Value of g - CGS, FPS, Earth, FAQs

Value of g - CGS, FPS, Earth, FAQs

Vishal kumarUpdated on 16 Nov 2025, 11:43 PM IST

Acceleration due to gravity, commonly denoted by g, is one of the most important concepts in Class 11 Physics and competitive exams like JEE and NEET. In this article, we will understand what g is, how it is derived, how it varies with height and depth, and how it differs from the universal gravitational constant G. You will also learn why objects fall at the same rate and how factors like altitude and Earth’s shape affect the value of g.

This Story also Contains

  1. What is Acceleration Due to Gravity (g)?
  2. Is g a Constant?
  3. Why Do Objects of Different Masses Fall at the Same Rate?
  4. Direction and Unit of g
  5. Relation Between g and G
  6. Mass, Radius, and Density of the Earth
  7. Variation of g-Factors Affecting Acceleration Due to Gravity
  8. Why is g Zero at the Centre of the Earth?
Value of g - CGS, FPS, Earth, FAQs
Value of g

What is Acceleration Due to Gravity (g)?

According to Newton's Second Law, a force $\mathbf{F}$ acting on a mass $\mathbf{m}$ produces acceleration a:

$
F=m a
$


If this force is due to the Earth's gravity, the acceleration produced is called acceleration due to gravity, represented by $\mathbf{g}$ :

$
F=m g
$

Thus, $g$ is the acceleration experienced by a body when it freely falls under the Earth's gravitational pull.

Is g a Constant?

Unlike $\mathbf{G}$ (universal gravitational constant), $\mathbf{g}$ is NOT constant everywhere.
The value of $g$ changes due to:

  • Altitude (height above Earth)
  • Depth below Earth
  • Shape of Earth
  • Rotation of Earth

However, a standard value is used for calculations:

$
g=9.8 \mathrm{~m} / \mathrm{s}^2
$

Why Do Objects of Different Masses Fall at the Same Rate?

The value of $g$ does not depend on the mass, size, or shape of the falling body.
This is why, as Galileo demonstrated, two objects dropped from the same height reach the ground at the same time (ignoring air resistance).
Air resistance (upthrust) is the only reason larger objects fall slower.

Direction and Unit of g

  • Direction: Always toward the center of the Earth.
  • SI Unit: $m / s^2$ or $N / k g$
  • Dimensional Formula: $M^0 L^1 T^{-2}$
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Relation Between g and G

Let us consider earth to be a sphere of mass M, radius R with the centre of earth as O. Now, if a body of mass m is placed on the surface of earth, g is the acceleration due to gravity acting on it.

A body of mass m is placed on the surface the earth.

The gravitational force between Earth (mass M) and the body is:

$
F=\frac{G M m}{R^2}
$


But this force is also equal to $\mathbf{m g}$ :

$
m g=\frac{G M m}{R^2}
$

$
g=\frac{G M}{R^2}
$

g depends on Earth’s mass (M) and Earth’s radius (R) not on the body’s mass.

Mass, Radius, and Density of the Earth

Using:

$
g=\frac{G M}{R^2}
$


We can calculate Earth's mass:

$
M=\frac{g R^2}{G}
$


For radius $R=6400 \mathrm{~km}$,

$
M \approx 6.0 \times 10^{24} \mathrm{~kg}
$
Density:

$
\rho=\frac{3 M}{4 \pi R^3}
$

Variation of g-Factors Affecting Acceleration Due to Gravity

Acceleration due to gravity changes with height, depth, and Earth's shape.
Let's understand each case.
1. Variation of g With Height (Altitude)

At Earth's surface:

$
g=\frac{G M}{R^2}
$


At height $h$ above the surface:

$
g^{\prime}=\frac{G M}{(R+h)^2}
$


For small heights ( $h \ll R$ ):

$
g^{\prime}=g\left(1-\frac{2 h}{R}\right)
$
g decreases with increase in height - this is why gravity is slightly weaker on mountains.

2. Variation of g With Depth

At Earth's surface:

$
g=\frac{G M}{R^2}
$


At depth $\mathbf{d}$ :

$
g^{\prime}=g\left(1-\frac{d}{R}\right)
$

g decreases linearly with depth and becomes zero at Earth's center.

3. Variation of g Due to Earth's Shape

Earth is not a perfect sphere; it is an oblate spheroid:

  • Radius at equator: larger
  • Radius at poles: smaller

Since:

$
g \propto \frac{1}{R^2}
$

g is maximum at poles and minimum at the equator.

Also Read:

Why is g Zero at the Centre of the Earth?

At the centre, gravitational pull from all sides cancels out, resulting in:

$
g=0
$


Summary

  • $\mathrm{g}=9.8 \mathrm{~m} / \mathrm{s}^2$ near Earth's surface
  • g varies with height, depth, and Earth's radius
  • $g$ is maximum at poles and minimum at equator
  • g becomes zero at Earth's centre
  • Objects fall at the same rate because $g$ is independent of mass

Also read -

NCERT Physics Notes:

Frequently Asked Questions (FAQs)

Q: How will you find the percentage decrease in value of g with height h?
A:

Decrease in value of g is- g-g’=2hg/R.

                Thus fractional decrease in value of g is (g-g’)/g=2h/R

                 Then, percentage decrease in value of g= [(g-g’)/g]×100=[2h/R]×100

Q: What will happen if gravity suddenly disappears?
A:

 If gravity suddenly disappears,

  1. all the bodies will be suddenly thrown away from the surface due to earth’s centrifugal  

force.

  1. Motion of the satellites around earth, both natural and artificial will not be possible as no centripetal force will be provided.

  2. All the materials will lose their weights, etc.

Q: What are the two factors which determine why some celestial bodies in the solar system have atmosphere and some don’t?
A:

Ability of a celestial body to hold its atmosphere depends on 2 factors mainly- acceleration due to gravity i.e. value of g and its surface temperature.

Q: What is the value of g on the moon?
A:

1.625meter per second squared.

Q: What is the value of g on the sun?
A:

Using equation-2 and putting values of the sun's mass and radius, the value of g on the sun 

       is found to  be 274.13 meter per second squared.

Q: What is the unit of g in FPS?
A:

In the FPS (Foot-Pound-Second) system, the unit of acceleration due to gravity g is:feet per second squared (ft/s²)

Q: What is the gravity of the Earth in CGS units?
A:

In the CGS system, the unit of g is:

cm/s² (centimeter per second squared)

Q: What affects the 'g value'?
A:

The acceleration due to gravity g is affected by:

  • Height (altitude): g decreases with height

  • Depth below Earth’s surface: g decreases with depth

  • Latitude / shape of Earth: g is minimum at the equator and maximum at the poles

  • Earth’s rotation: reduces effective gravity, especially at the equator

  • Local geological variations: density of rocks below the surface