Ultracold Quantum Gravimeters: An Introduction for Geophysicists
Ivaldevingles Rodrigues De Souza Junior, Andrea Trombettoni, Carla Braitenberg
TL;DR
This work provides a pedagogical blueprint for geophysicists to understand ultracold-atom quantum gravimeters, linking fundamental quantum concepts to Mach–Zehnder–type atomic interferometry and gravity measurement. It demonstrates that both two- and three-level Raman schemes yield the same interferometric phase structure, with gravity entering as a phase term proportional to $k_{ ext{eff}} g T^2$ and a laser-frequency chirp used to Doppler-compensate for gravity-driven detuning. The article also develops a stability framework based on Allan deviation and the sensitivity function, illustrating how phase and vibration noise propagate to gravity uncertainty through the interferometer response and the noise power spectrum $S_a(oldsymbol{ extomega})$. Overall, it provides a rigorous, self-contained exposition intended to facilitate adoption and innovation of quantum gravimetry in geoscience research and applications.
Abstract
This paper aims at providing an accessible introduction to ultracold quantum gravimeters tailored for geophysicists. We do not focus here on geophysical applications, as these are already well known to geophysicists, but rather provide a pedagogical exposition of the quantum-mechanical concepts needed to understand the operation of quantum gravimeters. We present a review of gravimeters based on two- and three-level atomic systems, focusing on the fundamental mechanisms of atomic interferometry. The functioning of Mach-Zehnder interferometers is discussed through the action of $π/2$ and $π$ pulses, showing how the resulting phase shift encodes gravitational acceleration. The effect of noise is briefly discussed.
