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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8. Data Collection - and Analysis<br />
8.1 Instruments -<br />
unetic sensors for geomagnetic induction work on land should meet<br />
as many as possi-ble of the following requirements:<br />
(1) Sufficient sensitivity and time resolution<br />
(2) Directional characteristics which allow observation of the<br />
magnetic variation vector in well-defined, preferably ortho-<br />
gonal components.<br />
(3) Stable compensation of the Earth's permanent field, if re-<br />
quired. The sensors should not show "drift" on a time scale<br />
comparable to the slowest variati-ons to be analysed.<br />
(4) Compensation of temperature effects or linear temperature de-<br />
pendence with well defined temperature coefficients for subse-<br />
quent corrections.<br />
C5) Low power consumpti.on to allow field operations on 57et or dry-<br />
cell batteries (less than 100 n;A at 10 to 20 Volts DC con-<br />
tinuous power drain).<br />
C6 1 Minimurn maintenance, all-owing unattended opera-tions over days,<br />
weeks or months, depending on -the period range to be irlvesti-<br />
gated.<br />
(7) Electric outmpu-t signal, adaptab1.e for digital recording<br />
w<br />
No single sensor system can possib1.y meet all requiremen-ts over thc<br />
full frequency range of natural geornagrletic variations and the<br />
- choice of instruments wil.1 depend on the type of variations under<br />
investigation. They record either the total field M Ho + 6H as<br />
?E<br />
sum of -tl;e s-teady field Ho and the variation field 6H, by coml2ensa.-<br />
tion of Ho, the time--derivative fl : 6f'i or a combina-tion of 61.1 nil<br />
x*<br />
& i1. In geomagnetic latitudes the spectral amplitude distr.Lbution of<br />
6H and 611, averagedoverextended perioss of moderate ma~c5tj.c acti-<br />
vity, is the following:<br />
x the variation field 6H only