2003
DOI: 10.1016/s0013-4686(03)00075-6
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Characterization of calcareous deposits in artificial seawater by impedance techniques

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Cited by 168 publications
(101 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%
“…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%
“…Cathodic protection often results in the formation of calcareous deposits on the metal surface in sea water [18][19][20][21][22][23]. The cathodic reactions of dissolved oxygen reduction or water reduction to evolve hydrogen at more negative potential will generate hydroxyl ions, with increasing the pH value of the electrolyte adjacent to the metal surface, which will promote the formation of calcareous deposits [19,[21][22][23].…”
Section: Introductionmentioning
confidence: 99%
“…The cathodic reactions of dissolved oxygen reduction or water reduction to evolve hydrogen at more negative potential will generate hydroxyl ions, with increasing the pH value of the electrolyte adjacent to the metal surface, which will promote the formation of calcareous deposits [19,[21][22][23]. Some works indicate that CaCO 3 is saturated at pH 8.7 or even lower in normal sea water and is ready to deposit as the inorganic carbonic equilibrium in the electrolyte is changed, while the critical pH value for Mg(OH) 2 to deposit is about 9.3 [24,25].…”
Section: Introductionmentioning
confidence: 99%
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