Toward a unified solid state theory for pre-earthquake signals

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An improved coupling model for the lithosphere‐atmosphere‐ionosphere system (2014, background): “In our LAI coupling model, the upward currents can be due to current dynamos associated with the stressed rock [Freund, 2010; Kuo et al., 2011] or the injection of aresols and radon into the atmosphere [Sorokin et al., 2007; Sorokin and Hayakawa, 2013].”
Physical bases of the generation of short-term earthquake precursors: A complex model of ionization-induced geophysical processes in the lithosphere-atmosphere-ionosphere-magnetosphere system (2015, background): “The differ ence is that the external current source used by the authors here is stress activated conductivity of rocks due to p type conductivity (p hole is the electron def icit in a crystalline lattice) (Freund, 2010).”
Ionosphere plasma bubbles and density variations induced by pre‐earthquake rock currents and associated surface charges (2011, background): “The effect of the field ionization of air molecules can be seen as to move some of the positive surface charges to the air with O2 + ions across the air‐rock interface [Freund, 2010].”