Field trials using HTS SQUID magnetometers for ground-based and airborne geophysical applications

Since December 1992, CSIRO and BHP have been field trialing rf HTS SQUID magnetometers for mineral prospecting applications. Ten field trials in widely varying environments(from -16/spl deg/C to +40/spl deg/C ambient temperatures) in mostly remote locations saw the development of a system which can...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:IEEE transactions on applied superconductivity 1999-06, Vol.9 (2), p.3786-3792
Hauptverfasser: Foley, C.P., Leslie, K.E., Binks, R., Lewis, C., Murray, W., Sloggett, G.J., Lam, S., Sankrithyan, B., Savvides, N., Katzaros, A., Muller, K.-H., Mitchell, E.E., Pollock, J., Lee, J., Dart, D.L., Barrow, R.R., Asten, M., Maddever, A., Panjkovic, G., Downey, M., Hoffman, C., Turner, R.
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext bestellen
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
Beschreibung
Zusammenfassung:Since December 1992, CSIRO and BHP have been field trialing rf HTS SQUID magnetometers for mineral prospecting applications. Ten field trials in widely varying environments(from -16/spl deg/C to +40/spl deg/C ambient temperatures) in mostly remote locations saw the development of a system which can be operated in many configurations including ground based and airborne Transient ElectroMagnetics (TEM). The magnetometer system has been developed to a point where, at late times in TEM applications, the SQUID system has a higher signal-to-noise level than the competing traditional coil technology. In some trials, a SQUID magnetometer detected anomalies at later times than were observed with the coil system, indicating an enhanced ability to detect highly conductive targets. This paper reviews development of our 3-axis SQUID magnetometer. SQUID systems as B field sensors have advantages over coils which are dB/dt type sensors. We will discuss the importance of these advantages for mineral prospecting in regions with a conducting soil cover or overburden typical of the Australian landscape.
ISSN:1051-8223
1558-2515
DOI:10.1109/77.783852