Abstract

The sensing of gravity has emerged as a tool in geophysics applications such as engineering and climate research1–3, including the monitoring of temporal variations in aquifers4 and geodesy5. However, it is impractical to use gravity cartography to resolve metre-scale underground features because of the long measurement times needed for the removal of vibrational noise6. Here we overcome this limitation by realizing a practical quantum gravity gradient sensor. Our design suppresses the effects of micro-seismic and laser noise, thermal and magnetic field variations, and instrument tilt. The instrument achieves a statistical uncertainty of 20 E (1 E = 10−9 s−2) and is used to perform a 0.5-metre-spatial-resolution survey across an 8.5-metre-long line, detecting a 2-metre tunnel with a signal-to-noise ratio of 8. Using a Bayesian inference method, we determine the centre to ±0.19 metres horizontally and the centre depth as (1.89 −0.59/+2.3) metres. The removal of vibrational noise enables improvements in instrument performance to directly translate into reduced measurement time in mapping. The sensor parameters are compatible with applications in mapping aquifers and evaluating impacts on the water table7, archaeology8–11, determination of soil properties12 and water content13, and reducing the risk of unforeseen ground conditions in the construction of critical energy, transport and utilities infrastructure14, providing a new window into the underground.

Highlights

  • To enable gravity cartography, and operation in application-relevant conditions, we implement an ‘hourglass’ configuration cold atom gravity gradiometer[27]

  • Reduces cloud centre-of-mass motion by an order of magnitude when compared to conventional six-beam approaches

  • To measure the gravity gradient, each magneto-optical traps (MOTs) is loaded for 1 to 1.5 s with 87Rb atoms before sub-Doppler cooling is used to reduce the cloud temperatures to the microkelvin regime

Read more

Summary

Tunnel

Future gravity cartography to search for tunnels and large or near-surface utilities, and to detect erosion features before they become sinkholes. The sensor could be moved from one spatial position to another within 75 s, including alignment to the vertical to within 1 millidegree If addressing these aspects, such as through operation on a rail or vehicle, the current instrument performance would in principle allow detection of the tunnel, or similar anomaly, with a 10-point line scan and a signal-to-noise ratio of 3 within 15 min of total measurement time. Capability assessment and challenges for quantum technology gravity sensors for near surface terrestrial geophysical surveying. A. Sensitive absolute-gravity gradiometry using atom interferometry. Bayesian signal processing techniques for the detection of highly localised gravity anomalies using quantum interferometry technology. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/

Methods
Code availability
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call