1986
DOI: 10.5006/1.3583050
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Characteristics of the Rust from Weathering Steels in Louisiana Bridge Spans

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Cited by 47 publications
(28 citation statements)
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“…The morphology of the oxide layer formed on mild steels has been observed by a number of authors [25,31,[36][37][38][39][40][41][42] . The phases most frequently found present typical lepidocrocite, globular (cotton balls) (C) and fine whiskers (D) typical of goethite, and "cotton balls" (E) and cigar-shaped crystals (F) typical of akaganeite [37][38][39][40][41] . [37][38][39][40][41] .…”
Section: Morphologymentioning
confidence: 99%
See 1 more Smart Citation
“…The morphology of the oxide layer formed on mild steels has been observed by a number of authors [25,31,[36][37][38][39][40][41][42] . The phases most frequently found present typical lepidocrocite, globular (cotton balls) (C) and fine whiskers (D) typical of goethite, and "cotton balls" (E) and cigar-shaped crystals (F) typical of akaganeite [37][38][39][40][41] . [37][38][39][40][41] .…”
Section: Morphologymentioning
confidence: 99%
“…The phases most frequently found present typical lepidocrocite, globular (cotton balls) (C) and fine whiskers (D) typical of goethite, and "cotton balls" (E) and cigar-shaped crystals (F) typical of akaganeite [37][38][39][40][41] . [37][38][39][40][41] . structures ( Fig.…”
Section: Morphologymentioning
confidence: 99%
“…The morphology of the oxide layer formed on carbon and weathering steels has been observed by several authors [10][11][12][13][14] . The phases more frequently found (lepidocrocite, goethite and magnetite) present typical structures.…”
Section: Introductionmentioning
confidence: 98%
“…Many authors [2][3][4][5][6][7][8][9] have studied the corrosion products formed on carbon and weathering steels exposed to various atmospheres by X-ray diffraction and Raman microscopy. The main phases reported are lepidocrocite (γ-FeOOH), goethite (α-FeOOH) and magnetite (Fe 3 O 4 ).…”
Section: Introductionmentioning
confidence: 99%
“…The ac tual min er al og i cal com po si tion can dif fer from those of pri mary pre cip i tates. For ex am ple, the goethite for ma tion is most prob a bly re lated to the pro cess of dis so lu tion and reprecipitation of ear lier cor ro sion prod ucts, lepidocrocite most likely (Raman et al, 1986). These iron oxides might be re spon si ble for spe cific colours of both the cor rosion prod ucts and speleothem sur faces, e.g.…”
Section: Discussionmentioning
confidence: 99%