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Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

Schmucker-Weidelt Lecture Notes, Aarhus, 1975 - MTNet

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!<br />

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

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