
Experimental techniques using quantum systems like atoms or photons to test gravitational effects and equivalence principles.Quantum gravity probes are experimental setups that use quantum systems — such as atoms, photons, or even macroscopic superpositions — to test how gravity behaves at the quantum scale. While gravity is well described by general relativity for large objects, its interaction with quantum particles remains untested territory. The core question is whether the equivalence principle — the idea that all objects fall the same way regardless of their composition — holds for quantum superpositions, and whether gravity itself must be quantized. These probes aim to catch the first deviations from classical gravity that would signal a deeper quantum theory.
The idea of testing gravity with quantum systems dates back to the 1970s, with the first atom interferometry experiments in the 1990s. The concept of using entanglement to probe quantum gravity was proposed in the 2010s, and current experiments are just reaching the required sensitivities.
A typical probe involves atoms in a state of superposition, where a single atom exists in two places at once. By letting these two 'branches' evolve under gravity and then recombining them, physicists can measure tiny phase shifts caused by gravitational potential differences — this is the basis of atom interferometry. More ambitious proposals involve creating entanglement between two masses purely through gravitational interaction, which would prove that gravity is quantum. Other approaches use photons: sending light through a gravitational field and looking for quantum correlations, or observing how the shadow of a black hole deviates from classical predictions. Each experiment pushes the sensitivity to gravitational effects on quantum systems, testing the universality of free fall at the quantum level.
Quantum gravity probes are primarily research tools, but the ultra-precise atom interferometers they use also serve as next-generation sensors for measuring gravitational fields, with applications in geodesy and inertial navigation.
A single rubidium atom in a superposition of two heights falls at exactly the same rate as a macroscopic object — a fact that has been verified to a precision of one part in a hundred million.








