TY - JOUR
T1 - Searching for Magnetic Monopoles with Earth's Magnetic Field
AU - Bai, Yang
AU - Lu, Sida
AU - Orlofsky, Nicholas
N1 - Publisher Copyright:
© 2021 authors. Published by the American Physical Society.
PY - 2021/9/3
Y1 - 2021/9/3
N2 - 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 |Bm|<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.
AB - 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 |Bm|<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.
UR - http://www.scopus.com/inward/record.url?scp=85114385550&partnerID=8YFLogxK
U2 - 10.1103/PhysRevLett.127.101801
DO - 10.1103/PhysRevLett.127.101801
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C2 - 34533340
AN - SCOPUS:85114385550
SN - 0031-9007
VL - 127
JO - Physical Review Letters
JF - Physical Review Letters
IS - 10
M1 - 101801
ER -