g=10~\mathrm{m/s^2}\): find \(u\) and total time
Ans: \(u=100\) m/s and \(t=20\) s ✓
e) Ball falls from table, reaches ground in \(1\) s (\(g=10\))
Ans: \(v=10\) m/s; table height \(=5\) m ✓
f) Force between Earth and Moon
Data: \(M_E=6\times10^{24}\) kg, \(M_M=7.4\times10^{22}\) kg, \(r=3.84\times10^5\) km \(=3.84\times10^{8}\) m, \(G=6.7\times10^{-11}\).
Ans: \(2\times 10^{20}\) N ✓
g) Mass of the Sun
Data: \(F=3.5\times10^{22}\) N, \(r=1.5\times10^{11}\) m, \(M_E=6\times10^{24}\) kg, \(G=6.7\times10^{-11}\).
Ans: \(1.96\times10^{30}\) kg ✓
Extra: Escape Velocity Examples
On the Moon
Data: \(M=7.34\times10^{22}\) kg, \(R=1.74\times10^6\) m, \(G=6.67\times10^{-11}\).
Ans: \(2.37\ \text{km/s}\) ✓
On the Earth (reference)
Final Notes
Spacecraft must launch with speed (or staged boosts) exceeding local escape conditions to break free of Earth’s gravity and set course for the Moon/planets.
All computations rounded sensibly; equations are typeset with MathJax for clarity.