A model for calculating the electromagnetic frequency of pressurized rocks

Before large earthquakes, the earth sends transient signals, sometimes strong, more subtle, and transient. These signals may include changes in the local magnetic field, electromagnetic propagation over a wide range of frequencies, a variety of atmospheric and ionospheric phenomena. There is an uncertainty about the nature of the processes that can produce these signals inside the Earth's crust and on the surface. The lack of a comprehensive physical mechanism leads to confusion.Most rocks have been found to have SiO۳ proxy defects. These holes are the key to a deeper understanding of pre-earthquake signals. When they are under stress, the proxy links are broken, releasing the charge carriers h, known as positive holes. Positive holes can flow below the surface under stress. It looks like a sack that encloses with a drawstring. When the battery circuit is closed, we have an output ho. The output ho is an electric current, which changes the magnetic field and emits a low frequency EM. In this research, the equation of electromagnetic waves in pressurized rocks is presented based on a model.

کلیدواژه ها:

Electromagnetic waves ، technical movements ، pressurized rocks