Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
where the subscripts "en and "i" denote the parts of external and internal origin at z = o. Further, let the Fourier transform of any one of the above six - ~ K Y dy. quantities be A 1 +m _ H(K) = - J H(y,o)e 2~ -m Then (5.4a,b) yields A A A A H /xZe =.-i Ye Y 1 sgn (K) , H . /HZi = +isynCK) (5.7alb) A product between Fourier transforms in the x-domain transforms to a convolution integral in the y-domain: Hence we obtain from (5.7aIb1 - . - -. H =+KxHze, H . = -I< x Ye Yl Hzi -. - - . = - K x H H =+ICxH 'ze ye' z i. .yi - €*K Convergence was forced by a factor e . The resulting convolution integral exists only in the sense of a Cauchy principzl val-ue, i..e. (5.8a) for example reads explicitly +m . - H (y) = 1 K (~-~)IX~~(TI)~~ Ye -m
The four equations A A A A H = i sgn (K) HZe , H = + isign(~) H Ye Y i z i A A A A can easily be solved for H yer Hze' $ir 'zi* When transformed into the y-domain it results 4 I Two-dimensional separation formulae I For practisal purpuses these separation formulae are not very con- venient, since the kernel decays rather slowly requiring a long profile to determine the internal and external part at a given ' surface point. 5.2. Conversion - formulae for the field components - of a two- - dimensional TE-fielci at the surface of a one-dimensional structure For the separation of the magnetic field components no knowledge of the two-dimensional conductivity structure is required. However, the conductivity enters if it is attempted to deduce for instance r the total ver-tical component of the magnetic field at the surface from *he corresponding tangential componenk. If the conductivity structure is one-dimensional, the conversicn between two component.: can be effected using a convolution integral, where the kernel is derived from the one-dimensional structure via the trans5er funs- '?here S([K[,W) is the ratio between internal and external part of A h H i.e. H . /H in the frequency wavenuder domain. Y' Yl yer From (5.9a-c) the,yarious conversion formuias for the durface com!31 nents can be derived. The following table gives the definition of
- Page 13 and 14: a) TM-mode From (2.251, (2.26); (2.
- Page 15 and 16: with " the abbreviation + - 1 - ? =
- Page 17 and 18: 2n -i~cr cos (8-$1 -iKrcU J e ~B=J
- Page 19 and 20: In the 1irnl.t a -+ o, I +- m, M =
- Page 21 and 22: -- 2.5. Definition -- of the transf
- Page 23 and 24: we arrive at - v The same appl-ies
- Page 25 and 26: ) Computation of ---- C for a laxez
- Page 27 and 28: The approximate interpretation of C
- Page 29 and 30: I ~ispersi-on relations I Dispersio
- Page 31 and 32: where L is a positively oriented cl
- Page 33 and 34: 1 2 3 4 CPD 1 2 3 4 CPD - g) Depend
- Page 35 and 36: The TE-mode has no vertical electri
- Page 37 and 38: i I Earth Anomalous domain 3.2. Air
- Page 39 and 40: Hence, the conductivity is to be av
- Page 41 and 42: The RHS i.s a closed line integral
- Page 43 and 44: 4. Having determined B;, the coeffi
- Page 45 and 46: 3.4. Anomalous region as basic doma
- Page 47 and 48: - 6 and 6= can be so adjusted that
- Page 49 and 50: From the generalized Green's theore
- Page 51 and 52: and y can again be so adjusted that
- Page 53 and 54: 4.2. In3ral - --- equation method L
- Page 55 and 56: The element GZx is needed for all z
- Page 57 and 58: With this knowledge of the behaviou
- Page 59 and 60: After having determined Qzr VJ,; @,
- Page 61 and 62: 4.3. The surface inteyral approach
- Page 63: F At the vertical boundaries the co
- Page 68 and 69: 6. Approaches to the inverse proble
- Page 70 and 71: to minimize the quantity a s = 12 /
- Page 72 and 73: It remains to show a way to minimiz
- Page 74 and 75: Agai-n, from a finite erroneous dat
- Page 76 and 77: Here lJ - is a N x P matrix contain
- Page 78 and 79: small eigenvalues. The parameter ve
- Page 80 and 81: Then - 77 - A(E2 - E ) = iwu U (E -
- Page 82 and 83: whence 2k d -2k d where a = CA:(A;)
- Page 84 and 85: . 7. Basic concepts of geomagnetic
- Page 86 and 87: orders of magnitude smaller' than t
- Page 88 and 89: Elimination of - E or .,. H yields
- Page 90 and 91: Observing that rot pot rot g = - ro
- Page 92 and 93: Two special types of such anomalies
- Page 94 and 95: Model : wo+ Solution for uniform ha
- Page 96 and 97: parameter u and that the pressure d
- Page 98 and 99: (=disturbed)-variations: After magn
- Page 100 and 101: with 4 as geographic latitude. From
- Page 102 and 103: Very rapid oscillations with freque
- Page 104 and 105: ! 8. Data Collection - and Analysis
- Page 106 and 107: A horizontal electric -- field comp
- Page 108 and 109: For a data reducti.on in the fr3equ
- Page 110 and 111: Let q be the tranfer function betwe
- Page 112 and 113: . A as transfer function between A
The four equations<br />
A A A A<br />
H = i sgn (K) HZe , H = + isign(~) H<br />
Ye Y i z i<br />
A A A A<br />
can easily be solved for H yer Hze' $ir 'zi*<br />
When transformed into the y-domain it results 4<br />
I Two-dimensional separation formulae I<br />
For practisal purpuses these separation formulae are not very con-<br />
venient, since the kernel decays rather slowly requiring a long<br />
profile to determine the internal and external part at a given '<br />
surface point.<br />
5.2. Conversion - formulae for the field components - of a two- -<br />
dimensional TE-fielci at the surface of a one-dimensional structure<br />
For the separation of the magnetic field components no knowledge<br />
of the two-dimensional conductivity structure is required. However,<br />
the conductivity enters if it is attempted to deduce for instance<br />
r<br />
the total ver-tical component of the magnetic field at the surface<br />
from *he corresponding tangential componenk. If the conductivity<br />
structure is one-dimensional, the conversicn between two component.:<br />
can be effected using a convolution integral, where the kernel is<br />
derived from the one-dimensional structure via the trans5er funs-<br />
'?here S([K[,W) is the ratio between internal and external part of<br />
A h<br />
H i.e. H . /H in the frequency wavenuder domain.<br />
Y' Yl yer<br />
From (5.9a-c) the,yarious conversion formuias for the durface com!31<br />
nents can be derived. The following table gives the definition of