Abstract

Magnetic monopoles have long been predicted in theory and could exist as a stable object in our Universe. As they move around in galaxies, magnetic monopoles could be captured by astrophysical objects like stars and planets. Here, we provide a novel method to search for magnetic monopoles by detecting the monopole moment of Earth's magnetic field. Using over six years of public geomagnetic field data obtained by the Swarm satellites, we apply Gauss's law to measure the total magnetic flux, which is proportional to the total magnetic charge inside Earth. To account for the secular variation of satellite altitudes, we define an altitude-rescaled magnetic flux to reduce the dominant magnetic dipole contribution. The measured magnetic flux is consistent with the existing magnetic field model that does not contain a monopole moment term. We therefore set an upper limit on the magnetic field strength at Earth's surface from magnetic monopoles to be |B_{m}|<0.13 nT at 95%confidence level, which is less than 2×10^{-6} of Earth's magnetic field strength. This constrains the abundance of magnetically charged objects, including magnetic black holes with large magnetic charges.

Highlights

  • As they move around in galaxies, magnetic monopoles could be captured by astrophysical objects like stars and planets

  • We provide a novel method to search for magnetic monopoles by detecting the monopole moment of Earth’s magnetic field

  • Using over six years of public geomagnetic field data obtained by the Swarm satellites, we apply Gauss’s law to measure the total magnetic flux, which is proportional to the total magnetic charge inside Earth

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Summary

Published by the American Physical Society

A numerical integration of Bðr; θ; φÞ · rdΩ will not be zero, even in the absence of a monopole term (for Swarm’s orbital parameters, B ≃ −70 nT, see the Supplemental Material [24]). To suppress this measurement-induced dipole contribution, we use the following modified Gauss law to measure the magnetic field from the monopole charge: B. The r3 scaling in Eq (1) is practically useful to improve the sensitivity of searching for the monopole moment because it reduces contributions to Bfrom the dipole and higher moments while preserving the monopole signal. Data analysis.—We use the VirES architecture to access the data via the PYTHON package VIRESCLIENT [25]

Magnetic field measurements are used from the Swarm
Findings
Time dependent

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