2020
DOI: 10.3390/geosciences10100382
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Dreaming of Perfect Data: Characterizing Noise in Archaeo-Geophysical Measurements

Abstract: For the interpretation of archaeological geophysical data as archaeological features, it is essential that the recorded anomalies can be clearly delineated and analyzed, and therefore, care has been taken to obtain the best possible data. However, as with all measurements, data are degraded by unwanted components, or noise. This review clarifies the terminology, discusses the four major sources of noise (instrument, use of instrument, external, soil), and demonstrates how it can be characterized using geostati… Show more

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Cited by 24 publications
(14 citation statements)
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“…In Figure 6, three texture attributes [39] were calculated on the same depth-slice. It is remarkable to notice that attributes have a strong potential, but are very sensitive to the SNR, which is often low in GPR datasets of archaeological sites [45]. Some attributes (such as the Chaos one) are able to highlight not only the edge of buried structures, but also their extension.…”
Section: Resultsmentioning
confidence: 99%
“…In Figure 6, three texture attributes [39] were calculated on the same depth-slice. It is remarkable to notice that attributes have a strong potential, but are very sensitive to the SNR, which is often low in GPR datasets of archaeological sites [45]. Some attributes (such as the Chaos one) are able to highlight not only the edge of buried structures, but also their extension.…”
Section: Resultsmentioning
confidence: 99%
“…This might indicate a greater thickness of the soil superimposed over archaeological features, which would explain the weaker response from these structures captured by the magnetometer. Also, there are considerable sources of noise located nearby, which additionally hinder the interpretation of this part of the magnetic map (Schmidt et al, 2020: 12–3).…”
Section: Discussionmentioning
confidence: 99%
“…The soil and sedimentological analyses were focused on a basic characteris the subsurface materials present with regard to properties such as particle size d tion and organic matter content, which are pivotal to the soil water infiltration, r properties, and drainage processes (Tables 3 and 4, see also Section 1.1). Monito tions 2 and 3 have no registered archaeological features, and therefore serve as re for the soil and sediment properties on the site, particularly with regard to the to Revisiting the depth-slices with this in mind, it seems that the level of background noise (background noise refers here to all unwanted elements in the GPR data including deviations from the desired signal attributable to the device used, to external sources as well as to what is sometimes called "soil noise" [35])-which, if high, can make the data interpretation significantly more difficult-increases the level of contrast, which is reflected by the higher standard deviation values of the respective depth-slice. Depth-slices showing a more homogenous background, in turn, imply a lower contrast and indeed show lower standard deviations, however, the lower noise levels in the background ultimately facilitate an interpretation of the archaeological features.…”
Section: Soil and Sedimentological Analysesmentioning
confidence: 99%