2016
DOI: 10.5194/gi-5-181-2016
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Magnetic airborne survey – geophysical flight

Abstract: Abstract. This paper provides a technical review process in the area of airborne acquisition of geophysical data, with emphasis for magnetometry. In summary, it addresses the calibration processes of geophysical equipment as well as the aircraft to minimize possible errors in measurements. The corrections used in data processing and filtering are demonstrated with the same results as well as the evolution of these techniques in Brazil and worldwide.

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Cited by 14 publications
(4 citation statements)
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References 15 publications
(20 reference statements)
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“…where C m = 10 −7 is a scale factor, the prime at each coordinate denotes the position of the differential volume element dv of magnetized material, and the components of M are referred with respect to the International Geomagnetic Reference Field (IGRF) [27]. M = χH = χ(H 0 + H a ) ≈ χH 0 , where χ is the magnetic susceptibility of a linear, isotropic and homogeneous material, H 0 is the auxiliary Earth's magnetic field (H 0 = B 0 /µ 0 , where µ 0 is vacuum's magnetic permeability), and H a is the auxiliary magnetic field generated by rocks, which is usually negligible for most magnetic rocks in Earth's crust.…”
Section: Potential Field Theorymentioning
confidence: 99%
See 1 more Smart Citation
“…where C m = 10 −7 is a scale factor, the prime at each coordinate denotes the position of the differential volume element dv of magnetized material, and the components of M are referred with respect to the International Geomagnetic Reference Field (IGRF) [27]. M = χH = χ(H 0 + H a ) ≈ χH 0 , where χ is the magnetic susceptibility of a linear, isotropic and homogeneous material, H 0 is the auxiliary Earth's magnetic field (H 0 = B 0 /µ 0 , where µ 0 is vacuum's magnetic permeability), and H a is the auxiliary magnetic field generated by rocks, which is usually negligible for most magnetic rocks in Earth's crust.…”
Section: Potential Field Theorymentioning
confidence: 99%
“…Since the gradiometric tensor G is symmetric and traceless, its independent components allow determination of the locations of the mass center (G xz , G yz ), edges (G yy , G xx ) and corners (G xy ) of the anomaly; G zz provides the correct spatial position of the anomaly, above the geological mass center, as conventional gravity [16][17][18][19][20][21][22][23][24][25][26]. On the other side, magnetometry is sensitive to anomalies of parts-per-million, making of it a very sensitive tool of geophysical surveying [27].…”
Section: Introductionmentioning
confidence: 99%
“…This often results in a compromise between UAS interference and boom length: a longer boom reduces interference but increases flight instability. Additional mitigation methods such as compensation using coils or rings (Leliak, 1961), shielding using permalloy (Leliak, 1961;Telford et al, 1990), demagnetization using a degaussing coil (Camara and Guimarães, 2016;Versteeg et al, 2007), optimal source positioning strategies (Forrester et al, 2014;Huq et al, 2015), or component replacement have been used. An effective way to deal with high-frequency interference is to sample at higher rates than the interference and remove with pre-filtering (Pharr and Humphreys, 2010); this method has been previously suggested for UAS magnetic interference mitigation (Versteeg et al, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…as compensation using coils or rings (Leliak, 1961), shielding using permalloy (Leliak, 1961;Telford et al, 1990), demagnetisation using a degaussing coil (Camara and Guimarães, 2016;Tuck et al, 2019;Versteeg et al, 2007), optimal source positioning strategies (Forrester et al, 2014;Huq et al, 2015) or component replacement (Versteeg et al, 2007) have been used.…”
Section: Introductionmentioning
confidence: 99%