Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet
I '. - L.. . . - I . --.> . ~ 4 The transfer function between the anomal.ous and normal field are now readily expressed in terms of a frequency-dependent . response function, a frequency-independmt geometric factor, and a frequency-dependent attenua-tion factor Q' for the normal field: wi-th Q' = (1 4. i nZ)-' , An approximate so1.ution of problem (ii) can be obtained by re- presenting the conductive substructure below the surface sheet by a perfect conductor at the (frequency-dependent) depth K~(C;) and by adding to the anomalous dipole field the field of an image dipo1.e of the moment R ~H;~ at the depth 2sRe(~i)-z~.
Problem (iii) j.nvol.ves mainly the attenuation of the upward diffusj.ng anomaly ca by ' uniform surface layers. This a.tte.iiuatri.on is, however, a second order effect and can be neglected, if at the considered frequency the widespread normal fieid pene- trates the surface layers to any extent, i.e. if the modulus of Q' is sufficiently close to unity. The inverse problem: Assuming the anomalous body to be a uniform cylinder, the model parameters zo,'R, cr can be uniquely in- R ferred from surface observations, providing the transfer func- tions for H and FIaz are known for at least two locations and aY frequencies. For.ming here the ra-tios the angles 8 and thereby the position- of the cylinder can be found, The depth of the cylinder axis being kncwn; the dipole moment RZf(n) can be calculated. Its argument fixes the size of the induction parameter n and two determinations of nZ at z different frequencies the radius R and -the conductivi-ty crz. NOW R and zo being known, the field of the image dipole can be cal-- culated. The inverse procedure is repeated now with the observed surface anomaly minus the field of the image dipole until con-. vergence of the model parameters has been reached. Interpretation with HIOT--SAVART1s law . . ~ Let - f he the current density vector within a volume dV at the Q n n h point - r = (x, y, z). Then according to UZUT-SAVART1s law in SI units -the magnetic fieled vector at: the point - r = (x, y , z) due c' to the line-current element idV is
- Page 116 and 117: Since it follows that - E 1 = - T E
- Page 118 and 119: - - . the same or from different si
- Page 120 and 121: The Fourier integral - +- -io t T -
- Page 122 and 123: The weigh-t . function W is then fo
- Page 124 and 125: Two convenient filters are 3 sinx I
- Page 126 and 127: (e.g. X), their realizations by obs
- Page 128 and 129: Observe that the residual, of which
- Page 130 and 131: Example: n = 12 and @ = 95%: 1 n =
- Page 132 and 133: - As a consequence, the real and im
- Page 134 and 135: This relati-on implies .that .the l
- Page 136 and 137: 9. --- Data 5.nterpretatj.on on the
- Page 138 and 139: The "modified apparent - - resistiv
- Page 140 and 141: Exercise Geomagne-tic varj.ations.
- Page 142 and 143: 9.2 Layered Sphere - The sphericity
- Page 144 and 145: The field within the conducting sph
- Page 146 and 147: and An algorithm for the direct pro
- Page 148 and 149: with I - and- a = gn g-n I 1 6-n-1
- Page 150 and 151: with ~ = - T E + as sheet current d
- Page 152 and 153: E~~ T r: j = const. or E T + E a r
- Page 154 and 155: Field equations and boundary condit
- Page 156 and 157: with N (w,y) being the Fourier tran
- Page 158 and 159: is calculated as function of freque
- Page 160 and 161: Both types of anomaly can be explai
- Page 162 and 163: A field line segment with the horiz
- Page 164 and 165: - 160 - below can neither enter nor
- Page 168 and 169: This law can be used to i-nterpret
- Page 170 and 171: Only in this special case will be j
- Page 172 and 173: anomalous conductivity oat OP the a
- Page 174 and 175: the product WUL' constant with L de
- Page 176 and 177: One of the thin plates represents t
- Page 178 and 179: low conductivity requires the use o
- Page 180 and 181: Other derivable properties of mantl
- Page 182: 11. References for general reading
Problem (iii) j.nvol.ves mainly the attenuation of the upward<br />
diffusj.ng anomaly ca by ' uniform surface layers. This a.tte.iiuatri.on<br />
is, however, a second order effect and can be neglected, if<br />
at the considered frequency the widespread normal fieid pene-<br />
trates the surface layers to any extent, i.e. if the modulus<br />
of Q' is sufficiently close to unity.<br />
The inverse problem: Assuming the anomalous body to be a uniform<br />
cylinder, the model parameters zo,'R, cr can be uniquely in-<br />
R<br />
ferred from surface observations, providing the transfer func-<br />
tions for H and FIaz are known for at least two locations and<br />
aY<br />
frequencies. For.ming here the ra-tios<br />
the angles 8 and thereby the position- of the cylinder can be<br />
found, The depth of the cylinder axis being kncwn; the dipole<br />
moment RZf(n) can be calculated. Its argument fixes the size<br />
of the induction parameter n and two determinations of nZ at z<br />
different frequencies the radius R and -the conductivi-ty crz. NOW<br />
R and zo being known, the field of the image dipole can be cal--<br />
culated. The inverse procedure is repeated now with the observed<br />
surface anomaly minus the field of the image dipole until con-.<br />
vergence of the model parameters has been reached.<br />
Interpretation with HIOT--SAVART1s law<br />
. . ~<br />
Let - f he the current density vector within a volume dV at the<br />
Q n n h<br />
point - r = (x, y, z). Then according to UZUT-SAVART1s law in SI<br />
units -the magnetic fieled vector at: the point - r = (x, y , z) due<br />
c'<br />
to the line-current element idV is