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  5. Environmental magneto-gradiometric marine survey in a highly anthropic noisy area
 
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Environmental magneto-gradiometric marine survey in a highly anthropic noisy area

Author(s)
Embriaco, D.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Carmisciano, C.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Caratori Tontini, F.  
Stefanelli, P.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Cocchi, L.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
Locritani, M.  
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia  
De Marte, M.  
Istituto Idrografico della Marina Militare, Genova, Italy  
Language
English
Obiettivo Specifico
1.8. Osservazioni di geofisica ambientale
Status
Published
JCR Journal
JCR Journal
Peer review journal
Yes
Journal
Annals of Geophysics  
Issue/vol(year)
5/52 (2009)
Publisher
INGV
Pages (printed)
459-467
Date Issued
October 2009
URI
https://www.earth-prints.org/handle/2122/5671
Subjects
04. Solid Earth::04.01. Earth Interior::04.01.99. General or miscellaneous  
04. Solid Earth::04.05. Geomagnetism::04.05.99. General or miscellaneous  
04. Solid Earth::04.05. Geomagnetism::04.05.09. Environmental magnetism  
Subjects

environmental reclama...

anthropic noise

magneto-gradiometric ...

Abstract
We describe a magneto-gradiometric survey performed in the «Mar Piccolo» of Taranto, Italy in May 2005 for environmental purposes. This region, which is a noisy harbour environment, provides a challenging test for magnetic methods. To reduce spurious noise signals, with both temporal and spatial origins, we used two Geometrics
G880 model caesium magnetometers towed in a transverse gradient configuration. We show how, in shallow waters, this gradiometric configuration allows us to distinguish anomalies due to small metallic bodies near
the seabed from the induced noise due to the anthropic contribution and geomagnetic field variations. A direct visual inspection confirmed that the peculiarities highlighted in the gradient anomaly map were due to abandoned metallic objects found on the seabed.
References
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