1998
DOI: 10.1016/s0013-4686(97)00303-4
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Characterization of calcareous deposits in artificial sea water by impedance techniques—I. Deposit of CaCO3 without Mg(OH)2

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Cited by 142 publications
(79 citation statements)
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“…Additionally, like paints, they are thought to have an increased ionic resistance and to afford some degree of resistance inhibition. A considerable amount of work has already been done in understanding the mechanism formation of calcareous deposits and factors influencing this formation [2][3][4][5][6][7][8][9][10][11][12][13][14]. However, the effects of corrosion and the development of corrosion products under cathodic protection are reported sporadically [8,9].…”
Section: Introductionmentioning
confidence: 99%
“…Additionally, like paints, they are thought to have an increased ionic resistance and to afford some degree of resistance inhibition. A considerable amount of work has already been done in understanding the mechanism formation of calcareous deposits and factors influencing this formation [2][3][4][5][6][7][8][9][10][11][12][13][14]. However, the effects of corrosion and the development of corrosion products under cathodic protection are reported sporadically [8,9].…”
Section: Introductionmentioning
confidence: 99%
“…The layers (region 1 in Figure 8) are clearly Mg-rich with the lighter contrast areas (region 2 in Figure 8) and Ca-rich with the fine layer at the metal surface a combination containing both Ca and Mg. The coating consists of a fine layer of a mixture of Ca and Mg, followed by a predominantly brucite coating; this is contrary to others findings of the two layer structure of a fine brucite layer followed by CaCO3 [7,14,16,17,[19][20][21]. Figure 9.…”
Section: Compositionmentioning
confidence: 66%
“…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%
“…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%
“…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). The reason for the increase in the surface pH that results in the precipitation of calcareous matter has been studied before [16][17][18][19][20]. The anode (aluminum, in the case of TSA-coated steel) polarizes the steel, resulting in the production of hydroxyl ions (OH − ), which increases the interfacial pH.…”
Section: Discussionmentioning
confidence: 99%