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Magnetic monopoles at the LHC and in the Cosmos - Rencontres de ...

Magnetic monopoles at the LHC and in the Cosmos - Rencontres de ...

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Polar volcanic rock search<br />

– equilibrium conditions<br />

Gravit<strong>at</strong>ional force F g = ma <strong>in</strong><br />

equilibrium with magnetic force<br />

F m = gecB<br />

• Dirac charge (g = 68.5) →<br />

equilibrium above <strong>the</strong> coremantle<br />

boundary (B) for:<br />

m < 4·10 14 GeV<br />

• (solid) mantle convection br<strong>in</strong>gs<br />

up <strong>monopoles</strong> to <strong>the</strong> surface<br />

Over geologic time, accumul<strong>at</strong>ion <strong>in</strong> <strong>the</strong><br />

mantle bene<strong>at</strong>h <strong>the</strong> geomagnetic poles for<br />

a wi<strong>de</strong> range of masses <strong>and</strong> charges<br />

14

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