Electrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary
ABSTRACT A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High‐resolution ERT data were collected along 28 uniformly distributed transects of variable length using the...
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| Published in: | Archaeological prospection Vol. 21; no. 3; pp. 169 - 183 |
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| Language: | English |
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Bognor Regis
Blackwell Publishing Ltd
01.07.2014
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| ISSN: | 1075-2196, 1099-0763 |
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| Abstract | ABSTRACT
A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High‐resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll‐along technique. A recently presented two‐dimensional fast non‐linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross‐sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non‐standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Copyright © 2014 John Wiley & Sons, Ltd. |
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| AbstractList | ABSTRACT
A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High‐resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll‐along technique. A recently presented two‐dimensional fast non‐linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross‐sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non‐standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Copyright © 2014 John Wiley & Sons, Ltd. A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High‐resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll‐along technique. A recently presented two‐dimensional fast non‐linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross‐sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non‐standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Copyright © 2014 John Wiley & Sons, Ltd. A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering an area of almost 6ha. High-resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll-along technique. A recently presented two-dimensional fast non-linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross-sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non-standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Copyright © 2014 John Wiley & Sons, Ltd. [PUBLICATION ABSTRACT] |
| Author | Sarris, Apostolos Duffy, Paul R. Parkinson, William A. Papadopoulos, Nikos G. Yerkes, Richard W. Tsourlos, Panagiotis Gyucha, Attila |
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| Cites_doi | 10.1016/j.jas.2008.07.002 10.1137/0702016 10.1002/arp.1442 10.1002/arp.291 10.1002/arp.423 10.1002/(SICI)1099-0763(199709)4:3<123::AID-ARP76>3.0.CO;2-9 10.1111/j.1365-2478.1990.tb01859.x 10.1002/arp.264 10.1002/arp.234 10.1016/j.jas.2003.12.007 10.1016/j.jas.2012.08.022 10.1111/j.1365-2478.1992.tb00536.x 10.1145/355984.355989 10.1002/arp.414 10.1002/arp.195 10.1017/S0003598X00062530 10.1111/j.1365-2478.2010.00936.x 10.1002/1099-0763(199509)2:3<141::AID-ARP6140020304>3.0.CO;2-V 10.1002/arp.1456 10.1137/10079687X 10.1002/arp.1434 10.1002/arp.335 10.1016/j.jappgeo.2009.12.001 10.1002/(SICI)1099-0763(1998060)5:2<91::AID-ARP97>3.0.CO;2-5 |
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| References | Casana J, Herrmann JT, Fogel A. 2008. Deep subsurface geophysical prospection at Tell Qarqur, Syria. Archaeological Prospection 15: 207-225. Nowaczinski E, Schukraft G, Hecht S, Rassmann K, Bubenzer O, Eitel B. 2012. A multimethodological approach for the investigation of archaeological ditches - exemplified by the Early Bronze Age settlement of Fidvár Near Vráble (Slovakia). Archaeological Prospection 19: 281-295. Křivánek R. 2006. Magnetometric prospection of various types of large ditched enclosures in Bohemia. Archaeological Prospection 13: 25-43. Salisbury R. 2012. Soilscapes and settlements: remote mapping of activity areas in unexcavated prehistoric farmsteads. Antiquity 86: 178-190. Salisbury RB, Bertók G, Bácsmegi G. 2013. Integrated prospection methods to define small-site settlement structure: a case study from Neolithic Hungary. Archaeological Prospection 20(1): 1-10. DOI: 10.1002/arp.1442. Berge MA, Drahor MG. 2011a. 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| References_xml | – reference: Nowaczinski E, Schukraft G, Hecht S, Rassmann K, Bubenzer O, Eitel B. 2012. A multimethodological approach for the investigation of archaeological ditches - exemplified by the Early Bronze Age settlement of Fidvár Near Vráble (Slovakia). Archaeological Prospection 19: 281-295. – reference: Ibrahim EH, Sherief MR, Al-Metwally AA. 1998. Shallow geophysical investigations on Tell el Farama, Northwest Sinai, Egypt. Archaeological Prospection 5: 91-100. – reference: Maillol JM, Ciobotaru DL, Moravetz I. 2004. Electrical and magnetic response of archaeological features at the early Neolithic site of Movila lui Deciov, Western Romania. Archaeological Prospection 11: 213-226. – reference: Sasaki Y. 1992. Resolution of resistivity tomography inferred from numerical simulation. Geophysical Prospecting 40: 453-464. – reference: Tsokas GN, Sarris A, Pappa M, et al. 1997. A large-scale magnetic survey in Makrygialos (Pieria), Greece. Archaeological Prospection 4: 123-137. – reference: Sarris A, Galaty ML, Yerkes RW, et al. 2004. Geophysical prospection and soil chemistry at the Early Copper Age settlement of Vésztó-Bikeri, Southeastern Hungary. Journal of Archaeological Science 31: 927-939. – reference: Schmidt A, Fazeli H. 2007. Tepe Ghabristan: a Chalcolithic tell buried in alluvium. Archaeological Prospection 14: 38-46. – reference: Berge MA, Drahor MG. 2011a. Electrical resistivity tomography investigations of multilayered archaeological settlements: part I - modelling. Archaeological Prospection 18: 159-171. – reference: Sarris A, Papadopoulos N. 2011. Geophysical Investigations at Szeghalom - Kovácshalom & Vèsztö-Mágor, Visztu, Hungary (KRAP 2011). Unpublished technical report, Foundation for Research and Technology Hellas: Rethymno, Greece. – reference: Papadopoulos NG, Yi MY, Kim JH, Tsokas GN, Tsourlos P. 2010. Geophysical investigation of Tumuli by means of surface 3D electrical resistivity tomography. 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A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary,... A large‐scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom‐Kovácshalom in southeast Hungary, covering... A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering... |
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| Title | Electrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary |
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