Work by a Variable Force
A spring stretches harder the further you pull. Gravity weakens with altitude. Real forces often vary along the path. The total work must then be calculated as a line integral, summing infinitesimal contributions.
Concept
For a force that varies with position, the work done as a particle moves along a path from point to point is
In one dimension with ,
Geometrically, this is the area under the – curve between and (with sign).
Example: Hooke's spring. A spring of stiffness pulled from its natural length to extension exerts force (restoring). The work done by the spring as it extends from to is
The work against the spring (your hand's work) is .
Derivation
Divide the path into many tiny segments . On each segment, the force can be considered constant and the elementary work is
Summing over all segments and taking the limit of infinitesimal ,
For a 1D force,
which is precisely the area under the – graph.
Worked Example
A force N acts on a particle along the -axis. Find the work done as the particle moves from to .
Solution:
Spring example: A spring of stiffness is stretched by 10 cm. Work done by the agent:
Common Confusions
- Not for variable . Plug in an "average" force only if you're careful — for a linear force like a spring, average is , which gives .
- Sign matters in the integral. Reversing the direction of motion flips the sign of , so work flips sign too. Going back to the start gives zero net work for a conservative force.
- Path independence is special. For conservative forces (gravity, spring, electrostatic), work depends only on endpoints, not the path. For non-conservative (friction), it depends on path.
- Area under –: sign matters. Below the axis means negative work.
Key Takeaways
- generalizes work to variable forces.
- In 1D, is the (signed) area under the – curve.
- Spring work: (against the spring).
- For conservative forces, work depends only on endpoints.
- Always integrate force times displacement, not just multiply.