2009
DOI: 10.4000/archeosciences.1790
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3D Inversion of Automated Resistivity Profiling (ARP) Data

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Cited by 4 publications
(4 citation statements)
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“…Comparing the ERT results and pseudo-sections, it is possible to observe a good agreement of depths for apparent interfaces and spatial resistivity transients, with a slight overestimation of depths under conductive volumes. A similar behavior is also described by Papadopoulos et al [39,40]. Combining ARP, 0.50 m depth, with DTM data (Figure 15), it is possible to evaluate the independence and spatial relations of the widest ARP anomalies to each other.…”
Section: Discussionsupporting
confidence: 73%
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“…Comparing the ERT results and pseudo-sections, it is possible to observe a good agreement of depths for apparent interfaces and spatial resistivity transients, with a slight overestimation of depths under conductive volumes. A similar behavior is also described by Papadopoulos et al [39,40]. Combining ARP, 0.50 m depth, with DTM data (Figure 15), it is possible to evaluate the independence and spatial relations of the widest ARP anomalies to each other.…”
Section: Discussionsupporting
confidence: 73%
“…This electrode array is designed to obtain simultaneously measurements of apparent resistivity simultaneously at three different subsoil depths. Papadopoulos et al [39,40] described a three-dimensional inversion of resistivity data acquired with the ARP system in order to obtain a reliable numerical model capable of describing the spatial distribution of the electrical resistivity in the subsoil of the investigated area. The inversion process described by the authors is based on the least squares method and establishes smoothness constraints in order to consider the instability of the model and the non-uniqueness of solutions [41].…”
Section: Introductionmentioning
confidence: 99%
“…The purpose of electrical resistivity surveys is to determine underground resistivity contrasts by making measurements on the ground surface, which result in electrical anomalies of subsurface materials [7]. Electrical resistivity imaging has been developed to create accurate 2-D and 3-D computational resistivity models of subsurface cross-sections [9? ], and [10]. In all resistivity surveys electrode configuration plays an important role in determination of output resolution and depth of investigation.…”
Section: Introductionmentioning
confidence: 99%
“…Recent developments in survey technology focus on flexible single devices, which use several sensors of one type on mobile platforms. The most widely‐used methods in archaeological geophysics are magnetic gradiometer surveys (MGS), ground‐penetrating radar (GPR) and electrical resistivity imaging or tomography (ERI or ERT, see Leckebusch, ; Erkul et al ., , ; Schultze et al ., ; Gaffney, ; Papadopoulus et al ., ; Rabbel et al ., , and references cited therein).…”
Section: Introductionmentioning
confidence: 97%