Gravitational Decoherence Experiment

Massive objects placed in two places at once — to ask whether gravity itself is what eventually picks one.

Tests proposals — most famously by Diósi (1989) and Penrose (1996) — that the gravitational field of a quantum object cannot itself superpose, so a sufficiently massive spatial superposition collapses spontaneously on a timescale set by its own gravitational self-energy. The experiments use opto-mechanical resonators, levitated nanospheres, matter-wave interferometers, or torsion balances to look for excess decoherence beyond environmental sources, in regimes where the predicted Diósi–Penrose timescale could be reached.

Two main strategies. (1) Matter-wave interferometry: split a massive object's centre-of-mass wave function over a separation Δx, hold it there for time τ, recombine, and read out fringe contrast. Diósi–Penrose predicts an additional decay of contrast as exp(-τ/τ_DP) where τ_DP scales inversely with the gravitational self-energy difference between the two branches. (2) Opto-mechanical: drive a levitated dielectric nanoparticle or membrane resonator into a quantum-coherent state, watch its phase-space distribution as a function of trap configuration, and look for excess noise beyond standard quantum mechanics. Both approaches require: cryogenic environments (typically <50 mK for opto-mechanics, ultra-high vacuum for levitated systems), magnetic and acoustic isolation, and exquisitely characterised baseline decoherence (gas collisions, blackbody photons, charge noise) so that anything left over could be attributed to gravity. As of 2024–2025 no experiment has reached the regime where Diósi–Penrose effects must appear, but several proposals (notably MAQRO, satellite-based; and ground-based ~10⁻¹⁵ kg superpositions) are within an order of magnitude.

In plain terms

Imagine a marble that's somehow in two places at once on a table. Most of physics says the marble stays in two places forever, until someone looks. A few stranger theories say gravity itself eventually picks one — like an invisible referee tapping the marble down. Gravitational decoherence experiments are the rules-of-the-game for catching that referee in the act.

Also called: GDE, Diósi–Penrose test, macroscopic-superposition gravity probe.

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A short history

Lajos Diósi proposed gravitationally induced wavefunction collapse in 1989; Roger Penrose independently formulated a closely related model in 1996, motivated by his concerns about general relativity and quantum measurement. The first proposed table-top tests (Marshall, Simon, Penrose, Bouwmeester 2003) used a tiny mirror reflecting a single photon. Levitated-nanosphere and atom-interferometer routes emerged in the 2010s. The MAQRO mission concept, proposed in 2010 and refined ever since, would carry an interferometer with 10⁻¹⁰-kg test masses to a Lagrange point to escape ground-based seismic and thermal noise. As of 2026, no Diósi–Penrose-regime test has been completed and no claim of detection is supported by the community.

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