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Electromagnetic excitation and seismicity in the natural time domain: simulations with theoretical model

Teisseyre R., Varotsos P., Rozłuski C.

Acta Geophysica Polonica

2004

Vol. 52, nr 4

477-496

Numerical simulations of electromagnetic field and electric current are based on the solutions of equations for the dislocation density field with the term including self-interactions between the dislocations; the case under study concerns the charge dislocations. The equations are solved numerically for the medium with thin layers representing the faults and for the initial conditions representing two groups of dislocations of opposite signs facing each other. This case refers to stress concentration; the gradients of stress field, opposite to the central point of stress accumulation, contribute to the respective dislocation densities since the linear dislocation density for a simple 1D case becomes proportional to stress gradient. A single fault, as a zone with small resistance/friction values, is described by rigidities smaller than the bulk rigidity value, while for a fine-band structure of faults the rigidities in the layers between the adjacent faults are assumed to be higher than the bulk value. The results obtained show characteristic features in which the seismic precursory activity simulates that of the main rebound processes represented in the natural time as counted in relation to the consecutive events. Our model contributes to the previous discussion and experimental data related to natural time analysis suggested recently by Varotsos and coworkers.

Thermodynamics of line defects and transient electric current: electromagnetic field generation in earthquake preparation zone

Nagahama H., Teisseyre R.

Acta Geophysica Polonica

1998

Vol. 46, nr 1

35-54

In thermal equilibrium the electrical neutrality of the charge dislocation is assured by a cloud of oppositely charged point defects around it. Here, from the view point of thermodynamics of line vacancies, we propose a possibility of constructing a model of transient electric current generation in an earthquake source zone which combines polarization processes and motion of charged dislocations under the influence of evolving field of stresses. This transient electric current differs essentially from the piezo-electric current in which the electric field is proportional to the stress itself. Then we review briefly the elements of stress evolution theory. Some examples of the stress evolution pattern with the electromagnetic field radiation are shown.