Precision Measurement of the Newtonian Gravitational Constant Using Cold Atoms

TL;DR

This paper reports a precise measurement of the gravitational constant G using laser-cooled atoms and quantum interferometry, providing an alternative approach that helps identify systematic errors in previous macroscopic experiments.

Contribution

It introduces a novel quantum interferometry method with cold atoms to measure G, differing from traditional torsion balance experiments, and refines the value of G with improved systematic error control.

Findings

Measured G as 6.67191(99) x 10^(-11) m^3 kg^(-1) s^(-2)

Achieved a relative uncertainty of 150 ppm

Value differs by 1.5 standard deviations from the recommended value

Abstract

About 300 experiments have tried to determine the value of the Newtonian gravitational constant, G, so far, but large discrepancies in the results have made it impossible to know its value precisely. The weakness of the gravitational interaction and the impossibility of shielding the effects of gravity make it very difficult to measure G while keeping systematic effects under control. Most previous experiments performed were based on the torsion pendulum or torsion balance scheme as in the experiment by Cavendish in 1798, and in all cases macroscopic masses were used. Here we report the precise determination of G using laser-cooled atoms and quantum interferometry. We obtain the value G=6.67191(99) x 10^(-11) m^3 kg^(-1) s^(-2) with a relative uncertainty of 150 parts per million (the combined standard uncertainty is given in parentheses). Our value differs by 1.5 combined standard deviations from the current recommended value of the Committee on Data for Science and Technology. A conceptually different experiment such as ours helps to identify the systematic errors that have proved elusive in previous experiments, thus improving the confidence in the value of G. There is no definitive relationship between G and the other fundamental constants, and there is no theoretical prediction for its value, against which to test experimental results. Improving the precision with which we know G has not only a pure metrological interest, but is also important because of the key role that G has in theories of gravitation, cosmology, particle physics and astrophysics and in geophysical models.