2002
DOI: 10.1016/s0022-0248(02)01532-4
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Calcareous scales formed by cathodic protection—an assessment of characteristics and kinetics

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Cited by 87 publications
(64 citation statements)
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“…Room temperature data suggest that calcareous deposits are usually formed on steel under cathodic protection, being composed of a thin Mg-rich layer on the steel surface with a Ca-rich layer on top of the Mg-rich layer [16][17][18][19]. Somehow, the conditions of this experiment did not allow the Ca-rich layer to form.…”
Section: Discussionmentioning
confidence: 78%
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“…Room temperature data suggest that calcareous deposits are usually formed on steel under cathodic protection, being composed of a thin Mg-rich layer on the steel surface with a Ca-rich layer on top of the Mg-rich layer [16][17][18][19]. Somehow, the conditions of this experiment did not allow the Ca-rich layer to form.…”
Section: Discussionmentioning
confidence: 78%
“…Somehow, the conditions of this experiment did not allow the Ca-rich layer to form. It is also reported that a local pH over 9.5 is required for brucite to form [1,17]. This, however, is only true for lower temperatures, as higher temperatures tend to shift (lower) the neutral point of water as well as the minimum pH required for the precipitation of brucite (Tables 4 and 5).…”
Section: Discussionmentioning
confidence: 97%
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“…The following increase of Rct gradually may be attributed to the repair of the passive film because of the alkaline environment formed due to cathodic polarization [42,43]. At the first stage before the 10-h polarization, Figure 4a is considered to be suitable for representing the electrode processes, which are dominated by the corrosion reaction of metal and the effect of passive film [30,39,40]. At the second stage after that time, a new semi-circle appeared at the high frequency region in the Nyquist plot as shown in Figure 3a, which is related to the produced calcareous deposits.…”
Section: Eis Evolution Of 304 Ss Withmentioning
confidence: 99%
“…In previous studies it has been established that the deposit has a two layer structure made up of a fine layer of Mg-rich brucite followed by a Ca-rich polymorph [7,14,[16][17][18][19][20][21]. Leeds and Cottis [22] found that a CaCO3 only deposit occurred at a potential of −0.7 V (SCE) and Barchiche et al [19] suggested an aragonite deposit would be formed at a potential −0.9 ≤ E ≤ −1.1 V (SCE), a combination of aragonite and brucite at −1.2 V (SCE) with brucite the only phase forming at a potential more negative than −1.3 V (SCE) in the 10-30 °C range with rotating electrodes.…”
Section: Introductionmentioning
confidence: 99%