2014
DOI: 10.1007/s11837-014-0880-8
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Microstructural Features in Corroded Celtic Iron Age Sword Blades

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Cited by 6 publications
(6 citation statements)
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“…This kind of precipitates were already found in other ancient steel artefacts, e.g. in bloomery iron [5], a nail from the 17 th century [6], a Celtic sword [7]. Note, in this area the needle-like cementite is homogeneously distributed all over the grain.…”
Section: Resultssupporting
confidence: 65%
“…This kind of precipitates were already found in other ancient steel artefacts, e.g. in bloomery iron [5], a nail from the 17 th century [6], a Celtic sword [7]. Note, in this area the needle-like cementite is homogeneously distributed all over the grain.…”
Section: Resultssupporting
confidence: 65%
“…It is worth commenting that the examination of corrosion products can reveal ghost microstructures and rich structural information can be gleaned as demonstrated recently in 2nd C B.C. Celtic sword blades [42].…”
Section: The Role Of Carbon Dating In Ferrous Based Artifactsmentioning
confidence: 86%
“…6a. These two bands are attributed to magnetite (Fe 3 O 4 ) [20,35,[40][41][42]. Furthermore, Raman spectroscopy revealed that discontinuous strips with color of light marbling in the DPL layer are composed of akaganeite (β-FeOOH) mixed with maghemite (γ-Fe 2 O 3 ), Akaganeite is defined at bands 720, 319, 400 and 551 cm −1 [43] and maghemite at 720 and 664 cm −1 [43,44], as shown in Fig.…”
Section: The Characterization Of the Corrosion Layermentioning
confidence: 99%
“…It is the reason why TM is mixed with the soil particles, in many cases [22,26,48]. The formation of goethite product of the studied TM layer attributed to two factors; the formation directly from magnetite with a dissolution/recrystallization pathway and the formation separately as an Fe corrosion product as results of the reaction with Fe 2+ which migrated [20,35,[40][41][42] Light marbling corrosion DPL 720, 319, 400, 720, 664 Akaganeite, Maghemite [43,44] Orange corrosion zone DPL 398, 139, 209, 338, 1312 Lepidocrocite [44] from the core through cracks' DPL layer [49,52,53]. The corrosion products of iron sulfate (Fe 2 (SO 4 ) 3 ) and ferric chloride (FeCl 3 ) in TM layer formed as a result of the reaction with soil anions such as dissolved ions of sulfate and chloride.…”
Section: The Characterization Of the Corrosion Layermentioning
confidence: 99%