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arXiv 2103.06286hep-phastro-ph.EP
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利用地球磁场寻找磁单极

Searching for Magnetic Monopoles with the Earth's Magnetic Field

Yang Bai, Sida Lu, Nicholas Orlofsky

摘要:

磁单极子在理论上早就被预测过,可能作为一个稳定的物体存在于我们的宇宙中。当磁单极子在星系中移动时,它们可能会被恒星和行星等天体捕获。在这里,我们提供了一种新的方法来寻找磁单极子通过检测地球的磁场的磁矩。利用Swarm卫星获得的六年多的公共地磁场数据,我们应用高斯定律测量总磁通量,它与地球内部的总磁荷成正比。为了解释卫星高度的长期变化,我们定义了一个高度重新缩放的磁通量,以减少占主导地位的磁偶极子的贡献。测得的磁通量与现有的不包含磁矩项的磁场模型一致。因此,我们将磁单极子在地球表面的磁场强度上限设定为$|B_{\rm m}| < 0.13$ nT(95%置信水平),该值小于地球磁场强度的$2\times 10^{-6}$。这限制了磁荷物体的丰度,包括具有大磁荷的磁性黑洞。

英文摘要:

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 the 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 the 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 $|B_{\rm m}| < 0.13$ nT at 95% confidence level, which is less than $2\times 10^{-6}$ of Earth's magnetic field strength. This constrains the abundance of magnetically-charged objects, including magnetic black holes with large magnetic charges.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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