Gravitation

Science & Technology
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Version 1Updated 9 Mar 2026

The fundamental principles governing the interaction of masses in the universe are encapsulated by Newton's Law of Universal Gravitation and Kepler's Laws of Planetary Motion. Newton's law states that every particle in the universe attracts every other particle with a force that is directly proportional to the product of their masses and inversely proportional to the square of the distance between…

Quick Summary

Gravitation is the fundamental attractive force between any two objects with mass, as described by Newton's Law of Universal Gravitation (F = G * m1 * m2 / r^2). This law explains why objects fall to Earth and why planets orbit the Sun.

The strength of gravity depends on the masses involved and decreases rapidly with the square of the distance. Kepler's Laws empirically describe planetary motion: elliptical orbits, equal areas swept in equal times, and a relationship between orbital period and orbit size.

Key concepts include gravitational acceleration (g), which varies with altitude, depth, Earth's shape, and rotation; gravitational potential energy; and escape velocity, the speed needed to break free from a celestial body's gravitational pull.

Gravitation is crucial for understanding orbital mechanics, enabling satellite technology (geostationary, polar), GPS systems (requiring relativistic corrections), and explaining tidal forces caused by differential gravity.

Recent advancements include the detection of gravitational waves, opening new avenues in astronomy, and ongoing research into dark matter and dark energy, which hint at deeper gravitational mysteries.

From a UPSC perspective, understanding the applications of these principles in space technology and everyday phenomena is paramount.

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  • Newton's Law:F = G * (m1 * m2) / r^2
  • G:6.674 × 10^-11 N m^2/kg^2
  • 'g' on Earth:~9.81 m/s^2
  • 'g' variation:Max at poles, min at equator; decreases with altitude/depth.
  • Kepler's 1st Law:Elliptical orbits.
  • Kepler's 2nd Law:Equal areas in equal times (faster near Sun).
  • Kepler's 3rd Law:T^2 ∝ a^3.
  • Escape Velocity (Earth):~11.2 km/s.
  • Orbital Velocity:v_orbital = sqrt(G * M / r).
  • Geostationary:35,786 km alt, 24 hr period, fixed position.
  • Polar:Low alt, global coverage, remote sensing.
  • Tidal Forces:Differential gravity (Moon/Sun).
  • Weightlessness:Continuous freefall.
  • GPS:Relativistic corrections essential.
  • Gravitational Waves:Ripples in spacetime, detected by LIGO.

GEKO-VEST: G(ravitational constant), E(scape velocity), K(epler's laws), O(rbital mechanics), V(elocity calculations), E(arth variations), S(atellite types), T(idal effects). This mnemonic helps recall the core concepts and applications of gravitation for UPSC.

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