Key relationship
Outside: g=GM/r². Inside uniform sphere: g=g₀r/RE; r=RE+h.
Physics · Class 11
Above Earth, gravity falls by the inverse-square law. Inside a uniform sphere only the mass enclosed by the probe radius contributes, so gravity decreases linearly to zero at the centre.
Open the interactive experiment →புவிக்கு வெளியே ஈர்ப்பு முடுக்கம் 1/r² என குறையும். சீரான அடர்த்தி புவியின் உள்ளே மையத்தில் அது பூஜ்யமாகும்.
Outside: g=GM/r². Inside uniform sphere: g=g₀r/RE; r=RE+h.
Above Earth, gravity falls by the inverse-square law. Inside a uniform sphere only the mass enclosed by the probe radius contributes, so gravity decreases linearly to zero at the centre.
The exterior inverse-square law cannot be extended unchanged down to the centre.
Spherical nonrotating Earth of uniform density inside, inverse-square field outside. Actual Earth is layered and rotating; depth relation is an idealization.
Compare altitude and depth laws and their assumptions.
Try both scenarios, change one control, and predict the result before checking the graph and readouts.
Change one input while keeping the others fixed, as you would in a controlled experiment.
At depth RE/2, r=RE/2 and g=g₀/2. At altitude RE, r=2RE and g=g₀/4.
The model connects probe gravity inside and above earth with an observable reading. Check the equation and assumptions before applying it.
SI units · algebra · graph reading
In a uniform Earth, what is gravity at the centre?
At r=0 the inward contributions cancel and g=g₀r/RE=0.
Course connection: Class XI Chapter 7. Consult the roadmap for CBSE, NEET, JEE Main and Advanced scope.