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dc.contributor.authorCuenca-Garcia, Carmen
dc.date.accessioned2019-05-02T12:15:59Z
dc.date.available2019-05-02T12:15:59Z
dc.date.created2018-10-03T19:44:39Z
dc.date.issued2018
dc.identifier.issn1075-2196
dc.identifier.urihttp://hdl.handle.net/11250/2596326
dc.description.abstractThis article explores the application of geophysical and soil geochemical methods to detect archaeological features in three traditionally ‘difficult’ survey environments in Scotland: wind‐blown sands (Bay of Skaill, Orkney), clay (Chesterhall Parks Farm, Lanarkshire) and glacial drift deposits (Forteviot, Perthshire). The results presented here are part of the first research project that systematically tested a combined approach using geophysical and soil characterisation to understand the proxy responses of known archaeological features. First, a range of geophysical techniques [earth resistance, magnetometry, frequency domain electromagnetics (FDEM) and ground‐penetrating radar (GPR)] was employed over archaeological targets. Second, the different geophysical results were considered with respect to soil chemical concentrations (total phosphate and multi‐element analysis), texture, pH, conductivity, organic matter content and magnetic susceptibility from archaeological deposits, topsoil and subsoil samples. This study demonstrates that, by focusing on the responses of single archaeological features and assessing their physical and chemical signatures, soil composition and processes involved in the ‘history’ of buried features are of importance in improving our understanding of the reasons behind their detection with geophysical means. For example, at the cropmark site at Forteviot, chemical transformations can be triggered by organic matter accumulation and increased water retention within prehistoric ditch deposits and can have an effect on the type of magnetic contrast. In addition, chemical concentrations revealing anthropogenic organic materials can explain the enhanced conductivity of theoretically impervious features, as illustrated at the Bay of Skaill site. The study also provide insights into how a particular soil environment may affect different geophysical techniques such as the masking effects of heterogeneous glacial drift deposits or deep windblown sands. These types of survey environments characterise many archaeologically rich areas in Scotland, where integrated strategies, such as the one used in this investigation, are the best option to maximise detection of subsurface features and provide confident and augmented interpretationsnb_NO
dc.language.isoengnb_NO
dc.publisherWileynb_NO
dc.relation.urihttps://onlinelibrary.wiley.com/doi/full/10.1002/arp.1723
dc.subjectArchaeological geophysicsnb_NO
dc.subjectGeoarchaeologynb_NO
dc.subjectAnvendt geofysikknb_NO
dc.subjectApplied geophysicsnb_NO
dc.subjectSoil sciencenb_NO
dc.titleSoil geochemical methods in archaeo-geophysics: Exploring a combined approach at sites in Scotlandnb_NO
dc.typeJournal articlenb_NO
dc.typePeer reviewednb_NO
dc.description.versionacceptedVersionnb_NO
dc.subject.nsiVDP::Annen arkeologi: 099nb_NO
dc.subject.nsiVDP::Other subjects within archaeology: 099nb_NO
dc.source.journalArchaeological Prospectionnb_NO
dc.identifier.doi10.1002/arp.1723
dc.identifier.cristin1617710
dc.description.localcodeLocked until 2.10.2019 due to copyright restrictions. This is the peer reviewed version of an article, which has been published in final form at [https://doi.org/10.1002/arp.1723]. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archivingnb_NO
cristin.unitcode194,31,5,0
cristin.unitnameInstitutt for arkeologi og kulturhistorie
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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