Gravitation

Physics
NEET UG
Version 1Updated 22 Mar 2026

Gravitation is a fundamental natural phenomenon by which all things with mass or energy – including planets, stars, galaxies, and even light – are attracted to (or gravitate toward) one another. It is one of the four fundamental interactions of nature, alongside the strong nuclear force, the weak nuclear force, and electromagnetism. In classical physics, it is described by Newton's Law of Universa…

Quick Summary

Gravitation is the universal attractive force between any two objects with mass. Newton's Law of Universal Gravitation states that this force is directly proportional to the product of their masses (m1m2m_1 m_2) and inversely proportional to the square of the distance (r2r^2) between their centers, given by Fg=Gm1m2r2F_g = G \frac{m_1 m_2}{r^2}.

Here, GG is the universal gravitational constant (6.674×1011,N m2/kg26.674 \times 10^{-11},\text{N m}^2/\text{kg}^2). The acceleration due to gravity (gg) on Earth's surface is approximately 9.8,m/s29.8,\text{m/s}^2, and it varies with altitude, depth, latitude, and Earth's rotation.

Gravitational potential (Vg=GM/rV_g = -GM/r) is the potential energy per unit mass, and gravitational potential energy (Ug=GMm/rU_g = -GMm/r) is the energy stored in a system of two masses. Escape velocity (ve=sqrt2GM/Rv_e = sqrt{2GM/R}) is the minimum speed needed to escape a planet's gravity, while orbital velocity (vo=sqrtGM/rv_o = sqrt{GM/r}) is the speed required to maintain a stable orbit.

Kepler's laws describe planetary motion: elliptical orbits, equal areas swept in equal times, and T2proptoa3T^2 propto a^3. These principles explain everything from falling objects to satellite motion and the structure of galaxies.

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Key Concepts

Variation of 'g' with Altitude

As an object moves to a height hh above the Earth's surface, the distance from the center of the Earth…

Gravitational Potential Energy

Gravitational potential energy (UU) represents the work done to bring a mass from infinity to a specific…

Relationship between Escape Velocity and Orbital Velocity

For an object orbiting very close to the surface of a planet (where orbital radius rapproxRr approx R), the orbital…

  • Newton's Law:F=Gm1m2r2F = G \frac{m_1 m_2}{r^2}
  • Universal Gravitational Constant:G=6.67×1011,N m2/kg2G = 6.67 \times 10^{-11},\text{N m}^2/\text{kg}^2
  • Acceleration due to gravity (surface):g=GMERE2approx9.8,m/s2g = \frac{GM_E}{R_E^2} approx 9.8,\text{m/s}^2
  • Variation of g (altitude):g_h = g left(1 - \frac{2h}{R_E}\right) (for hllREh ll R_E)
  • Variation of g (depth):g_d = g left(1 - \frac{d}{R_E}\right)
  • Gravitational Potential Energy:U=GMmrU = -\frac{GMm}{r}
  • Gravitational Potential:V=GMrV = -\frac{GM}{r}
  • Escape Velocity:ve=sqrt2GMR=sqrt2gRv_e = sqrt{\frac{2GM}{R}} = sqrt{2gR}
  • Orbital Velocity:vo=sqrtGMr=sqrtgR2rv_o = sqrt{\frac{GM}{r}} = sqrt{\frac{gR^2}{r}}
  • Relationship:ve=sqrt2vov_e = sqrt{2} v_o (near surface)
  • Kepler's 3rd Law:T2proptoa3T^2 propto a^3

To remember the variations of 'g': All Deep Layers Rotate Slowly.

  • Altitude: 'g' decreases.
  • Depth: 'g' decreases.
  • Latitude: 'g' minimum at equator, maximum at poles.
  • Rotation: Reduces 'g' at equator.
  • Shape (oblate spheroid): 'g' less at equator due to larger radius.
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