geoana.em.tdem.vertical_magnetic_flux_time_deriv_horizontal_loop#
- geoana.em.tdem.vertical_magnetic_flux_time_deriv_horizontal_loop(t, sigma=1.0, mu=1.25663706212e-06, radius=1.0, current=1.0, turns=1)#
Time-derivative of the vertical transient magnetic flux density at the center of a horizontal loop over a halfspace.
Compute the time-derivative of the vertical component of the transient magnetic flux density at the center of a circular loop on the surface of a conductive and magnetically permeable halfspace.
- Parameters:
- tfloat, or numpy.ndarray
- sigmafloat, optional
conductivity
- mufloat, optional
magnetic permeability
- radiusfloat, optional
radius of the horizontal loop
- currentfloat, optional
current of the horizontal loop
- turnsint, optional
number of turns in the horizontal loop
- Returns:
- dbz_dtfloat, or numpy.ndarray
The vertical magnetic flux time derivative at the center of the loop. The shape will match the t input.
Examples
Reproducing part of Figure 4.8, scaled by magnetic suscpetibility, from Ward and Hohmann 1988.
>>> import numpy as np >>> import matplotlib.pyplot as plt >>> from geoana.em.tdem import vertical_magnetic_flux_time_deriv_horizontal_loop
Calculate the field at the time given
>>> times = np.logspace(-7, -1) >>> dbz_dt = vertical_magnetic_flux_time_deriv_horizontal_loop(times, sigma=1E-2, radius=50)
Match the vertical magnetic field plot
>>> plt.loglog(times*1E3, -dbz_dt, '--') >>> plt.xlabel('time (ms)') >>> plt.ylabel(r'$\frac{\partial b_z}{ \partial t}$ (T/s)') >>> plt.show()
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Source code
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