Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

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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

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

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