Schmucker, 1970 (Scripps) - MTNet
Schmucker, 1970 (Scripps) - MTNet
Schmucker, 1970 (Scripps) - MTNet
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2. INS'THUMENTS AND FIELD OPERATIONS<br />
2.1 Askania Variograph<br />
The survey was conducted with six Askania variographs, model Gv3. The<br />
variograph records continuously on 16 mm film the three components of the<br />
transient geomagnetic variations: D (positive magnetic eastward), H (positive<br />
magnetic northward), Z (positive downward). The film speed is 5 mm/hour,<br />
hence a lOO-ft roll is sufficient for about eight months of record.<br />
Providing that the optical system is occasionally readjusted the sharpness<br />
of the traces allows at least 12 -fold magnification, thereby yielding a time<br />
resolution of 1 min/mm in Z. The variometers are of the classical type and<br />
employ suspended magnets in proper orientation. They are mounted inside a<br />
temperature insulated cylindrical container, and an intricate mirror system<br />
gives an effective optical lever of about three meters.<br />
At field sites where AC power is available the variograph can be operated<br />
with thermostat control, requiring 50 watts. If the variograph has to be<br />
operated on batteries, requiring 6 ampere hours/day, temperature compensation<br />
and additional temperature protection of the instrument are essential<br />
when the evaluation of long periodic variation is desired.<br />
Prior to the actual field operations the original sensitivities of the Dvariometer<br />
were doubled to match those of the H-variometer.. For that<br />
purpose a pair of compensation magnets were installed near the D-system to<br />
bias the horizontal magnetic field intensity. Since transient fluctuations in Z<br />
would be of particular importance during the survey, the sensitivity of the<br />
Z -variometer was also increased by adding a small coil of thin copper wire<br />
as trimmer weight to the system. This trimmer weight lifted the center of<br />
mass of the suspended Z-system closer to its axis of rotation, thereby making<br />
the system less stable.<br />
2.2 Intercalibration of the Variographs<br />
The detection and analysis of anomalous variations requires a precise intercomparison<br />
of magnetograms from different instruments at different sites.<br />
Therefore the six variographs were carefully intercalibrated by operating<br />
them side by side for about four months at <strong>Scripps</strong> Institution, La jolla. This<br />
test has been conducted twice, at the beginning and in the middle of the program.<br />
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