The Rikitake model arose from the study of two connected identical frictionless disk dynamos, where reversals of electric current and magnetic field are observed. An analogous model is proposed to explain the highly irregular reversals of the Earth’s magnetic field over geological history.
The original equations describing the system are given by:  ,  ,  ,  , where  and  are the self-inductances of the coils,  and  are the resistances,  and  are the electric currents,  and  are the angular velocities,  and  are the moments of inertia, and  and  are the driving forces. and making the substitutions with the parameter  , we obtain  ,  ,  . The Rikitake system exhibits Lorenz-type chaos while orbiting around two unstable fixed points. [1] T. Rikitake, "Oscillations of a System of Disk Dynamos," Mathematical Proceedings of the Cambridge Philosophical Society, 54(1), 1958 pp. 89–105. doi: 10.1017/S0305004100033223. [2] J. A. Jacobs, Reversals of Earth's Magnetic Field, New York: Cambridge University Press, 1994.
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