Gravitation
ЁЯУР Formula & Cheat Sheet (English)
MP Board Class 11 Physics: Gravitation (рдЧреБрд░реБрддреНрд╡рд╛рдХрд░реНрд╖рдг)
Comprehensive Revision Notes & Formula Sheet
1. Universal Law of Gravitation (рдиреНрдпреВрдЯрди рдХрд╛ рд╕рд╛рд░реНрд╡рддреНрд░рд┐рдХ рдЧреБрд░реБрддреНрд╡рд╛рдХрд░реНрд╖рдг рдирд┐рдпрдо)
- Statement: Every particle of matter attracts every other particle with a force directly proportional to the product of their masses and inversely proportional to the square of the distance between them.
- Mathematical Form:
F = G * (m1 * m2) / r^2m1, m2: Masses of the bodiesr: Distance between centersG: Universal Gravitational Constant
- Gravitational Constant (G):
G = 6.67 x 10^-11 N m^2 kg^-2(orm^3 kg^-1 s^-2)- Dimensional Formula:
[M^-1 L^3 T^-2]
2. Acceleration Due to Gravity (g) (рдЧреБрд░реБрддреНрд╡реАрдп рддреНрд╡рд░рдг)
- Acceleration gained by an object due to Earth's gravitational pull.
- Formula on Earth's Surface:
g = (G * M) / R^2- In terms of density (
╧Б):g = (4/3) * ╧А * R * ╧Б * G
- In terms of density (
- Standard Value:
g = 9.8 m/s^2or980 cm/s^2 - Dimensional Formula:
[M^0 L T^-2]
3. Variations in Acceleration Due to Gravity (g рдореЗрдВ рдкрд░рд┐рд╡рд░реНрддрди)
A. Effect of Altitude (Height 'h')
- For any height
h:g_h = g * [R / (R + h)]^2 - For small height (
h << R):g_h тЙИ g * (1 - (2h / R)) - Note:
gdecreases as height increases.
B. Effect of Depth (Depth 'd')
- At depth
dbelow Earth's surface:g_d = g * (1 - (d / R)) - At Center of Earth (
d = R):g_center = 0 - Note:
gdecreases linearly as depth increases.
C. Effect of Latitude / Rotation of Earth (рдЕрдХреНрд╖рд╛рдВрд╢ рдХрд╛ рдкреНрд░рднрд╛рд╡)
- At latitude
╬╗(or angle╧Ж):g_╬╗ = g - R * ╧Й^2 * cos^2(╬╗)╧Й: Angular velocity of Earth's rotation
- At Equator (
╬╗ = 0┬░):g_eq = g - R * ╧Й^2(Minimum value) - At Poles (
╬╗ = 90┬░):g_pole = g(Maximum value)
4. Gravitational Field & Potential (рдЧреБрд░реБрддреНрд╡реАрдп рдХреНрд╖реЗрддреНрд░ рдПрд╡рдВ рд╡рд┐рднрд╡)
A. Gravitational Field Intensity (E)
- Force experienced by a unit mass placed at a point in the gravitational field.
- Formula:
E = F / m = (G * M) / r^2 - Unit:
N/kgorm/s^2 - Vector quantity, directed towards the mass
M.
B. Gravitational Potential (V)
- Work done in bringing a unit mass from infinity to a point in the gravitational field.
- Formula:
V = - (G * M) / r - Unit:
J/kg - Scalar quantity. Always negative (zero at infinity).
C. Relation Between Field and Potential
E = - (dV / dr)
5. Gravitational Potential Energy (U) (рдЧреБрд░реБрддреНрд╡реАрдп рд╕реНрдерд┐рддрд┐рдЬ рдКрд░реНрдЬрд╛)
- Work done in bringing a mass
mfrom infinity to a distancerfrom massM. - Formula:
U = - (G * M * m) / r - Change in Potential Energy (raising height
hfrom surface):╬ФU = (m * g * h) / (1 + (h / R))- If
h << R,╬ФU тЙИ m * g * h
- If
6. Escape Velocity (v_e) (рдкрд▓рд╛рдпрди рд╡реЗрдЧ)
- Minimum velocity with which a body must be projected vertically upwards so that it escapes Earth's gravitational field permanently.
- Formula:
v_e = тИЪ(2 * G * M / R) = тИЪ(2 * g * R) - Value for Earth:
v_e тЙИ 11.2 km/s - Independent of the mass of the projected body and angle of projection.
7. Satellite Motion (рдЙрдкрдЧреНрд░рд╣ рдХреА рдЧрддрд┐)
A. Orbital Velocity (v_o) (рдХрдХреНрд╖реАрдп рд╡реЗрдЧ)
- Velocity required to keep a satellite in its orbit around a planet.
- Formula:
v_o = тИЪ(G * M / r) = тИЪ(G * M / (R + h)) - For satellite near Earth's surface (
h тЙИ 0):v_o = тИЪ(g * R) тЙИ 7.92 km/s
B. Relation between Escape Velocity and Orbital Velocity
v_e = тИЪ2 * v_o тЙИ 1.414 * v_o
C. Time Period of Satellite (T) (рдкрд░рд┐рдХреНрд░рдордг рдХрд╛рд▓)
T = Circumference / Orbital Velocity = (2 * ╧А * r) / v_oT = 2 * ╧А * тИЪ((R + h)^3 / (G * M)) = 2 * ╧А * тИЪ((R + h)^3 / (g * R^2))- Near Earth's surface:
T тЙИ 84.6 minutes(or1.4 hours)
D. Energies of a Revolving Satellite
- Kinetic Energy (KE):
KE = (G * M * m) / (2 * r) - Potential Energy (PE):
PE = - (G * M * m) / r - Total Energy (E):
E = KE + PE = - (G * M * m) / (2 * r) - Binding Energy (BE):
BE = -E = + (G * M * m) / (2 * r)
8. Kepler's Laws of Planetary Motion (рдХреЗрдкреНрд▓рд░ рдХреЗ рдирд┐рдпрдо)
- First Law (Law of Orbits): All planets move in elliptical orbits with the Sun at one of the two foci.
- Second Law (Law of Areas): The line joining the planet to the Sun sweeps out equal areas in equal intervals of time.
- Areal Velocity:
dA / dt = L / (2 * m) = Constant - Direct consequence of the Conservation of Angular Momentum.
- Areal Velocity:
- Third Law (Law of Periods): The square of the time period of revolution of a planet is directly proportional to the cube of the semi-major axis of its elliptical orbit.
T^2 тИЭ a^3orT^2 / r^3 = Constant
9. Satellites: Types & Comparison
| Parameter | Geostationary Satellite (рднреВ-рд╕реНрдерд┐рд░ рдЙрдкрдЧреНрд░рд╣) | Polar Satellite (рдзреНрд░реБрд╡реАрдп рдЙрдкрдЧреНрд░рд╣) |
|---|---|---|
| Orbit Plane | Equatorial plane | Polar plane (North-South) |
| Height above Earth | ~36,000 km | ~500 km to 800 km |
| Time Period | 24 hours | ~100 minutes |
| Direction of Rotation | West to East | North to South |
| Primary Uses | Communication, Weather forecasting | Remote sensing, Meteorology, Military |
10. Quick Memory Check Tips for MP Board Exams
- Weightlessness (рднрд╛рд░рд╣реАрдирддрд╛): Occurs when the effective reaction force on a body is zero (e.g., inside a freely falling lift or in an orbiting satellite).
- Center of Gravity vs Center of Mass: Center of gravity depends on
g, center of mass depends purely on mass distribution. - Inertial Mass vs Gravitational Mass: Inertial mass is measured via
F = ma; Gravitational mass is measured via Newton's law of gravitationF = (G M m)/r^2. Both are numerically equal.