Earth Electromagnetic Properties
Plate Tectonics to Pore Fluids (Plates to Pores)

George R. Jiracek- San Diego State University

 

1.7 Complex EM Properties

For many geophysical applications we neglect the permittivity (ε or K) term and assume the magnetic permeability is that of free space, i.e., Km = 1. This cannot be done for ground penetrating radar, GPR. In this case we must treat the total current density, JT as

JT = JC +D/t. (1.7.1)

Here, JC is the same current density, J defined earlier, however, in the context here it is usually referred to as the conduction current density to distinguish it from the displacement current density, ∂D/∂t.

By assuming that the time dependency of all fields is e+iωt we see that

JT = JC + iωD (1.7.2)
= (σ + iωε)E. (1.7.3)

(Using the exponential, e+iωt to express a sinusoidal time variation with time is discussed in Appendix B). Equation 1.7.3 allows a generalized complex expression of Ohm's law (equation 1.5.1). This uses the definition of complex conductivity, σ* as

σ* = σ' + iσ'' (1.7.4)

and yields

JT = σ*E, (1.7.5)

 

where σ' = σ and σ'' = ωε are the real and imaginary parts of the complex conductivity, σ* respectively. A convenient way to express the relative amount of conduction current versus displacement current is the loss tangent, tan δ.

tan δ = σ / ωε =
conduction current density
displacement current density
(1.7.6)

Another way to express JT is to modify the JT equation 1.7.3 above as

JT = iω(σ/ + e)E  
  = iω(ε - iσ/ ω)E  
  = iωε*E (1.7.7)

This leads to the definition of complex electric permittivity, ε* (von Hippel, 1954) as

ε * = ε' – iε'' , (1.7.8)

where ε' and ε'' are the real and imaginary parts of the complex permittivity, ε*, respectively. This allows the alternate expression of the loss tangent to be

tan δ = ε'' / ε' (1.7.9)

The complex dielectric constant, K* follows as

K* = ε*/ε0  
  = K' – iK''. (1.7.10)

Davis and Annan (1989) prefer to separate the imaginary part of the dielectric constant into two parts: 1) a dc component of conductivity σdc and 2) a high frequency contribution, K''. Then

K* = K' – iK'''  
  = K' + i(K'' + σdc/ωε0) (1.7.11)

The relations above can be represented in the complex plane. Figure 1.9 a, b, and c contain such examples.

a)
b)
c)
Image Image Image

Figure 1.9 Complex graphical representations of a) total current density, JT, b) conductivity, σ*, and c) dielectric constant, K*.