Uptake of Co, Cr, Ni and Cu by Pyrite in a tropical marine environment
Rem: Revista Escola de Minas, ISSN: 1807-0353, Vol: 54, Issue: 4, Page: 299-302
2001
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Example: if you select the 1-year option for an article published in 2019 and a metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019. If you select the 3-year option for the same article published in 2019 and the metric category shows 90%, that means that the article or review is performing better than 90% of the other articles/reviews published in that journal in 2019, 2018 and 2017.
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Article Description
The formation of pyrite and associated trace metals during diagenesis in a tropical pristine environment was investigated. Except for Cr, there was a generic trend towards increasing trace metal piritization with sedimentary depth. The results suggest that Co, Ni e Cu would be removed from the reactive fraction to the pyrite fraction through a sedimentary profile parallel to the diagenetic formation of pyrite. The results obtained in pristine environments may be used as a baseline to study contaminated areas for they represent true natural laboratories.
Bibliographic Details
http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672001000400011&lng=en&tlng=en; http://dx.doi.org/10.1590/s0370-44672001000400011; http://www.scielo.br/scielo.php?script=sci_abstract&pid=S0370-44672001000400011&lng=en&tlng=en; http://www.scielo.br/scielo.php?script=sci_arttext&pid=S0370-44672001000400011; http://www.scielo.br/scielo.php?script=sci_abstract&pid=S0370-44672001000400011; https://dx.doi.org/10.1590/s0370-44672001000400011; https://www.scielo.br/j/rem/a/VQqBsWZF7WgJd3LstKRLLcy/?lang=en
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