01Why this matters
Lifting a book or pumping water uphill stores energy in the object–Earth system. That energy can later transfer into motion or heating.
02See it
03Understand it
Near Earth’s surface, a change in gravitational potential energy is mass × gravitational field strength × change in height.
Use ΔEp = mgΔh when g is approximately constant. Height is vertical height, not distance travelled along a slope. Choose a reference level; changes in energy are what matter. In an ideal fall without air resistance, lost gravitational potential energy becomes kinetic energy.
04Guided example
Raise a 2 kg book by 1.5 m, using g = 9.8 N/kg.
- Identify the vertical change in height: Δh = 1.5 m.
- Calculate the weight: mg = 2 × 9.8 = 19.6 N.
- Multiply by height change: ΔEp = 19.6 × 1.5 = 29.4 J.
05Try it
06Practise it
07Use it in the real world
Pumped storage moves water to a higher reservoir. The higher water has more gravitational potential energy, although practical systems lose some transferred energy to heating and other processes.
Go a little deeper
The formula is a near-surface approximation. Across large changes in distance from Earth, gravitational field strength changes and a more general gravitational potential formula is needed.
08Quick check
09Summary
Near Earth’s surface, a change in gravitational potential energy is mass × gravitational field strength × change in height. Multiply by height change: ΔEp = 19.6 × 1.5 = 29.4 J.
Before moving on, explain the worked example in your own words. Use the hint on any question you want to revisit.
10Key idea
ΔEp = mgΔh
ΔEp: change in energy in J; m: kg; g: N/kg; Δh: vertical change in m.
Δh = ΔEp/(mg), for non-zero m and g
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