2021
DOI: 10.1002/celc.202101197
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Hematite as an Electrocatalytic Marker for the Study of Archaeological Ceramic Clay bodies: A VIMP and SECM Study**

Abstract: The electrocatalytic effect exerted by hematite, a ubiquitous component of clay bodies, on the oxygen reduction reaction (ORR) and oxygen evolution reaction (OER) can be used to acquire information on archaeological ceramics. The solid-state voltammetric response of different hematite and ochre specimens, accompanied by SECM analysis in contact with 0.10 M HCl aqueous solution, is described. In air-saturated solutions, catalytic effects on the ORR and OER are accompanied by Fe(III)/Fe(II) and Fe(IV)/Fe(III) re… Show more

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Cited by 2 publications
(8 citation statements)
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“…Considering the signals C g ,A g , C H /A H and C ORR we can apply a common scheme for the intensity of the signals based on theoretical models on the electrochemistry of redox‐active solids (Lovrić & Scholz, 1997, 1999; Oldham, 1998; Schröder et al, 2000). As previously discussed, the signals C H /A H can mainly be attributed to the oxidation of Fe(III) species; haematite in particular (Le Formal et al, 2010, Cummings et al, 2011, 2012; Doménech‐Carbó et al, 2021; Klahr & Hamman, 2014) overlapped with the catalysed OER. The intensity of the C H peak will be representative of the net amount of such Fe(III) species (as well as their shape and size distribution and crystallinity).…”
Section: Resultsmentioning
confidence: 78%
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“…Considering the signals C g ,A g , C H /A H and C ORR we can apply a common scheme for the intensity of the signals based on theoretical models on the electrochemistry of redox‐active solids (Lovrić & Scholz, 1997, 1999; Oldham, 1998; Schröder et al, 2000). As previously discussed, the signals C H /A H can mainly be attributed to the oxidation of Fe(III) species; haematite in particular (Le Formal et al, 2010, Cummings et al, 2011, 2012; Doménech‐Carbó et al, 2021; Klahr & Hamman, 2014) overlapped with the catalysed OER. The intensity of the C H peak will be representative of the net amount of such Fe(III) species (as well as their shape and size distribution and crystallinity).…”
Section: Resultsmentioning
confidence: 78%
“…That which appears in both negative‐ and positive‐going potential scan voltammograms at ~0.8 V can be associated (at least mainly) with the oxidation of haematite (C H , A H ), as judged by the similarity of the voltammetric response to that of clay bodies and haematites. The oxidation process can be represented as follows (Doménech‐Carbó et al, 2022): normalFnormaleIII2O3goodbreak+2xH2normalO0.5emnormalFnormaleIVxnormalFnormaleIII2xO3OH2xgoodbreak+2xH+goodbreak+2xe. As previously noted, both OER and ORR processes can be catalysed by some of the components of the sample, haematite in particular. This compound is a recognized catalyst and photocatalyst for the OER process (Bouhjar et al, 2018; Peter, 2013; Shimizu, Sepunaru, & Compton, 2016; Shimizu, Tschulik, & Compton, 2016; Wan et al, 2019; Zhu et al, 2013), a role conceivably played by other Fe(III) minerals.…”
Section: Resultsmentioning
confidence: 94%
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“…In the current work, we have studied ceramic clay bodies using the Fe (CN) 6 3− /Fe (CN) 6 4− couple as the redox probe in order to avoid possible complications associated to the catalytic effects of some components (hematite in particular) on the oxygen reduction reaction process (Shimizu et al, 2016; Wan et al, 2019; Zhu et al, 2013). Because these effects focused our VIMP study of the same sample (Doménech‐Carbó et al, 2022), the acquisition of complementary information required the use of another redox probe for impedance measurements.…”
Section: Introductionmentioning
confidence: 99%