Small-area XPS and XAES study of early iron metallurgy slags (Articolo in rivista)

Type
Label
  • Small-area XPS and XAES study of early iron metallurgy slags (Articolo in rivista) (literal)
Anno
  • 1992-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1002/sia.740180716 (literal)
Alternative label
  • G.M. Ingo, L. Scoppio (1992)
    Small-area XPS and XAES study of early iron metallurgy slags
    in SIA. Surface and interface analysis; Heyden, London (Regno Unito)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • G.M. Ingo, L. Scoppio (literal)
Pagina inizio
  • 551 (literal)
Pagina fine
  • 554 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 18 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 4 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 7 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • G.M. Ingo [1], L. Scoppio [1] [1] CNR, ISTITUTO DI TEORIA & STRUTTURA ELETTRONICA, AREA DELLA RICERCA DI ROMA, CP 10, 00016 MONTEROTONDO STAZIONE, ROME, ITALY [2] CENTRO SVILUPPO MATERIALI, I-10747 ROME,ITALY (literal)
Titolo
  • Small-area XPS and XAES study of early iron metallurgy slags (literal)
Abstract
  • A group of slags dating back to Iron Age II (Aramean Period, 800-720 BC), which appeared to be iron-smelting by-products, has been found at Tell Afis (Northwestern Syria). The chemistry of these materials has been studied by means of small-area x-ray photoelectron spectroscopy and x-ray-induced Auger electron spectroscopy. The results indicate that the slags can be associated with an iron smelting process and show the presence of large amounts of FeO1-x, Fe3O4 and FeOOH mixed with different aluminum and silicon compounds. As evidenced by the Wagner two-dimensional chemical-state plots of silicon and aluminum, these latter consist essentially of quartz and various silicates, such as wollastonite, Mg[SiO4] or Mg[SiO6] compounds, melilite and other complex aluminosilicates. Chemical information agrees with the predictions of the model of early iron-making furnaces and is used to elucidate some aspects of the early iron-making process. (literal)
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