P. Schmoldt, PhD - MTNet - DIAS

P. Schmoldt, PhD - MTNet - DIAS P. Schmoldt, PhD - MTNet - DIAS

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3. Mathematical description of electromagnetic relations Reducing F0 in Equation 3.51, applying the natural logarithm to both sides, followed by a multiplication by (−1) yields With Equation 3.43 this results in 1 = Re(kn)t ′ n−1 n + Re(ki)ti i=1 ⇔t ′ 1 n = Re(kn) − 1 n−1 Re(ki)ti. Re(kn) t ′ n = ρnT πµn − n−1 i=1 i=1 µiρn µnρi (3.52) ti. (3.53) Hence, the skin depth can be calculated for the case of a known 1D subsurface model with n-layers using ρnT n−1 µiρn δs = + dn−1 − ti, πµn µnρi (3.54) with dn−1 denoting the depth to the bottom of the layer n − 1, and ρi, µi, and ti are the resistivity, permeability, and thickness of the i-th layer, respectively. With the assumptions used for Equation 3.45 this yields: δs ≈ 0.5 ρnT + dn−1 − n−1 i=1 i=1 µiρn ti [km]; (3.55) µnρi and with the assumption that µi = µn = µ0 for all layers (cf. Sec. 3.5) Equation 3.55 further reduces to δs ≈ 0.5 ρnT + dn−1 − √ ρn 3.4. Boundary conditions n−1 i=1 ti √ ρi [km]. (3.56) The use of the so-called halfspace case is purely an idealistic principle and is never obtained in practice for a variety of reasons, such as the long periods used and hence the large area of induction (Sec. 3.3). Usually changes of conductivity, due to variations in composition or condition, are sensed vertically and at minimum in one horizontal direction; at the very least, the air-ground interface is always present in MT data. Furthermore, as MT is often superior to other deep-probing methods, like seismic tomography, in detection of vertical interfaces and therefore in determining the distribution of subsurface 40

3.4. Boundary conditions materials and their condition, it is important to examine the effects of such conductivity interfaces on the electric current and EM fields. From Maxwell’s Equations (Eqs. 3.1 - 3.4), with the aid of Stokes’ and Gauss’ theorems (Eqs. 3.6 and 3.7), it becomes immediately evident that the relationship for EM fields and electric currents on conductivity interfaces are such as given in Table 3.2. In Continuity on conductivity interface Component Normal Transverse B H E D Field El. current Normal Transverse J Tab. 3.2.: Behaviour of electromagnetic fields and electric current on conductivity interfaces with their components in regards to the orientation of the interface. summary, the magnetic fields B and hence the magnetic field strength H are constant on conductivity interfaces (presuming no magnetic permeability variation along with the conductivity change). The electric current J exhibits a continuous normal and a discontinuous transverse component, and since the electric field E is related to the current via the local conductivity as described by Ohm’s Law (Eq. 3.5) its behaviour is exactly opposite (and so is the electric displacement fields D, presuming constant permittivity). The relation between the electric components of two areas can be given in a form similar to Snell’s Law, i.e. and J1T J2T E1N E2N = σ1ET σ2ET = σ2JN σ1JN = σ1 σ2 = σ2 σ1 = ρ2 ρ1 = ρ1 ρ2 = tan(α1) , (3.57) tan(α2) = tan(α2) , (3.58) tan(α1) with αi representing the angles between the flow lines of electric current and a vector normal to the conductivity interface. 3.4.1. Horizontal interfaces To illustrate the effect of horizontal interfaces on MT observations consider a layered subsurface with Q layers, hence Q interfaces (including the air-surface interface at depth z = 0). In each of the first Q-1 layers the general form of the EM fields as described in Equation 3.20 is valid, including the upward term F1, whereas in the bottom half-space 41

3.4. Boundary conditions<br />

materials and their condition, it is important to examine the effects of such conductivity<br />

interfaces on the electric current and EM fields.<br />

From Maxwell’s Equations (Eqs. 3.1 - 3.4), with the aid of Stokes’ and Gauss’ theorems<br />

(Eqs. 3.6 and 3.7), it becomes immediately evident that the relationship for EM<br />

fields and electric currents on conductivity interfaces are such as given in Table 3.2. In<br />

Continuity on conductivity interface<br />

Component<br />

Normal Transverse<br />

B <br />

H <br />

E <br />

D <br />

Field<br />

El. current Normal Transverse<br />

J <br />

Tab. 3.2.: Behaviour of electromagnetic fields and electric current on conductivity interfaces with their components in regards to the<br />

orientation of the interface.<br />

summary, the magnetic fields B and hence the magnetic field strength H are constant<br />

on conductivity interfaces (presuming no magnetic permeability variation along with the<br />

conductivity change). The electric current J exhibits a continuous normal and a discontinuous<br />

transverse component, and since the electric field E is related to the current via<br />

the local conductivity as described by Ohm’s Law (Eq. 3.5) its behaviour is exactly opposite<br />

(and so is the electric displacement fields D, presuming constant permittivity). The<br />

relation between the electric components of two areas can be given in a form similar to<br />

Snell’s Law, i.e.<br />

and<br />

J1T<br />

J2T<br />

E1N<br />

E2N<br />

= σ1ET<br />

σ2ET<br />

= σ2JN<br />

σ1JN<br />

= σ1<br />

σ2<br />

= σ2<br />

σ1<br />

= ρ2<br />

ρ1<br />

= ρ1<br />

ρ2<br />

= tan(α1)<br />

, (3.57)<br />

tan(α2)<br />

= tan(α2)<br />

, (3.58)<br />

tan(α1)<br />

with αi representing the angles between the flow lines of electric current and a vector<br />

normal to the conductivity interface.<br />

3.4.1. Horizontal interfaces<br />

To illustrate the effect of horizontal interfaces on MT observations consider a layered<br />

subsurface with Q layers, hence Q interfaces (including the air-surface interface at depth<br />

z = 0). In each of the first Q-1 layers the general form of the EM fields as described in<br />

Equation 3.20 is valid, including the upward term F1, whereas in the bottom half-space<br />

41

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