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Connection of Potential Energy Formula with mgh

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  • Introduction
  • connecting the General formula to mgh
Maharashtra State Board: Class 11

Introduction

Gravitational potential energy is the energy stored in an object due to its position in Earth's gravitational field. When you lift an object to a height above the Earth's surface, its potential energy increases. Scientists have derived two formulas to calculate this change: a general formula that works for any height, and a simplified formula (mgh) that works for small heights. Understanding how these two formulas are connected helps us see when we can use the simpler mgh formula and when we need the more complex one.

Maharashtra State Board: Class 11

Connecting the General Formula to mgh

Potential Energy at Earth's Surface

When an object of mass m is at Earth's surface (distance r = R from Earth's center):

U1 = \[-\frac{GMm}{R}\]

Here, G is the gravitational constant, M is Earth's mass, and R is Earth's radius.

Potential Energy at Height h

When the same object is lifted to a height h above the surface (distance r = R + h from the center):

U2 = \[-\frac{GMm}{R+h}\]

Calculate Change in Potential Energy

The increase in potential energy (work done to lift the object) is:

ΔU = U2 − U1

ΔU = \[-\frac{GMm}{R+h}-\left(-\frac{GMm}{R}\right)\]

ΔU = GMm\[\left(\frac{1}{R}-\frac{1}{R+h}\right)\]

ΔU = GMm\[\begin{pmatrix}
\frac{R+h-R}{R(R+h)}
\end{pmatrix}\]

ΔU = \[\frac{GMmh}{R(R+h)}\]

Apply Surface Gravity Relationship

At Earth's surface, acceleration due to gravity is related to Earth's mass and radius by:

GM = gR2

Substituting this into our equation:

ΔU = \[\frac{gR^2\cdot mh}{R(R+h)}\]

ΔU = \[\frac{mgh\cdot R}{R+h}\]

Apply the Approximation for Small Heights

Key Condition: When h << R (height is much smaller than Earth's radius)

We can approximate: R + h ≈ R

Therefore:

ΔU = mgh

This is the familiar mgh formula for potential energy!

Approximation is Valid:

The simplified mgh formula is accurate when:

  • h is small compared to R: For heights up to a few kilometers above Earth's surface
  • Everyday situations: Heights we encounter in daily life (buildings, mountains, airplane altitude)
  • School-level problems: Most Class 12 physics problems use this approximation

The approximation breaks down when:

  • h is comparable to R: At very high altitudes (thousands of kilometers)
  • Satellite calculations: For objects orbiting Earth
  • Space exploration: When dealing with interplanetary distances

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