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P. Schmoldt, PhD - MTNet - DIAS

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3. Mathematical description of electromagnetic relations<br />

with ∇: Nabla operator, D: electric displacement field, Qe: electric charge density, E:<br />

electric field, ∂t: partial derivative with respect to time, B: magnetic field, H: magnetising<br />

field, and J f : electric current density of free charges. Maxwell found the four original<br />

laws to be inconsistent and added the so-called Maxwellian term (∂t D) to Ampère’s Law<br />

in order to provide a complete mathematical description of the physical relationship.<br />

3.1.2. Ohm’s Law<br />

Ohm’s Law describes the relationship between electric current J and electric field E for<br />

the case of an ohmic conductor with conductivity σ, viz.<br />

3.1.3. Vector calculus<br />

J = σ E. (3.5)<br />

Stokes theorem relates the rotation of a vector field F on a surface A to the flux of the<br />

vector field through the boundary s of the volume<br />

<br />

<br />

(∇ × F) · n dA = F · τ ds, (3.6)<br />

A<br />

with n and τ denoting the unit normal field and the unit tangential field of the surface,<br />

respectively.<br />

Gauss’s theorem (also referred to divergence theorem) relates the change of a vector<br />

field F inside a volume V to the flux of the vector field through the surface A of the<br />

volume <br />

<br />

(∇ · F) dV = F · n dA, (3.7)<br />

V<br />

with n denoting the outward pointing unit normal field of the volume.<br />

3.2. Deriving magnetotelluric parameters<br />

The relation between electric response of a subsurface to an incident magnetic field is the<br />

key element of MT, as electric conductivity (or its inverse the electric resistivity) can be<br />

derived from the amplitude quotient and phase difference of the EM fields, using basic<br />

equations (Sec. 3.1). Rewriting Equation 3.4 and using Ohm’s Law (Eq. 3.5) for the case<br />

of a homogeneous, isotropic halfspace with use of the constitutive equations<br />

32<br />

A<br />

s<br />

H = B<br />

µ , (3.8)<br />

D = ε E, (3.9)

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