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This research advances the feasibility of detecting gravitational waves using terrestrial atom interferometers, shifting focus from space-based baselines to ground setups with 100-meter scales. By deriving a novel phase response formula and providing open-source simulation tools, the study addresses critical noise modeling challenges for mid-frequency band detection. The work represents a significant step in integrating quantum sensing technologies into fundamental physics observatories.
Terrestrial Gravitational Wave Detection with Atom Interferometers
arXiv:2609.01227v1 Announce Type: new Abstract: Atom interferometers (AIFs) are highly precise inertial sensors and are considered promising instruments for the detection of gravitational waves (GWs) and certain dark matter (DM) candidates in the mid-frequency band. While GW detection with AIFs was initially proposed for space-based experiments with baselines spanning thousands of kilometers, recent developments suggest that terrestrial setups with baselines of at least 100 meters may also be capable of detecting GWs. In this work, we analytically derive the GW phase response formula of a ground detector, find an additional term compared to the existing literature and check it our findings numerically. Based on this treatment, we analyze the optimal geometric parameters for earth-bound AIF experiments. Subsequently, we numerically simulate GW detection schemes for these optimized interferometers using an open-source Python algorithm. Numerical simulations of these schemes have are not available to the community, yet crucial for the accurate modeling of noise and non-trivial gravitational backgrounds.
Abstract:Atom interferometers (AIFs) are highly precise inertial sensors and are considered promising instruments for the detection of gravitational waves (GWs) and certain dark matter (DM) candidates in the mid-frequency band. While GW detection with AIFs was initially proposed for space-based experiments with baselines spanning thousands of kilometers, recent developments suggest that terrestrial setups with baselines of at least 100 meters may also be capable of detecting GWs. In this work, we analytically derive the GW phase response formula of a ground detector, find an additional term compared to the existing literature and check it our findings numerically. Based on this treatment, we analyze the optimal geometric parameters for earth-bound AIF experiments. Subsequently, we numerically simulate GW detection schemes for these optimized interferometers using an open-source Python algorithm. Numerical simulations of these schemes have are not available to the community, yet crucial for the accurate modeling of noise and non-trivial gravitational backgrounds.
arXiv:2609.01227 [quant-ph]
(or arXiv:2609.01227v1 [quant-ph] for this version)
https://doi.org/10.48550/arXiv.2609.01227 Focus to learn more arXiv-issued DOI via DataCite (pending registration)
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