2011
DOI: 10.1002/arp.409
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Integrated Geophysical and Archaeological Investigations of Aquinum in Frosinone, Italy

Abstract: To better understand the location and help in the conservation of buried structures at the ancient site of Aquinum in central Italy, integrated archaeological and geophysical data were acquired. These datasets included historical and oblique aerial photographs, which were combined with topographical and archaeological field-walking survey. These data showed the general location of the Roman town Aquinum. To verify preliminary interpretations groundpenetrating radar (GPR) data were collected in an open area of … Show more

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Cited by 13 publications
(6 citation statements)
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“…Neubauer et al ., ), single‐antenna instruments are still widely used, and the comparison of a few recent single‐antenna surveys shows a large variation in the profile spacing. It ranges from 0.1 m to 0.5 m, or from ~0.25 to ~4.25 times the dominant wavelength of the antenna (Böniger and Tronicke, ; Piro et al ., ; Novo et al ., ; Rogers et al ., ; Leucci et al ., ). Determination of the proper transect spacing is important because too coarse a sample interval causes aliasing: in the samples measured, high wavenumbers originating from diffractions with steep dips are misrepresented by lower wavenumbers (Yilmaz, ), so that the signal is distorted and the image of the buried archaeological structures can no longer be reconstructed unambiguously from the samples.…”
Section: Introductionmentioning
confidence: 99%
“…Neubauer et al ., ), single‐antenna instruments are still widely used, and the comparison of a few recent single‐antenna surveys shows a large variation in the profile spacing. It ranges from 0.1 m to 0.5 m, or from ~0.25 to ~4.25 times the dominant wavelength of the antenna (Böniger and Tronicke, ; Piro et al ., ; Novo et al ., ; Rogers et al ., ; Leucci et al ., ). Determination of the proper transect spacing is important because too coarse a sample interval causes aliasing: in the samples measured, high wavenumbers originating from diffractions with steep dips are misrepresented by lower wavenumbers (Yilmaz, ), so that the signal is distorted and the image of the buried archaeological structures can no longer be reconstructed unambiguously from the samples.…”
Section: Introductionmentioning
confidence: 99%
“…Among various active geophysical techniques, electric and electromagnetic (em) methods are strongly effective for the detection of archaeological features located in the subsoil at different depths and scenarios [1][2][3][4][5][6][7]. Localization of anthropic structures placed in the soil is possible due to the contrast of the em physical properties between the materials constituting the buried objects and the subsoil where they are "preserved".…”
Section: Introductionmentioning
confidence: 99%
“…Depending on the inequalities between the emitted and received signal, various anomalies can be shown [25]. GPR has been used to discover previously unknown constructions [26][27] and provide useful information for the identification and characterization of archaeological remains buried at different depths [28].…”
Section: Introductionmentioning
confidence: 99%