Effect of coil inductance on geophone equation
|Series||Geophysical References Series|
|Title||Problems in Exploration Seismology and their Solutions|
|Author||Lloyd P. Geldart and Robert E. Sheriff|
|Pages||221 - 252|
|Store||SEG Online Store|
If we wish to take into account the small inductance term in the geophone equation (7.9a), show that, for a harmonic wave, it can be included approximately in the term involving the damping factor in equation (7.9b).
The moving-coil electromagnetic geophone is widely used for land seismic work. The basic elements are a case with attached magnet and a coil suspended in the magnetic field by means of springs in such a way that, when an arriving seismic wave moves the case vertically, the inertia of the coil causes it to remain relatively stationary, that is, it moves in a different manner from that of the case; the relative motion between the coil and the magnetic field induces a voltage in the coil that is a replica of the seismic signal that caused the ground motion.
Flexichoc and Vaporchoc are trademarks of Compagnie Géneralé de Géophysique; Maxipulse is a trademark of Western Geophysical Company.
Let , , , and be the mass, radius, number of turns, and current in the coil, and the resistance and inductance of the coil; is the magnetic field strength, the mechanical damping factor (the damping force being vertical velocity of the coil relative to ), electromagnetic force on the coil per unit current, the vertical displacement of the geophone case. Using these symbols, the geophone equation (see Sheriff and Geldart, 1995, 218–20) is
It is usually assumed that is small enough that it can be set equal to zero. In this case the geophone equation reduces to
where natural frequency of oscillation of the coil and
The quantity is called the damping factor for the following reason. If in equation (7.9b), the equation becomes that for undamped simple harmonic motion; if the geophone is at rest and the coil is set in motion, it oscillates forever (theoretically) with undiminished amplitude. However, if , the amplitude decreases steadily by a fixed proportion each cycle; this decrease in amplitude is called damping [see also equation (2.18b)].
If in equation (7.9a) we set in all terms except the first, we get equation (7.9b) plus the additional term . Assuming input of the form , we have , hence . Therefore we can take the term in equation (7.9b) into account by changing the coefficient of to .
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|Characteristics of seismic events||Reflection field methods|
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